You have found an item located in the Kentuckiana Digital Library.
General account of the commonwealth of Kentucky / prepared by the Geological Survey of the commonwealth for the Centennial exhibition at Philadelphia, 1876. Kentucky Geological Survey. 400dpi TIFF G4 page images University of Kentucky, Electronic Information Access & Management Center Lexington, Kentucky 2002 b92-275-32007847 Electronic reproduction. 2002. (Beyond the shelf, serving historic Kentuckiana through virtual access (IMLS LG-03-02-0012-02) ; These pages may be freely searched and displayed. Permission must be received for subsequent distribution in print or electronically. General account of the commonwealth of Kentucky / prepared by the Geological Survey of the commonwealth for the Centennial exhibition at Philadelphia, 1876. Kentucky Geological Survey. Press of J. Wilson and son, Cambridge [Mass.] : 1876. iv, 104 p.,  folded leaves of plates : ill., maps ; 25 cm. Coleman N.S. Shaler, Director. In its Reports of progress...Frankfort, 1876-80. 28 cm. new ser., v. 2 (1877) p. 361-463. Microfilm. Atlanta, Ga. : SOLINET, 1995. 1 microfilm reel ; 35 mm. (SOLINET/ASERL Cooperative Microfilming Project (NEH PS-20317) ; SOL MN05120.03 KUK) Printing Master B92-275. IMLS This electronic text file was created by Optical Character Recognition (OCR). No corrections have been made to the OCR-ed text and no editing has been done to the content of the original document. Encoding has been done through an automated process using the recommendations for Level 1 of the TEI in Libraries Guidelines. Digital page images are linked to the text file. Kentucky Description and travel. Geology Kentucky. A GENERAL ACCOUNT CIF THE COMMONWEALTH OF KENTUCKY. Rich Low Soils, 50 to 500 feet. Variabls S.', s, geuterally of good quality. 8ac to 2.500 feet. Rather Thin Soils, o to sco feet. Excellent Soils, no to 5oo feet. I Sandy Soils, Rather Light. .oo to 55o fOct. Dense Clay Soils. , about -oo feet. About too, feet. Best Blule G ass Scoils. Abou: s- foet. 8 '. ./ 3= t. = i 1' =_ I ( , ,/ g \ / =,. Zv ' I =1 = r F I 'r ,L FiE "r) :E. -iir Workable Boal Beds. 20 to 40 teet. Excellent lire Clays and Iron Ores. Potterv Clays. Ir-n Ores. Covals in Eastern Keattiicky. I leitchfield Potash AMads. Iron Ores. 'aimn. Earths. E Fxcellent Bluildting Stones. tena Vista Sandstone. Iile intl Pottcry Claai I ,ricating Oils. Silt Wells. ,d ldi'usdg StoiS. lclinto Iron Ore. tint Earths of excellent quality. Ientuckv Mlarble. euilding Stones. Il 6 eZkw tAis level not exoesed in Ky. 'he source of some Salt Wells and of the Blue-Lick and other Salt slulphbur Waters. CAR BC NI FEROUS f-- I I I El I I i i This page in the original text is blank. 0ds ,1 Ski T4;"' 0d :: r, h : ;4: ... X, - 'At /teah s A GENERAL ACCOUNT OF THE CO;MMONWEALTH OF KENTUCKY; PREPARED BY THE GEOLOGICAL SURVEY OF THE COMMINIONWVEALTH, FOR THE Crntennial K.xbibition at pbilabrIpbia. I 8 76. CAMBRIDGE: PRESS OF JOHN WILSON AND SON. I876. This page in the original text is blank. PRE F ACE. THE following brief and imperfect account of the Common- wealth of Kentucky has been prepared under the following circumstances: Owing to the fact that the Legislature of Kentucky did not meet: in 1874, or until 3i Dec., i875, no sufficient action was taken to insure the representation of the Commonwealth in the Centennial Exhibition of 1876. On the sixteenth of February of this year, an appropriation of five thousand dollars was made for the purpose of making some slhowin, of the resources of the State, and the following gentlemen were appointed commissioners to control the expenditure thereof:- Gov. JAMES B. MCCREARY, N. S. SHALER, Esq. First District . . . . . . .W. B. MIACHEN, Esq. Second . . . . . . . CLINTON GRIFFITH, Esq. Third . . . . . . . JAMFVS H. BOWDEN, Esq. Fourth " . . . . . . . Gen. E. H. HOBSON. Fifth . . . . . . . Dr. E. D. STANDEFORD. Sixth . . . . . . . JOSEPH C. HUGHES, Esq. Seventh . . . . . . . WILLIAM \VARFIELD, Esq. Eighth . . . . . . Dr. JENNINGS PRICE. Ninth . . . . . . . JOHN DISHMAN, Esq. Tenth . . . . . . . F. L. CLEVELAND, Esq. At the first meeting of this Board it became evident that, in the brief time at its disposal, it would be necessary to put the principal part of the burden on the State Geological Survey. The work of making thle collections of minerals, soils, &c., PREFACE. that accompany this Report, as well as the preparation of the Report itself, was put upon the Survey. Coming in the time of preparation for the field-work of the year, these Centennial preparations have proved a great burden to the Survey, and have been less perfectly executed than was desired. It is believed, however, that the collections, together with this and the several other pamphlets, will give the intelligent observer a good general knowledge of the condition and prospects of Kentucky. Persons desiring additional information are re- ferred to the publications of the Survey, or to the Reports now in preparation, -a list of which is given at the end of this pamphlet. All other information concerning the re- sources of the State will be cheerfully furnished, on applica- tion to the Secretary of the Geological Survey at Lexington, Kentucky. In the completion of these pages, every possible care has been taken to exclude errors. Owing, however, to the haste of its preparation and printing, some errors have doubtless crept into the text. Corrections are respectfully solicited, and all that may be furnished will be noted in subsequent editions. It is believed that the Tables from the United States Cen- sus, the Reports of the Sanitary Commission and the State Treasurer are quite without error. vIy ackaowledgrnents are due to my assistants, Dr. ROB- ERT PETER, Mr. J. H. TALBUTT, Chemists of the Survey; to MIessrs. A. R. CRANDALL, P. N. MOORE, C. J. NORWOOD, Geological Assistants; and more especially to Assistant JOHN R. PROCTER, for his cooperation in preparing the work for the press. N. S. SHALER, Director eniztucky Geological Survey. MAY 10, 1876. iv A GENERlAL ACCOUNT OF THE CO MMONWEALTH OF KENTUCKY. GEOGRAPHY. Positiozn. -The Commonwealth of Kentucky -situated between latituLCde 36 o' and 39 o6' north, and longitude 50 oo' and I 2o' 3S' West, from \Vashington - includes about forty thousand square mliles of area, extending for six hundred and forty-twvo and a half miles along the south bank of the Ohio River, from its junction xvith the Mississippi to the mouth of the ChatteraWah or B1ig Sandy. This river forms the north er, nortlh-western, and north-eastern borders of the State. A part of its north-eastern border, one hundred and twenty miles, is formed by the Chatterawah River; a south- eastern face of about one hundred and thirty miles lhas a natural boundary in thie several rano-es which receive the common name of Cumberlanci Mountains. The southern face alone is an arbitrary lin(e of two hundred miles in length. The western boundary of about fifty miles is formed by tle AMissis- sppi lRiver. A glance at the accompanying map w-ill make it )lain that the ren-ion occupicd by this Commonwealth has a position of peculiar importance with reference to the great feature-lines of the continent. The Mississippi-River system is t'le key to the continent. Those parts which lie beyond its borders are, by their limited area or their severe conditions of climate, relatively of minor importance. In this system the State of Kentucky, all things being considered, occupies a most im. portant place. Its western border is only one thousand and GENERAL ACCOUNT OF KENTUCKY. seventy-five miles from the mouth of the Mississippi, and its eastern boundary is within five hundred miles of the Atlantic ports. The special features of position to be considered in meas- uring the importance of this Commonwealth are its central place wvith reference to the Valley of the Mississippi, and the aclvanta-es it has from its extended contact with the river system of thrat valley. Afore than any other State in America it abounds in rivers. Including the Ohio and Mississippi Rivers, where they bound its borders, the State has within its limits rather more than four thousand miles of rivers, which are more or less completely navigable. Improvements of small cost will give this amount of navigation with complete permanency, except for an average of about fifteen days per annum, wNlhmzl they are ice-bound. GENERAL GEOLOGY. Just as the State of Kentucky is geographically but a part of the Mississippi Valley, so it is geologically composed of a series of rocks which extend far and wide fover the same region. On the eastern line, between Cumberland Gap and Pound Gap, it is generally in sight of the old crystalline rocks of the Bluc Ridge, or original axis of the Appalachian Chain, and is closely bordered by rocks of the middle Cambrian or Potsdam age; but the lowest exposed rocks of the State are those found at a point on the Ohio River, about twenty miles above the Licking River, where we come upon Cambrian rocks answering to the base of the Trenton period in New York, and probablv to the Bala or Carodoc beds of England. This series is about six hundred feet thick, and consists principally of the remains of organic life laid down in a continually shallowing sea, interrupted by occasional invasions of coarser sediment, derived fromi the northward. At the close of this Cincinnati section of the Cambrian, there came the invasion of a heavier sand-flow, pr:obably coming from the southeast, that arrested the life and formed some thick beds of rock, known in the reports It is 52S riles from Columbus to New Orleans by railroad, and 472 miles to Mobile. 2 GENERAL GEOLOGY. of the Kentucky survey as the Cumberland Sandstone. After this the floor of the sea was sparingly peopled with life, dur- ing the whole of the Clinton and Niagara epochs, when it was probably deep water. This deep sunken condition of the ocean floor continued in the D)evonian time, when this section seems to have been the seat of a deposition such as is now going on beneath the Sargassa Sea of the Atlantic of to-day. The de- caying sea-weed and other orranic matter made a bed from three hundred feet thick along Lake Erie to forty feet thick in South- ern Kentucky, averaginmg about one hundred feet in Kentucky. This bed furnishes the rich lubricating oils of the Cumberland Valley. After this came again shallowe water, and quick succes- sive sand-invasions moving from the north, which formed sev- eral hundred feet of beds. These beds probably represent but a fraction of the tim-e required to form the Black Shale which lies below. This part of our section is called the Waverlv, and is commonly regarded as being more nearly related to the Carbon- iferous than to the Devonian series of rocks. After this period came a repetition of subsidence, and a cessation of -he sand- invasions. During this time there was such a development of sea-lilies or stemmed Echinoderms, that this time deserves to be called the period of crinoids. This accumulation ranges in depth from a few feet along the Ohio River to five hundred or more feet under the Western Coal-field. It marks a period of tolerably deep still water, filled with lime-secreting animals. It is probably to the unbroken character of this succession of life, and especially to the crinoids with their upright stems, that we owe the uniformly massive character of many of the beds of this Subcarboniferous Limestone. Next in the ascending series we come on the coal-bearing rocks. Their deposition was begun by the sudden shallowinig of the water over this region, bringing the old sea-floor near the surface of the lowater, and subjecting it to alternating invasions of sand borne by stron- currents, and exposures in low-lying flats covered by a dense swaamp vegetation. Each of these swvamp-periods answers to a coal-bed; each recurring subsi- dence, to the deposits of sands and shales that lie between the coals. 3 GENERAL ACCOUNT OF KENTUCKY. After the Carboniferous period, we are warranted in believ- ing that this region was but little below the sea, and with this change it became essentially subjected to land conditions alone. The wear incident to these conditions has swept away a large part of the exposed rocks, and reduced the Carboniferous series to less than half of its original thickness. Near to the present time there came a sudden subsidence of this whole region, that brought the low-lying western part of the State beneath the level of the sea, and retained it there while the Tertiary deposits were being formed out of the waste of the higher parts of the Mississippi Valley that still remained above the sea. The disturbances that have changed the position of the rocks in Kentucky have been few and far between, though they have materially affected the general structure of the State. From the mouth of the Licking south a little west- erlv, through Monroe County, extends a ridge or axis of ele- vation, the beds dipping gently, rarely over ten feet in a mile, in either direction away from it. This was in part formed during the deposition of the Lower Cambrian, but probably was completed at a much later date. This has caused the limitation of the Carboniferous beds of this region. To it in fact we owe the abundant diversity of the rock out- crops within the State. In the south-east corner of Ken- tucky there is a region between Straight Creek and Clear Creek, tributaries of the Cumberland, and the Virginia border, where the Appalachian disturbance has thrown the rocks into mountain folds. Here are some fine exposures of the deeper rocks brought up by the great faults of the region. No glacial traces of the last period are known within the State, nor are the indications of the more ancient ice-periods at all distinct. This area has probably remained south of all those profound disturbances of temperature that have so greatly affected more northern regions.t The appended generalized section on second page of cover xvill give a general idea of the successions of the Kentucky rocks. Further facts can be found in the Reports of the Survey, for which see list at the end of this pamplhlet. t For further information own this subject, see the Bieninial Report of N. S. Shaler for i874-5, Kentucky Geological Survey, nowv in press. 4 SURFACE. Surface.- The whole of Kentucky lies within the Mlissis- sippi Basin, and within the special division of the Ohio Valley. Its principal feature-lines have been given it by the river ex- cavations. A small area on the south-east, containing not more than four thousand square miles, lies within the disturbed region of the Alleghanies, and has a true mountain-folded structure. The remainder is essentially a plain or table-land, sloping from the south-east towards the north-wvest, and little broken, except by the deep-cutting river excavations. In the eastern half this table-land has an average height of about one thousand feet above the sea; the ridges often reaching to fifteen hundred, and the valleys down to seven hundred feet. The greatest difference between the bottom of any one excava- tion valley and the borders of the divide does not exceed about seven hundred feet, and is usually about half this amount. Eight degrees west of Washington the country begins to sink clown rapidly to the west. The cause of this change will be explained in the geological description of the State. Its effect is to carry the upper surface of this table-land gradually down- wards, until along the Mississippi its average height is not more than three hundred feet above the sea, and the average difference between the bottoms of the valleys and -he tops of the ridges is not over fifty feet. This considerable height of the State above the sea is of great advantage in securing it against fevers, from which it may be said to be practically exempt, except in a narrow belt in the extreme western dis- trict, near the borders of the swamp regions. Although the general surface of the State is that of a table-land sloping towards the Ohio River, and consequently towards the north-west, it has many subordinate features which should be separately described. All that part of its surface indicated as Tertiary on the accompanying map is rather imperfectly drained, the rivers having low banks, and during the winter and earlv spring being subject to overflow from the floods. The re- mainder of the State, saving a strip a few hundred feet wide along somne of the larger streams, is absolutely free from this danger. The remainder of the State, to the east of this line, has only the variety which comes from the difference in the 5 GENERAL ACCOUNT OF KENTUCKY. wear of the streams in the rock. The nature of this difference w ill be discussed under the head of geology. It is only necessary to say here that the whole of the area described on the map as Cambrian is characterized by broad flat-topped ridges, with steep-banked rivers between; the general character being that of a much cut up table-land. The part marked as Devonian has broad valleys and steep-sided, tower-like hills. That marLed Subcarboniferous, especially in the region west of the Cincinnati Southern Railway, is characterized by having all its smaller streams underground, usually only the rivers over fifty feet wide at low water having their paths open to the sky. All this region wants the small valleys which we are accustomec. to see in any country, but in their place the sur- face is covered by broad, shallow, cup-like depressions or sink- holes, in the centre of which is a tube leading down to the caverns below. All this region is completely honey-combed by caverns one level below the other from the surface to the plane of tlie streams below. In one sense, this set of under- ground passages may be regarded as a continuous cavern as extensive as the ordinary branches of a stream when it flows upon the sulrface. The sink-holes answer to the smallest ex- tremities of the branches. Some idea of the magnitude of these unde&ground ways may be formed from the fact that the Mammoth Cave affords over two hundred miles of chambers large enough for the passage of man, while the county in which it occurs has over five hundred openings leading far into the earth, none being counted where it is not possible to penetrate bevond the light of day. The Carboniferous formation is characterized by being cut into very numerous valleys, mnostly rather narrow and with steep-sloped, narrow-topped ridges on either side. The relatively narrow valleys, and the general absence of any large areas of flat land on the top of the ridges, cause this region to have less land well fitted for cultivation than any other part of the State. Every part of the surface of the State not permanently under water mav be regarded as fitted by its surface for the uses of men, not one thousandth of it being so precipitous as to be unfit for cultivation in some fashion. The writer knows 6 RIVER SYSTEMS. of no equal area in Europe that has as little waste on account of its contour. RIVER SYSTEMS. Reference has been made to the fact that the whole of this Conmmonwealth lies witllin the basin of the 'Mississippi, and over ninety per cent. of its area within the Ohio Valley, thl2 remainder pouring its waters directly into the Mississippi. There are, however, a number of large streams which are the property of the State; and two, the greatest tributaries of the Ohio, gather a part of their waters in the State. Bi',, Sauz1y. - Beginning at the eastern end of the State, we have the Big Sandy or Chatterawah River, which sepa- rates for forty miles, by its main stern and then by its eastern fork, the State of Keitucky from West Virginia. This stream is the only river of its size in America all the basin of wh-1ich. is in the coal-bearing rocks. It drains a valley of about four thousand square miles. Its name of Sandy is de- rived from the very large amount of moving sand in the bed, coming from the rapid wear of the sand rocks which compose the beds of all its tributaries. The valley consists of a narrow belt of level, arable lanld bordering the streams, and a great extent of hill land of a good quality of soil, but only fit for permanent cultivation on the more gradual slopes. The greatest value of soil-products in this valley is to be found in its timber resources, which w-ill be found specially mentioned under the head of timber. It may be said here that the valley contains, next to the Upper-Kentucky and the Cumberland Valleys, the largest amount of original forest found in any part of the State, and more than any other valley is especially fitted for the continued production of timber of varied quality. The forests throughout this :-egion readily and rapidly reproduce thelselves in the same species, after being cut away. Trhe soil of this valley is very well fitted for the growth of fruits of all kinds. The season is rather later than that of the other river basins of the State, and the liability to frosts possibly rather less than in the central regio-n. Owing to difficulties of transpor- tation, fruits have been as yet but little grown for exportation. 7 GENERAL ACCOUNT OF KENTUCKY. The whole of the cereals are produced in the valley. The soil is usually of a light sandy nature, with generally enough clay to give it a fairly lasting quality. The principal disadvantage arises from the steepness of the slope of the hills. Aifincrai' Resources. - The coal resources of this valley are, in proportion to its total area, greater than any other in the State, scarcely an acre of its area but probably has some workable coal beneath it. These coals are mostly of the ordinary bitu- minous qualities; some cannel coal occurs therein of workable thickness. A full account of these coals, with illustrative sec- tions, will be found in the general description of the eastern coal-field. Little effort has been made to find iron ores in this valley. The dense forests and the softness of the rocks pre- vent the occurrence of trustworthy surface indications. In the lower part of the valley very important ores have recently been discovered, of which the precise areas and character are vet to be determined. (See the reports of A. R. Crandall and N. S. Shaler for further details.) The Li/lie Sandy Vallcy. -The general character of this small valley is much the same as that of the Big Sandy. The river is altogether within the Carboniferous formation. The early utilization of the iron ores of this valley has led to a knowledge of its mineral resources superior to that yet ob- tained for any other equal area in the State. About thirty-five feet of workable coals are known in the several beds of the valley. (See p. 42.) Tyger/'s Creek. - Here the coal resources are more deeply cut down 1Ly the stream, which in good part flows upon the Subcarboniferous Limestone. Though wanting some of the best coals, it has many of the best iron ores of the State. Some beautiful caverns are found along its banks in Carter County. Tlhe general surface is much as in the valleys before described. In its upper part, the Limestone rocks give occa- sional areas of more enduring soils than are furnished by the Sandstones of the country to the eastward. The timber and other soil products are much the same. The stream is not navigable, but can easily be made so by locks and dams, giving continuous navigation for about forty miles along the meanders of the stream. 8 RIVER SYSTEMIS. The streams from the mouth of Tygert's Creek to the mouth of the Licking or Nepemini are all quite small, and drain a region of limited mineral resources. K-inniconick Creek gives access to a region abounding in admirable Sandstone for build- ing purposes, and to some iron ores of undetermined richness, but of considerable promise. It can be made navigable at small expense. The whole of this valley abounds in excellent oak timber. 7e Lzcki;,zg-. - This stream, the fourth in size of the rivers of the State, ranking next to the Big Sandy, passes over all the formations found in the State except the Tertiary. From its source to near the mouth of Blackwater Creek it runs on the Carboniferous rocks. As far as Duck Creek, it is still bor- dered by these beds centaining excellent coals, both cannel and bituminous. On the Subcarboniferous Limestone, which crosses the river near Blackwater Creek, is an excellent iron ore. On Slate Creek, near Owingsville, is an admirable mass of ore, the richest of the State, having at places a depth of fifteen feet or more. Triplett and Salt-Lick Creeks afford excellent building- stones, and the same series of rocks (the Waverly) furnish somne stones which give great promise for lithographic pur- poses. From the mouth of Fox Creek to the end of the river the stream is entirely in the lower Blue Limestone or Upper Cam- brian rocks, which afford excellent building-stones, but no other marketable underground products. The soil of the valley varies greatly, - light sandy loam in the Carboniferous and WVaverly series; rather wvet clays on the Black Shale and Silurian; rich, loamy clays giving soils of the first quality over the lower or Cambrian half of the stream. k'cnucky. -Sixty miles below the Licking, the Ken- Jischarges into the Ohio. This stream is the second Kentucky streams in volume, and the first in length. Blue Limestone lands of the counties drained by the Fork are noted for their large yield of a tobacco highly by the manufacturers of " fine cut," and well known in rkets under the name of " 1\ason Count) tobacco." 9 GENERAL ACCOUNT OF KENTUCKY. Its head-waters, from Sturgeon Creek east, lie altogether with the coal-bearing rocks. At least four hundred miles of water- front, open to vessels able to carry three hundred tons of coal, can be mad2 or the three forks of this river. The coal holds along the hill-sides as far as Station-Camp Creek. The ul)per half of the Red-River branch contains also an abundance of coal. The entire drainage of the Kentucky River, above its forks in Lee County, is in the Carboniferous rocks. No portion of the State exceeds the Upper Kentucky region in number, thickness, or quality of coals. A preliminary section, made by 'Mr. P. N. Moore, of the Kentucky Geological Survey, from Red River in W\olfe County to the mouth of Trouble- some Creek in Breathitt County, establishes the fact that up to the latter point there are at least five workable coal-seams above the Conglomnerate Sandstone. The following analyses, from carefully averaged samples, will show the excellent cqual- ity of these coals:- No. i. NO. 2. N-O 3. No. 4. No. 5. Specific Gravity..... . 1.300 1.294 1.297 1.290 1.289 Moisture.. . . . . . . 2.50 3.50 3.56. 2.76 2.10 Volatile Combustible Matter . 41.10 35.20 33 56 36.60 36. 2o Fixed Carbon. . . . . . 49.22 56.70 58.38 56. 3o 58.20 Ash. . . . . . . . . . 7.18 4.60 4.50 4-o6 3.50 Coke . . . . . . . . . 56.40 6r.30 62.88 60. 56 61.70 Sulphur.o . 0.818 1.189 1.3S1 o.S65 0.836 No. i is a coal from Frozen Creek, Breathitt County. No. 2 is a coal 5' 7" thick, from D)evil Creek, Wolfe County. No. 3 is a coal fromn Spencer's Bank, Breathitt County. No. 4 is a coal 6' thick, from Wolfe Creek, Breathitt County. Ne. 5, from near Hazard, Perry County. Analvses by Dr. Robert Peter and 'Mr. Jno. H. Talbutt, chemists for the Kentucky Geolagical Survey. The cannel coal of the Upper Kentucky is to be found over an extensive area, and is of a remarkably good quality, as will be seen fromn the following analyses by the chemists of the sur- veV, made fromn average samples- I0 PLIVER SYSTEMS. N 0. 1. No. 2. No- 3- No- 4. No. .5 Specific Gravity... . . I.280 1.265 1.280 I.180 Afoiswlre.. . . . . . . o,4 IT 34 1. 20 I. -10 Moisture.0.94 1.30 3.40 1.0 .0 Volltile Combustible Mlatter . 2-38 47.00 34.4 ;S.So 40.S6 Fixed Carbon. . . . . . 35 54 44.40 46.96 35.30 46.44 Ash . . . . . . . . . 11.14 7.30 6.24 4.70 9.50 Coke . . . . . . . . . 46.68 51-70 53.20 40.00 57.94 SulIlhur. . . . . . . 1.423 I.574 o.630 not est. 0.634 No. i. Georges' Branch Cannel Coal, Breathitt County. NO. 2. Haddock's Cannel Coal, mouth of Troublesome Creek, Breathitt COU111tv. No. 3. Robert's Coal, Perry County. No. 4. Frozen Creek, Breathitt County. No. 5. Salt Creek, Perry County. Three of the best gas-coals in Scotland and England are: (No. i), Lesmahago Cannel; (No. 2), Ramsay's Newcastle Coal; (No. 3), \Veym'is Cannel Coal. Compare w ith the above the followin(g analyses, taken from Dr. Peter's Report, Vol. II. First Series Kentucky Geological Survey:- N O. I. N o. 2. No. 3. Specific Gravity.. . . . 1.228 1.29 1.1831 Volatile Matter.. . . . 49-6 36.8 58.52 Fixed Carbon. . . . . . 41.3 56.6 '5.28 Ash . . . . . . . . . 9.1 6.6 14.25 100.0 100.0 03.45 Sulphur not determined. The indications are that the coal-measures thicken, and the number of workable coals increase south-easterly from the mouth of Troublesome Creek. This, however, can only be determiined by detailed survey. In addition to the numerous workable coals above the Con- I I GENERAL ACCOUNT OF KENTUCKY. glomerate Sandstone in this region, there are two workable coals below the Conglomerate. The excellent quality of these coals can be seen from the analysis, No. i6oi, p. 8i. Just below the coal the Carboniferous Limestone bears upon its top the ore known as the Red-River iron ore, whichl has longt furnished a very celebrated cold-blast chai-coal iron, well known as Red River car-wheel iron. There is probably about one hundred miles of outcrop of this ore witlin a short clis- tance of the tributaries of the river, and within twenty miles of the main stream. Salt, fire-clay, and hydraulic cement abound in the Black Shale and Upper Silurian rocks. From Burning Creek to the mouth the Kentucky Valley runs entirely within the Upper Cambrian or Blue Limestone. The soil's in this valley have the same character as in the Licking, ranging from the light loamy soils of the Carbonifer- OUS, through the clays of the Silurian and Devonian to the exceedingly rich blue-grass soils of the Cambrian and Cincin- nati Limestone rocks. The navigation of the Kentucky River has been improved by locks and dams as far up as a point about twerty-five miles above Frankfort. The stream is admirably adapted for the extension of this method of naviga- tion, until over six hundred miles of navigable water is secured. As in the case of the Licking and the Green, it has the pecu- liar advantage of having a very great variety of soil and natural products within a narrow compass. The timber resources of the part of this valley that lies within the coal-bearing area are very great; all the important timber trees of Kentucky, except the cypress, are found within the valley. The black walnut is found in abundance on the hill-sides throughout this section, the finer qualities of oak, much vellow pine, some white pine, &-c. Sal; River. - This stream is the only considerable river in the State that has little in the way of mineral resources. It will be seen that it follows the line of the outcrop of the Sub- carboniferous Limestone throughtout its whole extension, being the only river in the State that does not run across the general trend of the stratification. The valley abounds in good Lime- stone for building purposes, the whole of the Subcarboniferous I 2 RIVER SYSTEMS. Limestone being exposed along its banks. The ufnderlying Sandstones of the WVaverly also furnish excellent building materials. Iron ores occur in the Waverlv Shales, and perhaps also in the Subcarboniferous. The salt-bearing rocks of the lower Waverlv and the Black Slale are doubtless accessihle from the line of the surface of the valleys. The flowT of water is rather more steady than in the other rivers to the east- ward, on account of the cavernous nature of the rocks along its bainks. It will, therefore, furnish excellent wvater-powers along its whole course. The soil of this valley is of lpretty even excellence through- out. The head-waters drain a region of Blue or Cambrian Limestone, and the maia stream takes the soils of the Waverlv which are rather sland\-, and the Carboniferous Limle- stone which affords ver, gc)od soil. The river has a more than usually rapid fall, descending about six hundred feet in its course of about one hundred miles from the head-waters, - probably the most rapid Fall of any stream-i of its size in Kentucky. This will make the imiprovemnent of the streamn more difficult than of other rivers of the State. The Gi-ccvt. - This, on many accounts the finest of the rivers that have their whole course wvithin the State, differs in many striking regards from the other streams. It is at its lowest stage ablout one-tthird larger than the Kentucky. The Kentulckys and Licking, streams have their mineral b Ats at their head-waters, while tCe lower part of their course lies in districts havin, their greatest value in their agricultural resources. The Green, however, has its lower half witlhin the western coal-field, and its upper \vaters in the older rocks. This western coal-field is described in another section of this pamphlet, to which the reader is referred for details. In a general wvay it maya be said that it is exceeding rich in coals of varied quality, and abounds in iron ores of highd grade. MIuddy River, Bear Creek. and N6lin, are peculiarly rich in iron ores, the district between Bear Creek and Nolin beingr one of the richest in America in the ores of the Carboniferous period. Soils. - The soils of this valley have throughout a higll order I 3 GENERAL ACCOUNT OF KENTUCKY. of merit when they lie on the Subcarboniferous Limestone. They are clay loarns with a perfect underground cavern drain- age, excellent for all grains and for fruits. The coal-bearing, rocks give soils of a much highler quality than is usual in suChi formations, nearly the -whole of the area occupied by these rocks giving good grain crops and tobacco of a high quality and of a large vield to the acre. The whole of this valley is peculiarly fitted for furnislhIin0 water-powe:. Rough Creek, Pond River, MuIuddy River, Bear Creek, Nolin River, Big Barren River and its tributaries, and all the other streams heading in the Subcarboniferous or lower Limestone are singularly steady in their flowv, owing to their urderground reservoirs of water. To these under- ground sources they owe as well their comparative immunity from freezing, the Green rarely freezing in the winter season. The whole of this valley is singularly -well fitted for fruit culture, on account of its immunity from winter killing and destructix'e spring frosts, and its neighlborhood to Chicago, Cincinnati, Louisville, and other great markets. Nearly the whole of this valley abounds in excellent timber, principally hard-wood. The upper wvaters have large quan- tities of valuable cedar timber ; the Carboniferous district abounds with the several species of oak, great quantities of valuable h1ckories, walnut, tulip-tree (or poplar), some holly of large size, sometimes over fifteen inches in diameter. There is also a good deal of hemlock along the cliff borders of the streams, and some cypress in the lower swamps in the Pond River district. T7racdlwalcr Rzvcr. - This stream bears about the same relation to the western mineral field that the Little Sandv does to tl-e eastern coal-field. Excepting a few of the less important head-waters, the whole of its basin lies within the coal-bearir.g rocks. Its soil is very fertile and well fitted for the growth of cereals 'and tobacco. An abundant growth of hard-wood timber of varied species compose its forests; for its area it is one of the richest fields for the oaks, hickory, poplar, that exists within the State. The coals accessible in this valley are, in part, only above I4 RIVER SEYSTEMS. the drainage level. Thiey represent some of the best coals in the western district. Iron ores exist in abundance, but have never been worked. Thle Cumzberlanzi. - This river has the upper half and lower sixth of its course within Kentucky. The upper region lies within the coal-field and traverses some of its richest sections. The part above Cum-iberland Ford is in a great mountain valley between Cumberland Mountain and Pine Mountain. This vallev is about twelve miles wide, and is a fertile region abounding in excellent tmlnber, with the land, so far as arable on account of its steepness, of excellent quality. About one- third of the surface is fit for culture with the plow. Below Curnberland Ford the river bottom widens, and the mountains sink down. The land along the river is very rich indeed, and that back on the hills is of good quality. At about two hun- dred miles from its source, the stream cuts down into the lower rocks, and from near the K'entucky line throughout most of its current in Tennessee runs on the Upper Cambrian or Blue Limestone formation; when it reenters Kentucky it is back to the rocks of the Subcarboniferous age, and the valley is an exceedingly fertile district. The line of this valley brings its southern edge near to the Tertiary formation of the western part of the State. Its proxim-iity to the Tennessee on the wrest and to the Green on the east narrows the valley to small size; all the tributaries on the lower waters are small, but the tip- per confluents of this stream contain some of the finest rivers of the State. Martin's Fork, Clear Creek, Straight Creek, Rockcastle River, and Big South Fork are all considerable rive-s, and afford excellent water-powers. They are all streams of great steadiness of flow, and all the conditions are favorable to the formation of valuable water-powers. They all traverse regions of very great resources in the way of iron and timber, and have soils of fair quality. It is probable that no other valley in the WVest possesses so great a body of valuable timber as the Cumberland and its tributaries. Poplar, the several varieties of oak, beech. maple, sweet and sour gum, walnut, and other deciduous trees abound. Red cedar, yellow and white pine, are fcund in certain districts in considerable quantities. 1 5 GENERAL ACCOUNT OF KENTUCKY. The Cumberland is nearly equal to the Kentucky in the area and richness of its mineral districts. The coal section in the valley between Pine I\Iountain and the Cumberland Moun- tains has a depth of two thousand feet, and about twenty dis- tinct beds of coal, of whichl half-a-dozen are workable. The iron ores Ilave not been examined or sought for. They may be expected to occur at several points in the coal-bearing rocks and on the top of the Subcarboniferous Limestone. The rich Clinton ores of the Cumberland-gap districtt though not in the drainage area of the Cumberland River, are in necessary commercial relations with it, inasmuch as they must be smelted by the charcoal and stone-coal of this valley. It is also most probable that these same ores are accessible along the hundred miles of the Pine-Mountain fault, by means of adits or galleries above the drainage, or by shafts of shallow depth. Detailed reports concerning this region may be ex- pected in the fifth and eighth volumes of the Reports of the Survey. 3eneath a large part of the upper Cumberland region the formation, commonly called the " Black" or Devonian " Shale, is filled with a lubricating oil of great value. Experience has shown that these wells are practically inex- haustible, and that the oil is of a very superior quality, espe- cially fitted for use in high latitudes, where other oils congeal. From one of these wells on Otter Creek, in WNayne County (see map), the oil is exported by wagon to Cumberland City, thence by rail to the river, thence by a precarious navigation to Nasllhille; even with these hindrances the business is Analvsis of an average sample taken from a coal-bank forty-four inches thick, on Yellow Creek, Bell County:- Specific gravity.. . . . . . . . . . I.282 Moisture .1.36 Volatile combustible matter . . . . . . . 35.80 FixedCarb.n . . . . . . . . . . . . 59.54 Ash... . . .... 3.30 Coke . . . . . . . . . . . . . . . 62 84 Sulphur... . , 0.97 t See Report of P. N. 'Moore. in fourth volume, and the Biennial Report of N. S. Shaler, :hird volume, in second series. r6 RIVER SYSTEMS. found to be profitable. \With effective transportation a very large industry could be founded on this product; for, unlike the ligrht burning oils, those heavy lubricating petroleums are of rare occurrence, and find a market that is scarce supplied by the present production. This river is navigable for steamboats for a part of the year as far as the crossing of the Cincinnati Southern Railway. The great falls offer an obstacle to improvement of navigation into the upper waters, but not an insuperable barrier. Except this fall and the rapids irmnmediately above it, the stream offers great facilities for improvemnent; it would be possible to make at least four hundred miles of slack-water navigation within the mineral belt on the upper waters of this stream. T/zc Tcnncssec. -This river debouches into the Ohio, within Kentucky, and has the last sixty miles of its magnificent course within the State. This part of the valley is among the lowest lands of the State ; on the east side the river is bordered by the Subcarboniferous Limiestone, rich in iron ores; on the other, it extends into the low Tertiary lands which reach to the Mis- sissippi River. The land along this stream is very fertile. The -limitations of this brief sketch make it impossible to speak of many lesser streams of great economic importance, some of them capable of being made navigable by simple canalization. Nor has reference been made to the resources of the main Ohio. The mineral resources available in this valley are only in part derived from Kentucky, so they will not be discussed here. The alluvial soils within the valley of the Ohio are of a high order of fertility throughout its course. From the mouth of the Chatterawah, or Big Sandy, downwards to the mouth, the valley is distinctly bounded by cliffs, which gradually diminish from about six hundred feet to less than thirty feet near its mouth ; no part of alluvial plains have any distinct swamnv character until we come below the mouth of the Tennessee, though they, in patt, are liable to winter overfloxvs. This strip of arable land on either side of the stream widens from an average of about one-half cf a mile near the Big Sandy to about one and a half miles near the mouth of the Tennessee. Its fertility becomes the greater the further it is removed to the west. 3 1 7 GENERAL ACCOUNT OF KENTUCKY. WATER-POWERS. The very numerous rivers of the State supply a large number of water-powers of great value. Although the soils want the retentive power which belongs to regions where they were formed by the glacial period, and extensive lakes are wanting, owVing to the absence of the action of the same agent in this region, yet the freedom from closure by ice, and the excellent character of the foundations for dams and mills, goes far to balance the advantages. It is impossible to con- sider these mill powers in detail. The following points may be noted: The main Ohio at the falls at Louisville offers a very great but unused water-power; the flow at the lowest stage of water exceeds that of any water-power used in this country. A very valuable power exists at Cumberland Falls, in Pulaski County, where a stream as large as the one named falls about sixty feet. This point is near the Cincinnati Southern Railroad. The various slack-water dams now building and to be built in the State all afford admirable water-powers where the powrer itself and the transportation of the manufactured products are both well assured. As a general rule, the other water-powers are best where the waters drain from the Sulb- carboniferotus Limestone; next in order of merit when their supply is from rocks of the Waverly or Subcarboniferous Sand- stones. Next in value are the streams in the Blue Limestones, or Upper Cambrian; and, least of all, the streams from the coal-bearing rocks, which are generally largely composed of dense Sandstones and impervious Shales, having little in the fway of water-storage spaces. The deficiency in the storage of water in the soil can be easily remedied by use of storage reservoirs, which, from the depth of the upper valleys and the generally good foundations, can be readily made. SOILS AN.D AGRICULTURE. All the Kentucky soils except the strip of alluvial land along the banks of the rivers have been derived from the decay of the underlying rocks. They may be called soils of I 8 SOILS. immediate derivation, as distinguished from the soils made up of materials that have been borne from a distance by water, or which deserve the name of soils of remote derivation. This feature of immediate derivation gives the Kentucky soils a more local character dependent on position than those of any State north of the Ohio. In that region the interm-ingling of materials due to the last ice period has reduced the soils to a more nearly equal character. Beginning with the lowest rocks, the soils of the Blue or Cambrian Limestone are those of the first quality, and are 'surpassed by no soils in any country for fertility and endurance. These soils are derived from a Lime- stone very rich in organic remains, which decays with great ra- piditv, and continually furnishes its dbris to the deeper-going roots. This soil varies considerably in different districts, and at some few points, where the underlying rocks are locally rather sandy, it falls from its usual high quality. The best soil may be known by the growth of blue ash, large black locust, and black -walnut. Mlany other trees are found in its forests, but these are characteristic, and are never found tagether save on best soils. The most advantageo-is crops on this soil are grass, it being a natural grass land, all the grain crops, and on the richer parts hemp. Fruits of all kinds belonging in this climate do quite well on this soil. The steep slopes along the valleys are well suited for grape culture. The peculiar features of the soil are its endurance under culture. This region having been the first settled in the State, the extraordinary capacity of this soil for withstandincg bad methods of farming led to the gen- eral opinion that soils of less inexhaustible properties were not worthy of notice ; hence the comparative neglect of the soils of the lower rocks, which, though generally fertile, can be wasted by careless agriculture far more easily than those of the blue-grass region. The soils of the Silurian (commonly called Upper Silurian Limestone) are much less fertile than those of the underlying rocks. When not too cherty, they make good grain a-id grass lands. There is generally such a mixture of the decayed mat- ter of the underlying and overlying rocks that this thin forma- tion, which does not exceed about one hundred feet thick, gives I9 GENERAL ACCOUNT OF KENTUCKY. but little soil which can properly be called its own. As this formation ranges from forty to one hundred feet thick in the outcrop, there is only a small area, not exceeding eight hun- dred square miles, occupied by these soils. The soils of the Black or Devonian Shale have even less im- portance than those of the formation last mentioned; not over four hundred miles of the area of the State is covered by them. WShen found, they are generally a tough clay which only needs drainage to have very valuable qualities. The \Waverly or Subcarboniferous Sandstone has a thick- ness of several hundred feet, and furnishes an area of about five thousand square miles. Its soils are generally light clay loarns, beccming more sandy as we go towards the north-east. They are throughout excellent fruit-soils, and yield fair crops of all the grains. Next higher in the geological succession we find the Sub- carbonifercus Limestone, or Cavern Limestone, as it is com- monly called. This rock makes a larger area of soil than anv other formation except the coal-measures and the Blue Limestone (Cambrian), and may slightly exceed the latter in area. These soils are generally excellent enduring soils, rank- ing next to the best of the Blue Limestone soils. They are excellent grain and fruit lands, and in the western region are well suited for tobacco. Their drainage is generally excel- lent, on account of the cavernous character of the Limestone beneath. The soils of the Carboniferous belt occupy by far the largest single area in the State, covering not far from fourteen thou- sand miles of surface. The soils in it are exceedingly variable in character, but are generally a sandy loam. On the con- glonmerate or lowermost part of the coal-measures, the soils are usually the poorest, -about the only really infertile soils of the State beinig the small strips of the soils formed on this rock. These strips are usually very narrow, and do not include alto- gether mor2 than three hundred or four hundred square miles. The remainder of the Carboniferous area is composed of fairly fertile light lands, interspersed with areas of great fertility. 20 Somne of the best lands of the State are upon the summits of the Carboniferous mountains of Eastern Kentucky; it is safe to say that, wherever the shape of the surface admits of cultivation, the Carboniferous rocks of Kentucky furnish fair soils adapted to a varied range of crops. The considerable part of its surface that is not fit for agriculture is admirably suited for the production of hard-wood timber of the most val- uable varieties, and will doubtless have in this fitness a source of wealth scarcely less than tillage of the best lands could give. As a whole, the surface of Kentucky includes a larger area of very fertile land and a less area of barren soil than any other equal area in a State so rich in mineral wealth. The prize of wealth hidden beneath the earth is generally bought by conditions that do not favor agriculture; but, despite the fact that Kentucky -has resources of coal and iron that ex- ceed those of Great Britain, she has scarcely a square mile of surface that cannot give a constant return from its soil. The production of these soils includes the whole of the crops of the Mississippi Valley, except the sugar-cane. Indian corn, wheat, oats, rye, barley, buckwheat, flax, flonrish over its whole surface. Sorghum, for making molasses and sugar, is grown over its whole area. The conditions favor the making of suaar from. beet-roots. All the ordinary fruits attain their perfection here. Cotton is raised as a crop in the south-western region of the State. Tobacco is more extensively cultivated here than in any other State in the Union. The best natural grass lands of the continent are found in the Cambrian or Blue Limestone district. Hemip is extensively grown in the same area. The blooded horses of the State are perhaps the most famous of its ex ports. Its remarkable superiority in this regard is doubtless in part due to the carp given thereto, but, in the opinion of the best juLdg-es, is in the main the result of the peculiarly favorable effects of a combination of conditions in which soil, climate, and water all have their place. Horned cattle and sheep also do well here. Climiaic. - That this State is peculiarly well fitted for the European races is shown by the fact that in no region is there a greater degree of physical vigor than in the population CLIMATE . 21 GENERAL ACCOUNT OF KENTUCKY. within its limits. The statistics of the United States Sanitarv Commission distinctly show that this is the largest-bodied native population in this country or Europe, as in the table on the opposite page. The climatic conditions, as far as they can be described here, are as follow-s: The average temperature is about 5o0 Fahr. As in all America, the range of temperature throughout the vear is considerable; it is, however, much less in Kentucky than in the States further to the north. It is rare to have the thermometer below the zero of Fahrenheit, and it never hap- pens that t remains for twenty-four hours below that point. The summ- ers, though warm, are less oppressive than along the lowlands near New York for instance, oving to the consider- able elevation above the sea and the relative dryness of the air. The summer heats do not at all interfere with the labor of northern-burn people in the open sun. There is much experi- ence to show that in this respect the climate is not more trying than that of New York State. Open-air work is generally possible during the whole winter, the ground rarely being so frozen as to impede construction-work or even ploughing. Cattle are not generally fed more than three to four months, and are often left in the pasture for the whole winter. The rainfall is about forty-five inches per annum along the Ohio River, increasing towards the south-east to about sixty inches at Cum-berland Gap. This is distributed with fair reg- ularity thlrcLighout the year, -the summer droughts not being sufficient at any time to destroy crops well planted on well ploughed ground, and rarely sufficient in any way to embarrass The foll-owin!Z, compiled from the United States Census Reports for 1870, shows the healthfulness of Kentucky:- In population, Kentucky ranked as the eighth State in the Union. In percentage of deaths to population, Kentucky ranked as the twenty-ei"1hth State: that is, there were twenty-seven States havinlg a greater death rate than Kentuckv. Population. in 1870, 1,321,011. Deaths, from all causes, 14.345, -or 1.09 per cent. of the population. The health of the State has increased, since i8;o, as follows :- Death to population was, in i18o, I.53 per cent. "I S6o, 1. 42 " "" " " 1870. 1.09" 2 2 CLIMATE. - 0 C; :: 3 C - -: .. It -;: Y 't , j-, :1 I = ;x : 5 S ;.4 N, M N ) 1 t N . \ 'IC '. ')" In C r, 0 v 0 :71 _-, m C' I tr- ;X -1 In N-0 -NO NNN N - 'N NN N N N 6 N N, e N N N N N N1 CA N1 Nq N 0 I. 0X _ CO t. OtXo 0c -- -C 0 00 - -tl - - -o -H, rt In i- 'n n Ne -5 C - -f, 0 ' :- -r C 0 C, N. c -EN 0 u .C c' N iC cCAN N. N 444441A4444I 0 t '_ N-t t IJ _ _ _ (-c _ _ _ _ _ _ _ _. _ _ _ _ _r. _I oI_ _t _ _ _ - F f -t i'Ft 4f 4t-ott tL _ s _ t) n m sM ', t cn I n I- -A- r-, -t 0 0 CC, N In.Z ] It RR.Nt.N.N.C -- _.-N -C -'- -C- - r-'N - _Z0-Z _ 'oN-N.NrZN0 t ZI I- N1) CiC "N - CC N. tN C N. '0 '.0 I'D 'IO II El- 0 - CC - z , 0 I '0 t - 0 t N ZN'0 In c ,. . .C. . . . CC '. '.0 r' 0 o '. r 34: 4) 4 ' _9 V - N 0 N. t- O-Z 0 cL3 - 0N srX 8 m _ 1l Z" ro _ 'lXz O 1 'N 0 - 0 r' - 0 N. (' -NNN N. N C5 z 5- '. r C - . . " a c- _C & - Z 0 0 -.-n.e_ . . . I I I I I I t t4 15 n2 H z 0 CC H z "S 'I- 0 Cfl z z -S -S U z C/C H 0 H -S 0 0 U 0 C'- U4 Un rLl 0 4 rJD r,, t _! z ,. .- IJ I i I I 23 24 GENERAL ACCOUNT OF KENTUCKY. agriculture. The number of days of sunshine is relatively very laige, considering the amount of rainfall. The healthfulness of this region is not exceeded by any State in this country. Epidemic diseases have never been destructive outside of somie of the towns. The experience of the city of Lexington has shown that even in the towns such diseases arc curable by the use of pure drinking-water. Alias- matic diseases are not known on the table-lands, being limited to the low regions near the large rivers; at least seven-eighlths of the State enjoy an absolute immunity from such diseases. ConsuLmption is rare, compared with the northern and eastern' States. Yellow fever never occurs. This region is remarka- ble for the number of persons in extreme old age, who retain their faculties quite unimpaired and a large share of bodily vigor. The writer, who has made this subject of longevity a MEAN TEMIPERATURE. .0 - 11 ! _ _ ___. _ __ ____ Loulisville.59. o846.433;436.739 1507 291 64. 5. 667 S.; 870-7;!. 3 I Loulosille..6o.544.038.030.8 360o38.7 591 167.674.3790 ,S.2 7 69.S56.3 Le 72-73. Lexi.gton. 3 .2 27.93 0.4 35(640-.9 53.1 16473 7!, 6573 768 Louisville..56.639.529-431.1 3i.S43.3 34.667. 78-I 79. 75 69; 55923 1,S73-74 .iI Lexington.53.84.7 39.636.5 39 244 3 46ig9 63.f677 9 7,7S 85-70.g5 5 Louisville..54.41.5 38-737.5 39. 45.6 8 168 2 o 87S.7 7 3 ,2 2 57 2 RAI N-FALL. - Inches. LouisvIL e.3.892.402.20 3.03 5.74 ' 7.2920.65.973.862.223.061.2342.95 Louisville.. S.852.513.29)() () 1.41 j 8.40 6.19 3.672.45 4.41 38.67 t 1872-73. ! I Lex;,lsto-. 1.21 4 53 .73 2.886.oS4. 543.372.94 .6 .j Louis-ille.3 92o.56 I 2.592.935.423.39 1 3.055.73 i 3.873.433.042.5640.42 tR73-74-1 , T.exinzgtoss.5.472.0)4.41 5.41 4.8 5 6.8r0.793. 5 6.26 1.87. 2.8950.04 Louisville..3.26 I 2.196.392.39 I 5.1S6.636.o1 I 1.172.652.713.230.6243,33 Average Annual Mean for thirty years, 55.9' Rain-fall, 50.30 ilnches. Rain-uage not in position. t Ten Months. SCENERY. matter of much inquiry, is satisfied that the region from the Big Sandy to the Cumberlandl, especially the higher parts of the table-land, and where Limestone soil is found, is peculiarly fitted by its conditions to retain the vigor of the body to an extreme old age, deservinrg, in this regard, to rank wvith the Canton de Vaud in Switzerland and the few other favored spots where longevity is a characteristic of the people. He is also satisfied that the proportion of bodily deformities and diseases of imperfect development,-such as curvature of the spine, rickets, &c.,-is smaller within this area than among any equally large native, population in this country or in Eu- rope. Of the whole poj)ulation of whites and blacks, about eleven hundred thousand of the former and three hundred thou sand of the latter have been on the soil for three genera- tions (these numbers are approximate). It needs only inspec- tion to slhow that there has been no degeneration during this time, and that the world-wide reputation for vigor which the State has acquired is not likely to be lessened in the time to come. i ;a/rlRBcau1/ics of Scec'zcry.-In all those features of natural beauty which go to lend attractiveness to a fertile region, this State is much favored. Above any other State it is rich in rivers, and these lhave an. incomparable variety of loveliness. Their head-waters lie around the stately mountains of the Cumberland range, their middle distances course through gorges often cut into deep canons, and their lower wvaters verge gently into the (great valleys of the Ohio and MIississippi. The valley of the Upper Cumberland lies in a broad moun- tain troughl, affording some of the finest scenery of the whole .Appalaclhian chain. Big South Fork of the Cumberland, Rock- castle River, Red River, of the Kentucky the whole of the Upper Kentucky, Tygerts Creek, the upper part of the Big Sandyl, - all present that mingling of clear stream, steep cliff, and beautiful vegetation, which is the great charm of a moun- tain country. The canon of the Kentucky, between Frank- fort and Boonesburg, is perhaps the most charm-ning, scenery of its kind in the region. east of the Mississippi. The deep gorges of Green River and its tributaries, Nolin and Barren 4 25 GENERAL ACCOUNT OF KENTUCKY. Rivers, abound in exquisite scenery; cliffs, in the semblance of castles, towering hundreds of feet above the streams, their faces pierced by caverns, and hung with a foliage of almost tropical luxuriance. The cultivated district of Central Kentucky, comnmonly known as the Blue-grass District, is perhaps for its area the most beautiful rural district in America. The surface is un- dulating; large areas of the original forests have been cleared of their undergrowth and produce a fine close sod, and in these wood-pastures are some of the finest flocks and herds in the world. It has happened to the writer to pass on sev- eral occasions from this region to the richest lands of Middle England, or vice versa, and he has always been struck by the singular likeness of the two countries. There is probably a closer resemblance between the surface of the country, the cattle, horses, the agriculture, and even the people of these two areas than any two equally remote regions in the world. The western part of the State abounds in natural beauties; the rich forests and the noble rivers, the Mississippi, Ohio, Tennessee, Cumberland, and the Green, give it a most attrac- tive surface. Even the deep swamps of the lowest re-ions have a sombre charm that deserves the attention of the tourist. No region ever visited by the writer exceeds in weird beauty the environs of Reel Foot Lake, where the great earthquakes of i8ii-i3 formed a lake some fifty miles in area. All over its surface stand the trunks of the cypresses that grew in the swamp before the convulsion. These are now reduced to tall columns blackened and whitened by decay. The surface of the lake is a mass of water-plants, in summer a perfect carpet of flowers; Nymphieas, a half-foot or over, and the Nelumbium, water-chenquepin, or American lotus, a golden flower often exceeding a foot in diameter, cover its surface with their blos- soms and fil[ the air with their perfume. Caverns. -- The subterranean beauties of the State are al- ready famous. The Mammoth Cave is, however, only a noble specimen of a vast series of caverns, to be numbered by the tens of hunlreds, that occupy nearly all of the Subcarbonif- erous Limestone area of the State. This cavern-belt extends 26 MARKETS AND TRANSPORTATION. in a gnreat semicircle from Carter County, where there are several beautiful caves arid two remarkable natural bridges, to the Ohio below Louisville. These caverns have as yet been but little explored, and their beauties are mostly undis- covered. There are probably many thousand miles of these cavern-ways accessible to man. The Indian tribes knew them better than our own race; for it is rarely that we find any part of their area which does not show some evidence of the presence of ancient peoples. MARKETS AND TRANSPORTATION. As regards proximity to markets, this State has peculiar advantages, which only await the completion of transportation routes already begun to render its position unequalled among American States. Reference to a map will show that it is the most centrally placed in the group of States east of the Rocky Mountains. From the geographical centre of Kentucky it is about an equal distance to Central -Maine, Southern Florida, Southern Texas, and Northern Minnesota. The State of Col- orado, the Great Lakes, and the mouth of the Mississippi fall in the sweep of the same line. The river system of the Mississippi has its centre within the borders of Kentucky, and her lands are penetrated by more navigable rivers than any other State in the Union. Her terri- tory includes about fifteen hundred miles of streams that are navigable at all stages of water, and about four thousand miles of other streams that can be made navigable by locks and dams. These streams give access to the whole Mississippi system of inland navigation, which includes about twenty-five thousand miles of streams now navigable, or readily rendered so by the usual methods of river improvement. The State has at pres- ent connection by water transportation with at least twenty millions of people, occupying an area that will probably con- tain near two hundred millions within a century from this date. There is a proposition now under discussion to use the con- vict labor of the State on the improvement of the rivers, which if carried to success is likely to make their complete canalization an accomplished fact within twenty-five years. 2 7 GENERAL ACCOUNT OF KENTUCKY. The existing railways of the State form a system which wants but a few connecting links to give it an admirable relation to the rest of this country. The north and south lines consist of the following roads, beginning on the cast: The Eastern Kentucky, from Riverton in Greentup County to \Villarc in Carter County; thirty-five miles of road built to develop the coal and iron district of this section, with the expectation of eventual continuation to Pound Gap, and connecting with the south-eastern system. Thie 1\Iavsville and LexinAton Railway, running south as far as ILexington, and connecting there with the system of roads about to be described. Third in the series on the west we have the Ken- tuckv Central Railway, now extending to Lexington along the baniks of the 'Main Licking Valley and its South Fork. The continuation of this road, by either Pound Gal) or Cumber- land Gap, to the railway systemn of Eastern Tennessee and the xvalley of Virginia, is likely to be accomplished at an early dav. The Cincinnati Southern Railway, from the mouth of the Licking directly south to Chattanooga, will'be completed during the present year, and afford an admirably built road traversing the State on its longest south and north line, and crossing the Blue-grass lands on their longest and best sec- tion. Thi's road is likely to be of incalculable value to the State, forming as it does a main line to the South and South-east. The Lexcington and Big Sandy Railway is comrpleted, as far as Mount Sterling in 'Montgomnery County. This road when finished will give Kentucky cheaper and more direct communication, by -way of the Chesapeake and Ohio Rail- road, with the Atlantic ports. The Mlount Sterling coal- road. now almost completed, extends from the latter place to the border If the eastern coal-field, in 'Menifee County. The extension of this road will greatly facilitate the dlevelopment of the coal and iron region through which it is proposed to continue it. The Kentucky and Great Eastern Railway is a proposed road on which considerable work has been done; extendincg up the south bank of the Ohio River from Newport, Kentuckvy, 2S MARKETS AND TRANSPORTATION. to the Big Sandy River. The completion of this road xill add greatly to the wealth of riv-er line of counties, and xvill give the State a shorter road to the Atlantic ports than she now has. The Louisville, Frankfort, and Lexington Railroad extends through the Counties of Jefferson, Oldcham, Shelbv, Franklin, alid Fayette. Fronm Lagrange in Oldham County a branch extends from this road to Cincinnati, known as the Louisville and Cincinnati short line,-tthat line, passing throughl the counties of Oldham, Henry, Grant, Carroll, Gallatin, ]3oone, and Kenton. The Cumberland and Ohio Railroad, narrow--guagye, noxv building, when completed, will pass throug(h the counties of Henry, Shelby, Spencer, Nelson, WVashington, MAarion, Tay- lor, Green, .Metcalf, Barren, and Allen. Its length in Ken- tucky will be I65 m-niles. Thie Louisville and Nashville Railroad extends, with its branches, a distance of 356.4 miles through Kentucky in different directions. The IMain Stem, froom Louisville to Nashville, has a length within the limits of the State of I 39.6 miles, running through the counties of Jefferson, Bullitt, Nel- son, Har-dini, Laulle, Hart, Ednmonson, Barren, Warren, and Simpson. The iMemphis Branch runs through the counties of XVarren, Logan, and Todd, having a length in the State of 46 miles. The Lebanon Branch extends into South- eastern Kentucky, running, througih the counties of Nelson, Marion, Boyle, Lincoln, and Rockcastle; it has a completed length within the State o- IO9.9 miles, and its extension to the State line is projected, and its completion only a matter of time ; it will then connect wvith a road leading to Knoxville in the State of Tennessee. The Richmond Branch runs through the counties of Lincoln, Garrard, and Madison for 33.4 miles, to within a short distarLce of the rich iron region cf Ken- tuckv. The Bardstown Branch runs through the county of Nelson, a distance of 17.3 miles. The Glasgow Branch, 10.2 miles long, runs to Glasgow, the county-seat of Barren County. The Louisville and Nashville Railroad is undeniably one of the most important thoroughfares of this continent ; it is second only to the 'Mississippi River as a way for the com- 29 GENERAL ACCOUNT OF KENTUCKY. inerce betwveen the Northern and Southern States. By means of the mlctagnificent railway bridge over the Ohio River at Louisville it connects with all the great northern roads, and at Nashville and TMemphis, its southern termini, it connects with all the important roads of the South. The Louisville, Paducab, and South-western Railroad ex- tends from Louisville to Paducah, a flourishing city situated on the banks of the Ohio River, fifty miles from its jullCtiOnl wvith the Mississippi, and is the principal market-town of West- ern Kentucky. This railroad penetrates Western Kentucky in such a mlanner, therefore, as to afford easy access to a large lortion of that section. It runs through the counties of Harclin, Grayson, Ohio, Mluhlenberlg, Hopkins, Caldwell, L-ons, Livingstone, Marshall, and McCracken. It passes directly tlkroughi that section of the valuable coal-fields of Western Kentucky which lies within the area of the counties of Ohio, _Muhlenberg. Hopkins, and Grayson. The entire length of the Louisville, Paducah, and South-western Rail- road is 2`5 miles, all of which is within the territory of Kentucky. The Paducah and MIemphis Railroad runs through the counties of McCrack-en and Graves, connecting at Memphis all of the south-western railroads. The Owensboro, Russelville, and Nashville Railroad is completed from Owensboro, on the Ohio River, to Owens- boro Junction on the Louisville, Paducah, and South-western Railroad, passing through the counties of Daviess, McLean, and Mut1.hlenburg. Ihle Evansville, Henderson, and Nashville Railroad, from Henderson onl the Ohio River to Nashville, Tenn., passes through the counties of Henderson, Webster, Hopkins, Chris- tian, and Todd. At Henderson a ferry takes cars to the north- ern system of roads. It forms the most important link in a great trunk line known as the St. Louis and South-eastern Railwoay. The New Orleans, St. Louis, and Cairo Railroad passes through the counties of Ballard and Hickman. The i\Iobile and Ohio Railroad, connecting the city of Mobile on the Gulf of Mexico with the Ohio River, penetrates Kentucky through the counties of Hickman and Fulton. 1o MARKETS AND TRAN-SPORTATION. At Columbus, in Hickman County, a ferry fitted for the carriage of trains gives paassage to cars from St. Louis directly throughl to the south-eastern cities. Of the ten before de- sc ribed north and south rail way-s, four have northern con- nections; two (the Cumberland and Ohio and the Cincinnati Southern), now under construction, will have southern con- nections. The others all look to the same end, but have not yet succeeded in accomplishing it. It is in roads with eastern connections that the State lacks most. There is not yet a single railway crossing the eastern line of the State. It is tlo this difficulty of access from the seaward that the State owes the small share it has had in the immig-ation of capital and labor that has filled the lands of less attractive regions. Three routes have been begun, which, when complete, will fully remedy this grave defect; namely, a road from Louisville to the south-east via Cumberland Gal), completed to Livingston, and requiring a continuation of about one hundred miles to connect with roads leading from lIorristown, Tenn., to Charleston, S. C.; a road from Mount Sterling to Abingdon, Va., via Pound Gap, requir- ing about one hundred and sixty miles of road to complete the connection; a road from Lexington to connect with the Chesapeake and Ohio, requiring about eighty miles to bring it to completion. The northernmost and southernm-nost of these roads are likely to be carried forward to completion within a few years. There is a project for building up, east and west, a road along the northern range of counties of the State, giving a continuous route from Henderson, and the roads connecting at that point, to the connections with Charleston and Savannah from M\Iorristown, Tenn.; also a project for a road from Chicago to Charleston, crossing Ken- tucky from Gallatin County to Cumberland Gap. It will be seen from this brief sketch that the railway svs- tern of Kentucky is on the whole good, and wants but little to make it, as a system of tr-unk lines, exceedingly well adapted to the development of her resources. Taken in connection wvith the river system, it is clear that, xvithin a generation, we may expect here a transportation system excelled by no State on the continent. 31 GENERAL ACCOUNT OF KENTUCKY. W\ith reference to markets, it will be seen, by consultinag the census tables, that the State has at present access to a larger nullber of markets than any other Western State: although there is but one large city within her limits, the cities of Cincinnati, St. Louis, Nashville, and Indianapolis lie upon her borders. Her principal export products have a special value that makes them souaht on her own soil by purchasers enough to take any product that can be furnished ; on the borders of the State, a ]lost of manufacturing towns are rising fhat will certainly milake a market for all the food, fuel, and raw products from her soil, quarries, and mines. PRICE OF LANDS. In no other State having any thing like the same advan- tages can lands be bought at so low a price. The best agricultural lands, or those commanding the highest price, are found in the Limestone regions and along the principal rivers; these, when cleared and not worn, bring from thirty to one hundred dollars per ac re. The same, uncleared, will be about half these rates. The second-rate lands in the same regions brirg from ten to forty dollars per acre. The lands on the coal-bearing beds, though often exceedingly fertile, are generall X very cheap. MVien contiguous to transportation they may generally be estimated at about ten dollars per acre, but the tracts of good tobacco lands, with excellent timbering and great mineral resources, can often be purclhasedl for twvo to four dollars per acre in tracts suitable for ordinary farming within ready access of permanent transportation. Vast tracts of timber land, suitable for grazing, With much excellent land in the coves, or other level places, can be bought for from fifty cents to one dollar and a half per acre. As a general thing. it may be said that the lands in this State are much cheaper than in any State north of the Ohio River. This is owing to the fact that, destitute of eastern communication, the State has hitherto had but a small share of the tide o&- immigration of capital and labor that has poured past her borders to fill the favored fields of the far West. Nearly all the products of Kentucky have their prices " 2 PRICE OF LANDS. determiined by the cost of transportation to the great centres of population aloneg the Atlantic seaboard or beyond the sea. Its tobacco, pork, grain, and some of the costlier na- tive woods, and some other products find their principal markets in Europe; cattle, and to a certain extent the other agricultural products of the State, have their values deter- miled by the cost of transportation to the American At- lantic markets. Hitherto., this access to the domestic and forceign markets of the Atlantic shores has been had lv way of the railw ay systems which traverse the region north of Kenltucky, and from which the State has been divided by op- posing interests and the physical barrier of the Ohio River. All the development of the State has taken place under these disaadvantages. A comparison of the tables of cost given below will show that the comnplete opening of the mouth of the .Mis- sissippi to occean ships will result in the enfranchisement of the productions of Kentucky in an extraordinary way. At the present time, the freight-rates from the lower Ohio to Liver- pool would permit the profitable shipment of the cannel coal "The following are taken from published freight-rates, and give time and cost of transit from St. Paul's, two thousand miles above New Orleans, to Liverpool by the two routes:- Cost per b-hel. Tihm. Cents. Days. From St. Paul's to Chicago.. . . . . . . 4 Lake from Chicago to Buffalo.. . . . . . 6 Canal from Buffalo to New York . . . 14 24t New York to Liverpool.. . . . . . . . i6 I2 Elevator or trans-shipment charges, Chicao . 2 2 ,, Buffalo. 2 2 New York 4 2 Total. . . . . . . . . . . . 64 52 Cost per b,,shel. T'm,. Cents. Days. From St. Paul's to Newv Orleans (via river) . . iS I0 New Orleans to Liverpocl... . . . . . 20 20 Elevator charges, New Orleans.. . . . . 2 1 Total.40 31 Here is a saving by direct trade of twenty-four cents per bushel, or eighlt shil- lings per quarter, and a saving of twenty-one days in time. To be fa r, I have taken the extreme point: butt the ,,earer tde grazin is to the Gzdf,; tdie cheaper the tra ,zzspor-taz don. ' ; GENERAL ACCOUNT OF KENTUCKY. and native woods of many different species to Europe with one trans-shipment at New Orleans. It is impossible, on account of limited space, to give a detailed statement on this point; but evidence cani be furnished to those desiring it. It is to be no- ticed that il. is possible for several months each year to bring ships of large draught of water to the loading points on the Ohio River, and load them for direct trade with Europe. The tonnage of such vessels both ways from New Orleans would be at the lowest rates for such work current in any region. It will be seen that the State of Kentucky has the most exten- sive shore on the navigable waters of the Mississippi Valley, and that even in the present incomplete development of her navigation system she will have over fifteen hundred miles of frontage on continuously navigable waters. There can be no doubt that the market expenses of the products of the State wsill be reduced nearly one-half when the far-reaching conse- quences of the development of water-transportation are at- tained. It will not be amiss to notice that the costs of trans- portation by water, far lower than by rail in most countries, is peculiarlY cheap on the Mississippi and its principal tributa- ries; coal is lower than in any other country, as is also timber for boat-building; there are no tolls on the streams, and the currents are generally slow near the shores, admitting of toler- ably easy ascent. FITNESS FOR INVESTMENTS OF CAPITAL AND LABOR. For all the important branches of agriculture and manufact- ure, so far as the) depend on cheap and fertile soils, good climate, and a great abundance and low price of coal, iron, and hiard-wood timber, and last, but not least, low taxation, - Kentuckv offers unsurpassed advantages for the creation of industries. It will be impossible to name these opportunities in detail, but some of the most important may be suggested. The growing in- dustries of the Oh1io-River Valley and the neighboring regions offer continued opportunities for the increase in the export of the raw products of the State. Coal, iron, salt, timber, cements, building-stones, can all be produced at great profits, even in the present depressed state of the industries of the 34 INVESTMENTS OF CAPITAL AND LABOR. world. The Ohio Valley probably gains in population at an average rate of not less than five per cent. per annum. This (great elasticity of demand insures a successful result in any cliscreet industrial venture. Besides the coal and iron mines, the attention of capitalists is requested to the production of other articles of equally steady demand. Salt can be produced over a large area at the cheapest possible rate,- the water hardly reqluirint, uLmp1ing from the shallow Xells, and the gas furn'isl- ing luel. The great amount of fire-clays should be considered. The tile-clays are admirable in quantity and quality. An area of several thousand square miles in the State is rich in marls, containing large quantities of potash and soda, fitted for the production of fertilizers. The western section of the State is admirably fitted for ship-building; excellent ship-timber can be had cheaper than in any other country, and there is ampule water to take ships drawing twenty feet to the sea for half the year-. Besides the enormous possibilities of business derived from the xvorking of raw products, finding their market in the great and growing States of the Mississippi Valley, there are most important opportunities derived from its relation to the regions beyond the sea. The natural outlet to the Atlantic ports for these products is by way of the Mississippi to the sea. The freights from Western Kentucky to New Orleans are less than one-half of the rate from the same region directly to New York. Until the success of the Eades-Jetty project, this method of carriage to the sea was practically impossible. At present it is practicable to load timber-ships and coliers at the l)orts from the western coal-field, and send them directly to the Atlantic ports, or to any markets beyond the sea. Al- ready a large trade in wvine-cask staves exists between this reoion and Europe. These staves pass through six hands be- fore com-inig to the consumer. These exchanges could be readily reduced to three by direct shipment. The demand seems to be practically inexhaustible, and the timber exists in very' great quantities. To this industry there could be readily added a business in the manufacture and shipment of spokes, felloes, and other carriage-parts, the parts of railway-carriages, agricul- tural implements, &c. Building-stones of admirable qcuality 35 GENERAL ACCOUNT OF KENTUCKV. exist all alcng the tributaries of the Ohio, and their export to the Atlantic ports is already a considerable commerce. As will be seen from the accompanying map, the State of Kentucky lies, as a region of peculiar mineral resources, in the centre of thl2 region now holding, and destined always to hold, the mass cf American population. The present centre of population is adjacent to the northern border of Kentucky, and it is practically certain that in centuries to come it must re- main within or on the borders of Kentucky. This makes it sure that manUfactures will from this region always command the widest markets with the least carriage. The advantages of this district to the agriculturist are known by tlie c heap land, good cli inate, and abundant variety of crops. T1hese crops are near to a great and growing set of markets. Amlonog the new ventures in agriculture must be placed fruit-culture for the northern markets, -a business that is now taking a very important place in the industries of the State. The poorer lands of the southern part of the State have a peculiar fitness for this purpose. The followving table, compiled from the United States cen- sus report, proves that Kentucky is susceptible of a greater varietv of production than any other State. It will be ob- served that it is in each census the first State in the production of some one or more staple articles: - 1840. is -O. i86o. 1 S70. Wheat . . . . . . . . First. Ninth. Ninth. Eirhtth. Swine . . . . . . . . Second. Second. Fourth. Filth.II Mules . . . . . . . . Second. Second. 1 bird. Indian Corn. . . . . . Second. First. Sixt!;. Tobacco . . . . . . . Second. Second. Second. F irst. Flax. . . . . . . . . Third. First. Third. Ei-lhth. Rye . . . . . . . . . Fourth. Fifth. Fifth. Hemp . ... . First. First. First. Cott(n. . .. .. Eleventh. Twvelfth. Value of Home Manufactures Third. Second. T hird. I In 1570 K-uckv proeduiced near one-ha]f of all the tobacco Irodiced in the United States. I and ,ore th-ti h'It ofall the Hempl. The production of Tobacco increased from 1o5,305,iofIds I i n 1370, to 15i, 1 ...29 po..nds in 187.3. The high rank of Kentucky as an agricultural State can best be appreciated when it is remembered that more than one- 36 INVESTMENTS OF CAPITAL AND LABOR. half of the State is in forest, and that the State is only exceeded in area of woodland by three States. Yet, with less than half the land in cultivation, the State ranks eighth in the value of agricultural products. Building and ofzer Economzic Sloncs.- The building-stones of this State are limited to Limestones and Sandstones. Within these limits, however, there is a most abundant variety of color, hardness, and other qualities. The Limestones of the Upper Cambrian, or so-called Lower Silurian, are excellent stones of exceeclingly varied qualities. Usually they afford a gray mjar- ble of admirable resisting powers against wear, especially fitted for buildings when their courses of rocks are suitable. Along the Kentucky River this series of rocks affords a beau- tifull buff and cream-colored marble, admirably fitted for detailed sculpture work, the Clay Monument at Lexington being made of this stone. This stone can be quarried on the banks of the river in any quantity and at small expense, and transported by boat to the Ohio River. Next above this level wxle have the equiv- alent of a part of the cliff-limestone of Ohio, which has received the local name of Cumberland Sandstone in the Kentucky re- ports. This Sandstone is thin, and passes into a chertv Limie- stone in the northern part of the State ; but in the basin of the Cumberland it is of a peculiar greenish color, affording a very handsome and durable building-stone, resembling in many re- gards the Buena Vista Sandstone of Ohio. This stone will doubtless have considerable value in the time to come, as it is peculiar in its color among all the building-stones of the Ohio Valley. No other good building-stones occur until, after pass- ing above the Black Shale, we come to the beds of Sandstone of the Waverlv period. The beds of this section afford the only Sandstones of the State that have been extensively worked for building purposes. These beds, commonly known as Buena Vista stone, are the only source of the Sandstones used in Cin- cinnati and Louisville, and in most of the other western cities. At present they are worked along the Ohio and soulth-east of Mount Sterling in Montgomery County; but they can be had where the Licking, Kentucky, Salt, and Green Rivers cross the Waverly, and at the points where the railroads of the State Iass over the same formation. 3 7 GENERAL ACCOUNT OF KENTUCKY. 3 It is, however, in the Subcarboniferous or MIountain Lime- stone that the greatest variety and area of econonmic stones OCCur. Here we have Limestones (carbonates) which are the finest known in this country; Oblites ,which, for beauty of grain and endurance of time and other forms of wvear, are uLn- surpassed; Dolomites that have all the fine qualities belonging to those MIaLgnesian Limestones; and, finally, a series of more or less Argillaceous Limestones, some of which are already in use as lithographic stones, and promise good results. These Odlites have, been in use for forty years in the town of Bowling Green, and retain all their tool-marks as when dressed, having hardened very much since their working. Stones for furnace- hearths abound throughout the whole mineral district. Some millstones l ave been worked for local purposes, but have had no extensive test. Grindstones are made from the XVaverly Sandstone, which is admirably fitted for this use. Some good grindstones have been made from the Carboniferous Sand- stones of Western Kentucky. GOVERNMENT, POPTULATION, TAXES, EDUCATION, FUTURE. The govcrnment of Kentucky is at present modelled in part on that of New York, and in part on that of Virinia, -the legal framewAdork being essentially that of the former State. The legislative machinery differs somewhat from that of the other States, in that the senate is re-elected one-half each two years, while the lower house is simply renewed each two years by election. There is no actual State debt, - the schaool-fund debt being such only in a ppea1-ance, in fact only an obligation to pay a certain sum for the support of schools. No State debt can conlstituLtionally be contracted, and during the last ten years, while other States have been steadily increasing their obligations, Kentucky ]has paid off the debt which was left by the war, and now is debtless, and with considerable assets. The last legislature (1876) reduced the taxes by one-eighth, after a careful inquiry going to show that it could be done with safety. The following statement summarizes the condi- tion of the State in I875:- EDUCATION. " It will thus be seen, that in the last two y7ears we have redeemed and paid off 347,000 of the public debt, and there now only remains of bonds outstanding and unredeemed 184,394. The residue of these bonds are not due and redeemable until :;894-5-6." To meet this indebtedness we had, on the ioth of October, 1875, the end of the fiscal year, - To the credit of the Sinking Fund . .13,559.07 230 United States 5-20 gcld-bearing interest bonds, worth not less than 20 per cent. premium . . . 246.ooo0o0 Making.. . . . . . . . . . . . 399,39.07 The whlole traditions o:L the State are strongly in favor of economy and honesty in every branch of public affairs. No loss by defalcation has ever occurred to the State. Debts cannot be incurred by counties, cities, or towns without special authority from the legislature. This permission is now given only in rather rare cases, and is subject to great limitations from the organic law. The result of these conditions is an immunity from the danger of destructive taxation, such as does not exist in any other State in this country. Etduca/joit. -The State now gives from the general treas- ury the sum of one million dollars to the purpose of common school education ; this is, per capita, as large a contribution from the general fund as is given in any State; as yet, this has been inadequately supplemented by local aid, but much progress is now making towards the creation of graded schools in every village where the population admits of it. The laws allow the imposition of a considerable local tax for schools. There is no State with an equally scattered population where so much has been done for the elementary education. Universities and colleges have never received the aid of the State. There are, however, a number of excellent institutions of this grade in the State. The first collegiate institution west of the Alleghanies was Transvlvania University, at Lexington. Kentucky University, Georgetown College, Centre College, and a number of other similar schools of newer date, many of In a report made by the State Treasurer, January, 1876, the State debt was shown to have been much less than the above, and the surplus in the Treasury had increased to near one million of dollars. This report will appear in next edition of this pamphlet. 39 GENERAL ACCOUNT OF KENTUCKY. them excellent in their methods, and provided with considera- ble endowmn-ents, furnish the higher education of the State. The cha:-itable institutions, nominally so called, are suffi- ciently furnished by the State. A very high place is held by the aslumis for the deaf and dumb and for the feeble-minded, in both of which recognized advances have been made in the methods of dealing with these forms of human infirmity. It remains to speak of the most important element in the State, its population. Probably no other State in this Union contains a people as purely English in descent as this. At this date (1876) the population numbers i,6oo,ooo; of these Onlly 200,000 are of African descent, or about one-eighth of the total. There is a steady decrease in the black population, and an equally steady increase of the white, so that the negro now makes but an inconsiderable fraction of the State; by far the greater part of the blacks are gathered about the towns in lig-lt labor of the domestic class. The relations be- txveen the two races are those of entire harmony. Separate schools are founded for the two races. In I80o, the foreign-born population in Kentucky amounted to 63,398 (is probably at the present time less than iooooo); of these 3 1,767 were Germans, and the remainder from various other Europzan countries. The greater part of this foreign population is settled along the Ohio River, but it exists in almost every county. The honest and self-supporting citizen of every country has always received a warm welcome in Kenltuckzy; no jealousy has ever showsn itself towards the foreigner. The government of the State has for years always had a number of Conspicuous members from beyond the sea; one of the United States senators and several of the members of the legislature are also from other countries. Without indulgence in excessive claims, which would be quite foreign to the sober tone of this Commonwvealth, we may reasonably expect for Kentucky, in the time to come, a substantial growth proportioned to her natural advantages. As at the present moment, when the country generally is under In 1790, Kentucky was the fourteenth State in population, having a population of 73,677. In 187o, Kentucky wvas the eighth State in population, having 1,321,01I 40 FUTURE. a heavy burden, the result of its commercial extravagances, the State of Kentucky is actually prosperous in a fair degree, so we may expect in the future a consistent and conservative progress that wvill not be attended by those periods of commercial depres- sion that so generally accompany a growth of an excessive kind. The unequalled blessings of the Ohio Valley, its wealth of mineral stores, fertility cf soil, goodness of climate, and fa- cilities for transportation, are all shared in large measure by Kentucky. Another century will doubtless see this Valley the greatest seat of those predictions that require cheap power and cheap food for their making, bringing a population equal to that of the equal areas in the great European States; when this comes, this Commonwealthl will contain within her borders probably not less than eight millions of people, and sources of wealth and power unsurpassed on this continent. 6 41 Plat&eNo. 1. 440f 01fo VAINYI F NN'iOAI2A9m VAu" 01 : 'Ni.SM f' IN9 0 _4Tt X W. z / TIICXNN I = _iI V ON ff00:efI)wr1 ::: OX D Cf l T0 If & art L A W 'NC: :0 S0 0f: :X :0 ff:X f:00::0 iX0CO U 'N1:I ' S.\ ;t; 0 00 - \ aa 0:00:: A ; f0ff::0 'i.N0t: :\ X: : u : : ::::: : :OA : 1::O : : : : :: O j:'4:[ :;0 X f 1S : : 0 : : :: : Si: : t = . V C : : : :: ::S&S IK 0X -; V 0; COA NO : : I'I':: N':: 0: :fi: IN AT .M :f 'ii : 4 4 41 I P j K 44 4 _ I: '' +I...... ,I-;1 1, i_ ---g 7 I I ro OF W A V N ,I I L'u 4-K 011 .t t 0 ; tSANO41tOSf COALt illork 0444t: St0 C: AL N t 1 :; :) I I IatF 4444;4 :: : : : 0:::: ;::: :: :: 0 : : : f::: :: :::: 7, :g:f : :: CON0:t :0fXA li1t [0 0444 ,4 4 14 4 0 X '114414444 TO 11c.[ONOL. 9A. N i4 0 I'll: w w = I I a I I I I 4 11 :I s 7.Kil2 BRIEF STATEMENT OF THE ECONOMIC GEOLOGY OF THE BIG-SAN-DY VALLEY. TtiE valley of the Chatterawah or Big-Sandy River is entirely within the limit of the coal-measures, and, with perhaps one or two exceptions, where the Subcarboniferous Limestone is brought to the surface, the rocks exposed on the waters of the Big Sandy are those of the coal-measures proper. Thie number of distinct beds of coal known to be present in this valley is twelve. Iron ores are found at about an equal number of levels. The accompanying general section, from report of A. R. Crandall on the geology of Greenup, Carter, Boyd, and Lawrence Counties, shows the order of the beds, both of coal and of iron ore, near the Ohio River. Further southward changes occur in the general character of the rocks above coal No. 3, so changing the general section as to render any identification of beds from the little that is now known of themii quite untrustworthy. Fuller investigation will doubtless discover most of the coals as found near the Ohio, and the thickening- of beds as found southward gives promise of richer fields than those already developed. The following table shows the thickness of the beds that have been fully identified as seen in the localities where mined - Miininim . Maximum. Coal, No. r. 3 ft- o in. 5 ft. o in. ,,2. 2,, 0, 3 ,,8,, 3- 2,, 6,, 6,, 6,, 4- 2 ,, 0 ,, 4 ,, 6 ,, ,,5. 3,, 6,, 9,, 0,, ,, ., 6. 3,, 0,, 4,, 0,, , 7. 3 ,.0 ,, 6 ,, o,, 8. 2,, 6,, 8,, a,, ,, ,, 9. 2 ,!0 2, 2d6,, ,,lo. 3,, 6,, ;; I. 2 0 2 6 , _[2. Coal 5 is generally slaty in part where found in great thickness. t Not opened. ECONOMIC GEOLOGY OF BIG-SANDY VALLEY. The followving table of analyses of samples, taken from the whole thickness of beds as mined, will serve to indicate the character of the beds included, and of the coals of this field generally: No. x. No. 2. No. 3. No. 4. No. 5. No. 6. No. 7. No. s. I- .o , . I_-C SpecificGravity. . 1.267 1.289' 1.3171 1.306 1.36o 1.279 1.320 1.367 Moisture. . . . 2.50 4.10 3.26 1-50 3.20 2.94 5 00 3-50 Volatile Com. Mat. 136.00 34.60 34.22 .52.20 32.30 32.50 34 50 31-90 Fixed Carbon . . 57.30 55.25. -5536 40.6o 53.00 56.76 55.40 52.o6 Ash. . . . . . l 2.90 4.77 7.16 5-70 I11.507-74 5.10 12.50 Sulphur . . . . 1.148 1.414 0.901 0.7821.9991-972' 1.28S0.873 Coal No. 8, as represented in this table, is from the head of Nat's Creek, in the north-eastern corner of Johnson County, where it is fully eight feet in thickness, with slight partings. The only average sample from this locality was necessarily taken from near the outcrop, giving too large a percentage of ash, and probably too small a percentage of sulphur. The thickness of the measures, which include the coals of this table, is about four hundred feet in the regions best known. Coal No. I is exposed along the Big Sandy, south- ward from Peach Orchard and Warfield, at a level which is in general slightly above high-water mark. The hills along the river and the main creeks rise to the height of six and seven hundred feet, including the equivalents of the accompanying general section from coal No. i upward. What beds are pres- ent in these hills is yet to be ascertained. 44 GENERAL RESOURCES OF THE WESTERN COAL-FIELD AND BORDERING TEERRITORY. I. SUBCARBONIFEROUS BEDS. THE coal-field is bordered by Subcarboniferous beds, which are, in succession, those forming the Chester group, and those included in the St. Louis group. The Chester series are rich in stores of potash-marls, while the St. Louis group yields a number of beds of very admirable building-material. It is also in the region underlaid by the Subcarboniferous beds that the excellent Limonite iron-ore, so highly esteemed by iron -manufacturers, is found. As the group is of especial interest, the following typical section of the Chester group, as it occurs on the eastern out- skirts of the coal-field, is given No. i. Shale, with thin beds of Limestone 2. Heavv-hedded, cherty Limestone . 3. Red and green Shale. 4. Rhornboiclally-jointed Sandstone, frequently char Brachiopoda. 5. Limestones.t ........... 6. Shale ........ ....... 7. Limestone and Shale. 8. Green, red, purple, and blue, marly S hales ; the Li marls 9. Shale and thin-bedded Limestone. io. Shaley Sandstone . i i. Heavy-bedded, dark-gray, and blue Limestone 12. Massive Sandstone; the "bi--cliftv" Sandstone 1t, .. I5 fe( I3 ,) . . . 51 ed with . .0 tO 10 2,, . . IO ,, . . 20 , tchfield 25 to 6o ,, . . . 5 ,, 0 to 20 ,, 5 to 45, .6o tq 130 ,, et. Described in detail in Part VT., Vol. I., Second Series Kentucky Geological Reports. N. S. Shaler, Director. GEN,'E RAL RESOURCES OF WESTERN COAL-FIELD. This section is frequently modified. The economic values of the different beds are dependent, in a measure, on their per- sistenc. Space forbids any detailed discussion of the ques- tion here. It may be remarked, however, that none of the beds are found to be trustworthy over large areas, unless it be the marls. The persistency of the marls, however, as i'idi- vi/dal beds, is not a settled question. Thie strata are ex- ceedingly variable in their lithological features, and lateral Changes are very frequent, both in their composition and thickness. It is not uncommon for Limestone or Sandstone- beds to be, either in whole or in ltart, replaced by Shales. Hence beds occurring at some certain locality that would, from their color and composition, be referred to the horizon of the Leitchfield marls, may really belong at a lower or higher level, having replaced som-e more solid bed. This, however, docs not militate against the fact that the Leitchfield marls proper extend over a great area. The St. Louis group is distinctly separated by the physical characters of its strata into two divisions. The upper or gray Limestone division is formed of a series of gray and drab beds, among ws hich are included two well-marked varieties. One variety, a white Oblite, is quite characteristic of the divi- Sion. Usually associated with the Odlite are beds of dense drab to cream-colored stone, which breaks with a smooth, conchoidal fracture, and resembles lithographic stone. The upper divrision furnishes some of the best building- stones and materials for lime that are to be found in the State. The lower division includes beds of dark-blue to bluish-gray Limestone. The rock is frequently fetid from carbonaceous matter, such as bitumen, held in it, and nests of massive calcite and fluor spar are not infrequent in it. The study of this group is especially interesting on account of its being the repository of the lead deposits of Western Kentucky. A section of the beds formin- the group, and other matters concerning it, will be found in Part VI., Vol. I., Second Series Kentucky Geological Reports. N. S. Shaler, Director. 46 TILE COAL-FIELD. II. TH E COAL-FIELD. IN studying the resources of the area occupied by the Carboniferous beds in Western Kentucky, the greatest inter- est naturally belongs to that section underlaid by the coal- measures. In form the coal-field is somewhat basin-like; that is, the beds incline from the margins towards the centre. The border of the field has never been completely traced -with accuracy; but its course may be approximately delineated as follows: Commencing at the Ohio River, in Crittenden County, it follows up the valley of the Tradewater River into Caldwell County; thence crossing into Clhristian County at a point about five or six miles above Tradewater station (on the Louisville, Pacudah, and South-western Railroad), it keeps in a south of easterly course towards the head-waters of the Pond River. From a point about two and a half or three miles south of Petersburg, Christian County, the southern boundary makes a south-eastwardly curve, passing by the head-waters of the Pond River to the Muddy River, which stream it crosses somewhere near its forks. Thence it passes through the southern part of Butler County, crossing Barren River below the mouth of Gasper River, thence eastwardly along the divide between those rivers, crossing Green River above the mouth of Nolin River, and extending north-eastward to the head-waters of Casey Creek in Hart County. Thence it curves to the north-west, crossing Nolin River near the mouth of Dog Creek; passing a point between MNillwood and Leitch- field in Grayson County,-an outlier or tongue extending north-eastwardly, on the north side of Nolin River to the These outlines have been mainly obtained from Vol. 1. Kentucky Geological Reports, First Series; D. D. Owen, Director. They are quite imperfect, so far as regards details, but are sufficiently accurate for present general purposes. The faithful delineation of the outline of the coal-field has been made part of the work of the present survey. 47 GENERAL RESOURCES OF WESTERN COAL-FIELD. head-waters of Hunting Fork, of Rock Creek, - and thence on to the Ohio River, to a point not far below Cloverport in Breckenridge County. In the space thus included lie the whole of nine counties, and parts of five more, making an approximate total of nearly four thousand square miles for the area of the coal-field. Tue Nuvzibcr of Coal-bcl as, &c. - Twelve coal-beds have been identified in the space between the Conglomerate (the base of the coal-measures) and the summit of the series. It is believed as not improbable, however, for reasons un- necessary tc discuss here, that, when sufficient data have been gathered to warrant a Generalization concerning the number of beds, it will be found expedient to designate a less number of coals in the general section for the coal-field. For the present, therefore, a letter is used to designtate each bed. The results of the work of the Survey, so far, point to eight as the number of beds that may prove sufficiently trust- wortlhy to receive final numbers. Tlhe total thickness of the coal-measures is as yet only approximately known. The thickness is variable, as is the number of coal-beds, and is greater at some localities than at others. It does not seem probable, however, that it will anywhere exceed one thousand (I.ooo) feet, and there are districts in which it is less than eight hundred (Soo) feet. On the map of Kentucky will be found a section showing the position and number of these coals as determined by Dr. Owen's Survey, as well as some modifications made by the present Survey. The thickness indicated for each bed, and the included space, are strictly in accordance with Dr. OwNen's statement. i. Anvil Rock Sandstone... . . . . 20 feet. 2. Coal, No. 12 (Coal A')... . . . . 3 3.Space. ... . . . . . . . . . . 21 4. Coal, No. ii (Coal B)... . . . . 5. 5. Space.. ... 46 6. Coal No. io (Coal C).. . . . . . 3 7. Space........ . .... 68 8. Coal No. 9 (Coal D)... . . . . . 5 9. Space.. . . . . . . . . . . . 50 NUMBER OF COAL-BEDS. 49 io. Coal No. 8 (Coal E).. . . . . . . 2L feet. i i.Space. . . . . . . . . . . . . 43 I2. Coal No. 7 (Coal F ).. . . . . . 2 I3. Space..... 84 I4. Coal No. 6 (Coal G). . . . . . . ,, 15. Space . . . . . . . . . . . . 65 i6. Coal No. 5 (Coal H ).. . . . . . 4 , 17.Space. . . . . . . . . . . . . 95 i8. Coal No. 4 (Coal I).. . . . . . . 4 I 9.Space . . . . . . . . . . . . 154 20. Coal No. 3 (Coal J).. . . . . . . 2 ,, 21.Space. . . . . . . . . . . . . 71 22. Coal No. 2 (Coal K) No thickness given. 23. Space. .... ... ... 82 24. Coal No. i B (Coal L).. . . . . . 5 The preliminary arrangement adopted in the present sur- vey differs in some particulars from the foregoing. In some instances the distances between the coals are increased, and in others diminished ; and several of the beds are represented at a (reater or smaller thickness than they are in Dr. Owen's Section. The irregular distribution of the coal necessitated the separation of that part of the coal-field thus far examined into three divisions. The first extends from the eastern border of the field to the Green River; the second is approximately bounded by the Green and Pond Rivers; and the third ex- tends from the Pond River to the western margin of the field. In the first division are found coals A, B, C, D, E, H, K, and L; proving eight of the twelve beds to be present. In the second division are found coals A, B, C, D, E, F, G, and H ; the number here also being eight. This, how- ever, does not represent all of the coals that may be found, as the base of the coal-measures was not reached; it repre- sents only those coals that come to the surface, or that have been reached in pits; no doubt, most of the lower beds are present. The region in question is that which is traversed by the Louisville, Paducah, and South-western railroad: none of the couintry bordering the Ohio River is in- cluled; nor yet that lying near the southern maroin of the field. None of that re-ion has yet been sufficiently studied to report on the number of beds. See Part VI. Vol. L., Second Series Kcntucky G;eological Reports, page 374. 7 GENERAL RESOURCES OF WESTERN COAL-FIELD. In the third division most of the coals are found, the absent ones probably being C, F, G, and K ('). Generalizing from the results obtained in each of these divisions, it is found that the average distances between the coals from A, to H about as follows: i. Coal A 2. S pace 3. Coal B 4. Space 5. Coal C 6. Space 7. Coal D. S. Space 9. Coal E I0. Space i i. Coal F 1 2. Space I3. Coal G 14. Sp ace I5. C oal H inclusive, in the region examined, are . . . . . . . . . . . . . . . . . . . . . . . . 5 feet. 5 .............6,, I5 20 -- - - 75 ,, 50 ......... -75 20 , .........../5,, 100 ,, 4/2 From coal H to coal L the spaces between the beds are very variable, and sufficient data have not been obtained to warrant the making of an average. As an instance of the changes, it may be mentioned that the distance from coal I to coal J varies from fifty to eighty-three feet. Were all of the coals united in one bed, the deposit would be about thirty-five feet thick. As far as our examinations now show, coals K, G, F, E, and C may prove to be only local beds. Quality of the Coals. - As a consequence of the very imperfect knowledge hitherto had concerning the coals of this field, the percentage of sulphur in the coals of Western Kentucky has been rated by many not only as inordinately high, but greater than in the coals of neighboring regions. Thin has been an error. It is true that in some of the beds the percentage of sulphur is large ; but as a class the coals will compare favorably with those in any section of the Western coal-field. The matter of sampling coals for a rep- resentative analysis has not always received the attention that shoulcl be given it; what may be termed " hand " or 50 QUALITY OF COALS. picked specimens have in the largest number of cases been used for analysis, and analyses made under such conditions cannot be fairly compared with ours, that were in every case made from samples mechanically taken and faithfully averaged. It has been known for some years that the coals of the WVestern coal-field carry, as a class, more sulphur than do those in the Appalachian field; and less than do those in the Missouri and Iowa coal-field. It is not, therefore, with the coals of the States in the Appalachian coal-field that the Western Kentucky beds are to be compared as a class, but with those in the West; and when such comparison is im- partially made, the Kentucky coals, as a class, are not excelled by those in other sections of the Western coal-field. In Indiana and Illinois there are certain beds that have wvon a high reputation, a better one indeed than has hitherto been accorded the Kentucky coals; but later investigations have developed the fact -hat here, too, are exceptional good beds, unexcelled, perhaps, by the most famous of those States. They have hitherto escaped general notice, from the fact that they do not lie in what has been the district of active mining operations, although within convenient reach of trans- portation facilities. Followving are averaged analyses of those beds which so far have been deemed the most important:- Nutmber of Coal. A. B. ). J. L. t Moisture.. . 3-43 3.27 3-37 3-70 4-81 3.3C 1.30 Vtflatile Comnb. Mat.39.2t 38.30 36.66 32.56 32.22 [ 36.Oc 59.60 Fixed Carbon . . 50.235I12351.97 50.04 5503 1 57.8 27.00 Ash . . . . . 7.o8 6.70 8.o 13.70 7.9 2.82 I2.10 100.00 [00.00 100.00 100.00 O00.00 100.00 100.00 Sulphulr.. . . 2.753 2.548 2.So6 3.716 1 373 1.024 1.896 Specific Gravity. 1.383 1-309 1-354 1.39S I-319 1.241 1.213 From the C,.altosn Baniks, Christian Countv. t From near Grit htsbtr, Mcl C mu tsy. t The' Breckenridge " Cannel Coal, from near Cloverport, Breckenridge County. Some of the beds as yet insufficiently studied for judgment to be passed on them may prove fully as important, so far as regards qulality, as those now wrought. 5 I 52 GENERAL RESOURCES OF WESTERN COAL-FIELD. For comparison with the analyses of coal L, the following analyses of the Indiana " block " coal, and the " Big Muddy" coal of Illinois are given. These coals are considered to be among the best in the Western coal-field: Number of Analysis. No. i. No. 2. No 3. No. 4. Moisture. . . . . .2.70 2.68 2 62 3-44 Volatile Combustible Matter. 36.33 36.32 32.04 3 r.86 Fixed Carbon.. . . . . 55.64 53-58 58.58 59 54 Ash. . . . . . . . . 5.28 7-42 6.76 5.i6 Sulphur.. . . . . . . I1664 .802 2.472 1.376 Specific Gravity... . . 1-313 not est. 1.310 1.310 Numbers i and 2 are analyses of the Indiana "block" coal; numbers 3 and 4, of the " Big 'Muddy" coal of Illinois. The analyses were made in the laboratory of the Kentucky Geological Survey of carefully averaged samples collected in the same manner that the Kentucky coals are sampled. Special attention is directed to the analyses of the Coaltown and Wrightsburg coals. These are what are known as "blocking" coals, and withstand weathering remarkably well. The Wrightsburg coal is remarkably good, containing less than three per cent. of ash, a small proportion of water, and but little more than one per cent. of sulphur. There is rea- son to hope that the XWrightsburg and Coaltown coal may prove serviceable as an iron-making fuel. The Breckenridge Cannel is already well known for its remarkable properties. Coal D seems to be the most trustworthy of all of the beds, and is the one most generally wrought throughout the coal- field. It is most useful as a household fuel. Coal B is usually divided about the middle by a clay part- ing. The upper sixteen inches serves admirably for gas- making; several analyses show it to contain very little sulphur, and a large proportion of volatile combustible mat- ters. At some points the coal yields an admirable coke. See page 177 of the Chemical Report of the Kentucky Geological Survey; Vol. I. Second Series. N. S. Shaler, Director. WATER-WAYS AND RAILWAYS. III. WATER-WAYS AND RAILWAYS. THE coal-field is crossed by three railroads, and is so drained by several streams that, were they all prepared for navigation (a work of no very serious difficulty), no part of it would suffer for means of transportation. All of the streams drain towards the Ohio River, which offers cheap transportation to the sea. Tfhe streams that have already been made navigable for part of their extent are the Green, the Tennessee, and the Cumber- land Rivers; those streams whose partial improvement is both feasible and desirable are the Tradewater and Pond Rivers, Rough Creek, Nolin River, Muddy River, and Bear Creek. The Green River and its tributaries is navigable by locks and damns for two hundred and sixty-eight miles. The Ten- nessee is navigable from its mouth to Florence, Alabama, a distance of about two hundred and fifty miles; and the Cum- berland River is navigable from its mouth to a point about one hundred miles above Nashville. Regular lines of steamers ply on these rivers. Large ship- ments of coal are sent south by the Tennessee River. The Pond River flows into the Green River, and during high stages of water is navigable for about fifteen miles; it may be rendered navigable by a system of locks and dams, as far up as Bakersport, a distance of about thirty miles. The Tradewater River is ascended by light-draught boats during the spring freshets as far up as Belleville; it is quite practicable for it to be rendered navigable for forty miles, or more. Prior to the building of the Louisville, Paducah, and South- western Railroad, Rough Creek (which empties into Green River), was regularly plied by light-draught steamers as far up as Hartford, Ohio County, having been rendered navigable by locks and dams. It will be seen that it is a mere question 53 GENERAL RESOURCES OF WESTERN COAL-FIELD. of enterprise whether or not the streams may be used as roads for carrying out produce, &c. The railrvavs are the St. Louis and South-eastern Railway (connecting St. Louis, Mo., and Nashville, Tenn.), which passes north and south through Henderson, Webster, Hop- kinis, and Christian Counties; the Evansville, Owensboro', and Nashville railroad (not yet completed), which (so far as built) passes north and south through Daviess and McLean Counties into 'Muhlenburg County; and the Louisville, Padu- cah, and South-western railroad which passes westwardly through Grayson, Ohio, Muhlenburg, Hopkins, and Caldcwell Counties intersecting the north and south running railroads; one at Owcnisboro' Junction, and the other at Nortonville. The total number of miles of railroads in the coal-field is about one hundred and eighty-five. Thus it will be seen that transportation is, or can easily be, furnished to nearly all of the workable coal-beds. The Green, Pond, and Tradewvater Rivers and their tributaries (some of them of considerable size), and Rough Creek drain a large portion of the coal-field; while other portions are reached by the several railroads. Some of the best coals are found on the Green and Tradewater Rivers; but as yet comparatively little mining has been clone in them. So far nearly all of the important mines have been opened along the paths of the railroads, a plan which has resulted in giving themi a more rapid, although more costly, transportation than was offered by the rivers. IV. NUMBER OF COAL MINES, &c. IN all there are about thirty collieries of importance in the coal-field. The mines are worked on a general plan modelled on the post and stall-system. About fifteen of them are located along the Louisville, Paducah, and South-western Railroad; six along the St. Louis and South-eastern Railway; and two 54 THE COAL TRADE. on the Evansville, Owenshoro', and Nashville Railroad. Others are located in the neighborhood of Owensboro', bordering the Ohio River; at Airdrie on the Green River; and several in Crittenden and Union Counties, in the vicinity of Caseyville. The Coal Trade. - It is difficult to determine the precise amount of coal raised in this field, as the records are very imperfect. The product of the Kentucky collieries, however, has operated greatly in regulating the amount of foreign coal brought into the State and into the Southern markets. Louisville, of the home markets, has especially been bene- fitted by these mines, as the following will show : In the winter of I87I-72, on account of low water, the Pittsburgh coal reached the price of 7.00 per load of twenty- five bushels, while the Kentucky coal sold at 5.oo and 5.50 per load. In the succeeding winter (1872-73), the Ohio River was again at a low stage but the highest price paid for Pitts- burgh coal was s.oo, the average being 4.50; the Kentucky article selling at 4.50 and 4.00 per load. In the winter of i873-74, there was a good stage of water in the Ohio River, and at the same time plenty of Kentucky coal, and the Pitts- burgh coal sold at 3.50 and 4.00 per load. In I874-75, there was a still greater reduction in prices, the Pennsylvania coal selling at 3.oo, and that from Kentucky at 2.75 per load. This season, the Kentucky collieries have suffered in com- mon with those of other regions, and also from internal com- plications; hence their product may fall behind that of former seasons, or at most not go beyond it. According to the census reports of i870, when few collieries were in operation in this field, the production of the mines amounted to about I I 5,094 tons of coal; of which 67,466 tons were raised in Union County, and 23,600 tons in Crit- tenden County. The product of the mines on the Louisville, Paducah, and South-western Railroad alone, from October 1872 to October I874, amounted to 270,000 tons.t and at least half as much A ton of coal contains about twenty-five bushels. t A number of the largest collieries were not in operation until 1873, hence for some of them the statement does not represent a business of two years. Scarcely anv of the mines had been opened longer than two years when the statistics were obtained. 55 56 GElNERAL RESOURCES OF WESTERN COAL-FIELD. more may be estimated for the product of the other mines for that time, placing the probable product at 405,000 tons. V. BUILDING MATERIALS. [Vood. - The larger portion of the region Wvest of Salt River, especially that lying within the limits of the coal-field, is supplied with forests of valuable timber. In different sections of the region bordering the Green River fine white oak, chestnut, oak, yellow poplar, and black- walnut trees are found. In Daviess, and some other Counties, large-sized chestnut trees are not infrequent. The forests of Hopkins County and neighboring regions are noted for their growth of large-sized oaks and poplars. Sloue. -The St. Louis group furnishes admirable building- stone and material for lime. Some important quarries have been opened in its beds. At Bowling Green the O6lite is quarried very extensively, and the exportation of the stone in dressed blocks has grown into an important industry. At Glasgow J unction, in Barren County, the " lithographic " beds have also been largely quarried and dressing-works erected. The Olite and "lithographic " stone are both very valuable as building material, being unexcelled, perhaps, for nice work by any of the Subcarboniferous beds. The Olite is especially esteemed bv builders for its durability and beautiful appear- ance after dressing. Large quantities of it are sent to St. Louis and other western cities and to the south, and even to the Atlantic States. The dark blue beds of the St. Louis group, and a few of the Chester group, serve very well for heavy work. Few of the Sandstones in the coal-measures are of much value as building material. They are, as a class, too soft and incoherent; hence liable to disintegrate when set in a wall. They are occasionally found suitable for ordinary purposes. The great sand-rock at the base of the Chester group is in a number of places a fairly good building stone. MARL BEDS. Gravel Beds. - Between the Cumberland and Tennessee Rivers are large deposits of gravel, the shipment of which to cities in which gravelled streets are used may prove a source of profit. The gravel covers a considerable area, and in many places seems to have formed into ridges. The beds seem to be practically almost inexhaustible, and may be accounted among the valuable deposits stored in XWestern Kentucky. The material is largely used on the streets of Paducah, and has also been tried in Louisville. Pa/zi' Aaer/ta/s. - It is possible that some of the red earths found associated with the St. Louis beds may prove useful as materials for paint; their merit, however, is as yet only conjectural. The Chester group, however, furnishes deposits of un- doubted value for paint material. Southwardly from Leitch- field, Grayson County, beds are found of two colors, - red and light blue. The material has been locally used, and with very favorable results. The Shales overlying Coal A frequently furnish an abundance of ochre. VI. OTHER MATERIALS. .7A1ra Beds. -One of the most interesting results of the geological survey was the discovery of potash and soda in some of the marls of the Chester group, in such quantities as to prove them valuable as fertilizers. Attention was first. directed to the deposits near Leitchfield, Grayson County, and now they are searched for with interest wherever the Chester group is known to occur. They have been found in Gravson, Edmonson, Breckenridge, Cald- well ('), Christian (), and Livingston Counties. Their entire extent is unknown, but it is not improbable that further ex- plorations may prove their existence wherever the Chester group is fully developed. Scarcely too high an estimate can be placed on these marls in Kentucky, as we have therein a ready and cheap fertilizer 8 5 7 8 GENERAL RESOURCES OF WESTERN COAL-FIELD. for tobacco lands, -the properties of the marl being to renew the vigor of the soil as it is impoverished by the tobacco. The infertility of much of the land is largelv due, not to origi- nal poorness, but to the exhaustion produced by tobacco; these potash marls are expected to serve in placing the lands once more in a fertile condition. Followincg, is the analysis of a sample of the marl collected from Haycraft's Lick, Grayson County: - Composition, dried at 2I2 Fahrenheit - Alumina, iron, &c., oxides . . . . . . . . 27.81I Lime carbonate . . . . . . . . . . . .88o Magnesia . . . . . . . . . . . . . .824 Phosphoric acid. .. . . . . . . . . I09 Potash .... . . . . . . . . . . 5.554 Soda . . . . . . . . . . . . . . . .657 Water and loss.. . . . . . . . . . . 4.245 Silica and insoluble silicates . . . . . . . 59.920 I 0o.000 Lead. - In nearly all of the regions where the St. Louis group is fully developed more or less lead has been found. The only mining that has been done for the metal, however, has been in Livingston, Crittenden, and Caldwell Counties. In Livingston and Crittenden Counties a number of pits and excavations of various sorts have been dug for the purpose of working the deposits; with possibly one exception, however, the work has so far proven unprofitable. In Crittenden County considerable lead has been found at a point known as the Columbia mines, leading to the supposition that, eco- nomically managed, they may be wrought at a small profit. So far these lead-mines have had to contend with the produc- tion from the mines in the Rocky Mountains, where a large quantity of this metal has been produced, almost without cost, in the reduction of ores for their silver. Should this compe- tition be in time removed, they would become more important sources of profit. Zinc. - Zinc is frequently found in the form of the sulphide (Black-Jack) accompanying the lead; it has never been found in sufficient quantities for working. 58 MINERAL SPRINGS. Irou Ore. -As hitherto mentioned, some of the regions underlaid by the Subcarboniferous beds furnish admirable Limonite ore. Towards the base of the coal-measures the Shales frequently carry good beds of the Carbonate ore; in general, however, the beds of the coal-measures are unproductive, save near their base, where some of the best ores of the Ohio Valley are found. Fluor SpAar.- Fluor spar is found in more or less quanti- ties throughout the lead region. In Crittenden County, north- wardly from the Columbia mines, fillor spar is found in great abundance. Considerable deposits of the massive varier, very white and apparently free from impurities, are found at the Memp-his mines and vicinity. It is not unlikely that other important deposits may be found. llineral Spriings. - Springs of sulphur and chalybeate water are not uncommon in regions where the Subcarbonif- erous series come to the surface. The ones most frequented are the Grayson and Rough Creek Springs in Grayson County, the Ohio Springs in Ohio County, and the Sebree Springs in Webster County. The Grayson and Rough Creek Springs are watering-places of considerable popularity in Kentucky and the South; the Grayson Springs being, perhaps, the most generally known. There are a number of Dther springs resorted to, and whose waters are esteemed by many; they have, however, more of a local reputation. The Sebree Springs have many visitors from the western part of the state and contiguous regions during the summer. The coal-measures also furnish mineral waters in some regions. The most interesting are in Daviess County, and are known as Hickman's Springs. Several of the waters are re- markable for the amount of alum they contain. Analyses of the waters from the various springs will be found in the Chem- ical Report, Vol. I, Second Series, Kentucky Geological Reports. 59 6o GENERAL RESOURCES OF WESTERN COAL-FIELD. VII. GENERAL REMARKS ON AGRICULTURE. .Soil. -There are three general varieties of soil found in the region of the Carboniferous rocks. The soil of the coal-measures, originating as it does from SandstonQs and Shales, is a light, sandy mixture, usually yellow- ish in coler; or a rather dense, dark-colored mater ial becoming waxy and unmanageable after rains, - according to localities. The soil resulting from the beds of the coal-measures seems especially adapted for the growth of tobacco. This may be due to the fact that nearly all of the Sandstones are micaceous, and that upon disintegration the mica furnishes the mixture with the potash required by the plant. In the Chester group wve get a mingling of sandy, calcareous, and alumniious materials, producing in some regions a fairly good soil. In general, however, Shale predominates largely, and produces, w-hen unmingled with other materials, a l)oor and stubborn soil. The finest soil for general purposes is furnished, perhaps, by the St. Louis group. It is a deep-red earth, rich in iron and other desirable matters. This soil is very characteristic of the St. Louis group, and is almost invariably found where the limestones are the first beds below the surface. CroAs. -- Tobacco is the staple agricultural product of Ve.steirn Kentucky; the other crops, such as wheat, oats, corn, and hay, are raised more for home consumption than as an article for exportation. The following are the yields per acre of the several products, so far as past observation would indicate: Lowest Highest Average Yield. Yield. Yield. Corn . . . . . . . . . . . lo 6o 30 Wheat . . . . . . . . . . . S 35 10 Hav, (Timothv) t.. 2 I 2 (Red Top) t.. I 2 I Y Tobacco +. . . . . . . . . . 300 1500 Soo i Yield in Bushels. t Yield in Tons. Yield in Poutvtds. TOBACCO CROP. In her tobacco yield, Kentucky now stands first among the States, and the western part of the State furnishes by far the larger portion. The principal tobacco-growing counties east of the Tennes- see River are Caldwell, Christian, Daviess, Henderson, Hardin, Hopkins, Muhlenburg, and Ohio; Daviess County is said to be the largest producer, Christian County standing second. The principal shipping points are Henderson, Owen sboro', and Hopkinsville ; Princeton and Eddvville are also depots for the handling of tobacco, -the former place doing a con- siderable business. Owensboro', it is said, is the largest "strip" market in the world; Henderson falls but little behind it, and was until within the last year or two the largest market. The time has been too limited wherein to obtain complete statistics of the trade at the different shipping points; the following statements, however, of the market at Owensboro' and Hopkinsville for a period of years will serve to show the magnitude of the tobacco interest. The statistics concerning the Owensboro' market were kindly furnished by Captain R. L. Triplett. Statemnent of die Amount of Tobacco exported from Daviess Couy for six Ye r-s prez'iotis to 1876. Frn j From other Pounds Oweusboro'. F luints. Hhds. Product of i868 5,000 5oo 5,500 8.250.000 ,, ,, i 869 5,500 5oo 6,ooo 91000,000 1870 6,0oo 500 7,000 10,500,000 I, 871 6, ooo 500 6,oo 9.750,000 ,, i872 7,500 500 8,ooo 12.000,000 , i8(73 9.000 500 9,500 14.250.000 1874 3,000 jO t 3,z0o 5,250.000 1I875 Soo I0 500 8,500 12,750,000 A short crop year. t Not quite that much, but a fair enotiph estimate. : Product nut yet gone forw;rd, but will reach as much. Statistics concerning the Hopkinsville market are taken from the Annual Circular of Mlessrs. J. K. Gaut & Son: - 6I 62 GENERAL RESOURCES OF WESTERN COAL-FIELD. In i870, there were sold 2,468 hog-sheads. I87 1, 5,970 1873, 9,155 a'1874, 13,047 These sales are up to Nov. I of each year, and include all the sorts of tobacco that are sent from the place. Statistics of the Henderson market have failed to come to hand. It must be borne in mind that Louisville and Paducah also receive large amounts of tobacco from this region; hence the foregoing show but a small proportion of the yield. The following Table, extracted from a late circular from Liverpool, may be of interest, as it shows the number of hogs- heads of Virginia and Kentucky tobacco on hand, March I, for a series of years: - This table serves as an approximate means of measuring the- exports from the two States. Much cf the Puducah exports, however, are of the tobacco grown west of the Tennessee River. THE IRON ORES OF KENTUCKY. THE iron resources of Kentucky are extensive and varied. At a few localities a considerable development of them has been attained; but, taking the State as a whole, it has hardly reached a fraction of the possibilities of production. The greater portion of the ore territory of the State is as yet untouched by the pick of the miner; but enough has been done in most of the ore districts to learn the quality and some- thing of the extent of the ores. Geographically the ore districts of the State may be divided into the eastern and western. Geologically the ores of most importance may be divided into three classes, as follows- i. The Clinton ore of the Silurian period. This is the equivalent of the Dyestone ore of Tennessee and Virginia. 2. The unstratified Lirnonites of the Subcarboniferous Lime- stone. 3. The stratified Carbonates and Limonites of the coal- measures. There are also ores associated with the WVaverly and De- vonian Shales in many parts of the State, which have been worked to some extent; but they are of minor importance in comparison with the other varieties of ore. Of the three classes of ore above named the first and the third are found in Eastern and the second and third in Western Kentucky. It may be said also that the ores of the coal-measures are the best developed and of the most importance in Eastern, while the unstratified Limonites of the Subcarboniferous Limestone are of the greatest value in Western Kentucky. THE IRON ORES OF KENTUCKY. It is also proper to state here that the State has been imper- fectly prospected, and that it is altogether possible, and indeed probable, that the ores of one or another of these varieties will be found to be much more extensive and valuable than at pres- ent supposed. 7/ze Iron Ores of _Esleriz Kcuhckly. - The ore districts of Eastern Kentucky, where the ores have been manufactured, are two, kinown as the Red River and the Hanging Rock iron regions. The Red River iron region embraces portions of Estill, Lee, Powell, Menifee, and Bath Counties. The ores found in this region are the Clinton ore, and an ore, stratified, resting upon the Subcarboniferous Limestone at the base of the coal-bearing Shales. It is found both as Carbonate, or clay Ironstone, and as Limonite, or Brown Hematite. It is this ore which has been most largely worked, and upon which the excellent reputation of the iron from this region has been maide. The Clinton ore has not been so extensively worked; but the principal deposit of it is situated geographically near this region, and may be said to belong to it. The best known deposit of this ore in Kentucky is in Bath Counts, on the waters of Slate Creek, and is known as the Slate F-irnace Ore-bank. It is a stratified deposit of Oblitic Fossiliferou.s Limonite, capping several hills in the vicinity. It reaches a thickness of fifteen feet at places. The area covered by the ore at this point is somewhat over forty acres, and the total amount of ore about one and a half million tons. The ore bears evidence of having been formerly a Hematite, similar to the Dvestone ore of the same geological horizon alon, the great valley from New York to Alabama, but it has lain so long, unprotected by any thing except a slight covering of earth, that it has absorbed water, and been converted into a Limonite. This deposit seems to be somewhat local, -at least of this thickness, - as it grows thin, and finally disappears in this neighborhood. The Limestone which bears the ore is, howv- ever, present in a narrow rim all round the central part of the State, and it is probable that, when thorough examination is made, other deposits of the ore will be found. 64 ORES OF EASTERN KENTUCKY. Thie following analysis by Dr. Peter and 'Mr. Talbutt, of the Kentucky Geological Survey, of a sample of ore from this deposit, shows the composition of the ore: Iron Peroxide. .. . 70.o60 Alumina . . . . . . ... . . . . 4.540 Lime Carbonate . . . . . . . . . . . l040 MILagnesia.. . . . . . . . . . . . . .021 Phosphoric Acid. . . . . . . . . . . i.620 SulphuricAcid. . . . . . . . . . . . .03I Silica and Insoluble Silicates . . . . . . . I I 530 Combined Water . . . . . . . . . . . 12.C0O 100I.42 Metallic Iron... . . . . . . . . . . 49.042 Phosphorus. . . . . . . . . . . . . .707 Sulphur . . . . . . . . . . . . . . .0] 2 The Dyestone ore, a Fossiliferous Hematite, extends along the flank and foot-hills of the Cumberlaud Mountain in Vir- ginia, just across the State line from Kentucky, the crest of the mountain forming the line for about forty miles. It lies in two or three beds, ranging from six inches to three feet or more in thickness, and forms in the aggregate an enorm-nous mass of cheaply-obtainable ore. This ore, although situated in Virginia, is of the greatest importance to Kentuckv, as it is destined to be smelted with Kentucky coals, which lie on the opposite side of the mountain, and are the only coals accessilble to the ore, as there is no coal to the south of the mountain. This ore, although somewhat phosphatic, is easily worked, and yields from forty to fifty per cent. of iron. From this ore, smelted with stone-coal, iron will probably be made as cheaply as in any region of the country. The great Pine-NIountain fault, which extends from some distance south of the Kentucky line in Tennessee, in a course about north thirty degrees east through Kentucky to the Chatte- rawah or Big-Sandy River, at many places is of sufficient uplift to have brought the rocks of the Clinton or Dyestone group above the drainage; and it is probable that on exploration the ore will be found in Kentucky. It has been found at the foot 9) 65 THE IRON ORES OF KENTUCKY. of the Pine Mountain in Tennessee. In Kentucky the place of the ore is usually covered deeply by the talus from the overlying rocks, which probably accounts for its not having been discovered. Should it be found along the foot of Pine Mountain in Kentucky, it will be most favorably situated for cheap iron-making, as on the opposite side of the stream, which flows at the base of the mountain, there is found excel- lent coal in great abundance. The Limestone ore of the Red River iron region, from wvhich the iron is manufactured which gives to the region its reputation, rests upon the Subcarboniferous Limestone, and from this association takes its name. It lies in a bed of irreg- ular thickness, ranging from a few inches to three feet or more in thickness, but probably averaging, where found in any quantity, about one foot thick, or a little less. It is occasionally irregu- lar and uncertain in its distribution; but, in general, it may be said that it is found in its proper position almost wherever the Subcarboniferous Limestone is above the drainage, along the edge of the coal-measures from the Kentucky to the Ohio River. South of the Kentucky River the ore is known to extend a short distance, as far as it has been explored; but its limit in this direction is as yet unknown. The Red River region embraces, however, only that portion between the Licking and the Kentucky Rivers. This region has been little developed, except in a portion of Estill County where four charcoal-furnaces have been in operation. There are many eligible sites for charcoal-furnaces in this region, where timber and ore are both in abundance and as yet un- touched. The development of this region has been retarded b-y the lack of transportation facilities, as the iron had to be hauled a long distance in wagons to railroad or river. This difficulty is likely to be remedied in the near future by the construction of one or two projected railroads into or along the edge of this region, and we can then look for a largely- increased production of the excellent iron from this region. The iron is of great strength, and ranks very high in the markets of the \Vest. It is used principally for car-wheel purposes, as it is of very great strength and chills well. 66 HANGING ROCK IRON REGION. The following analyses show the character of the ore of this region: No. i. No. 2. No.. O 4- Iron Peroxide..... . 66.329 63-535 74.127 65.59t Alumina. . . . . . . . 12.532 2.798 3.342 3.762 Lime Carbonate. . . . . trace. .450 .390 trace. I M agnesia. .... . .173 1.073 .46 i .248 Phosphoric Acid.. . . . .709 .537 .6o i 447 Silica and Insoluble Silicates . 9.720 20.480 9.;5 80 6 230 Conibined Water.. . . . 9.580 9. 800 1 1.270 I I o6o Total. . . . . . . 99.043 i00.673 99-971 99.914 Metallic Iron.. . . . . 46.440 45-874 51.889 45.914 Phosphorus.. . . . . . .309 .234 .262 .195 No. I. From the Richardson Bank, Clear Creek, Bath County. No. 2. From Logan Ridge. Estill Furnace, Estill County. No. 3. From Thacker Riclde. near Fitchburg, Estill County. No. 4. From Horse Ridge, Cottage Furnace, Estill County. The above analyses were made by Dr. Peter and Mr. J. H. Talbutt, chemists of the Kentucky Geological Survey, from samples selected by the writer. THE HANGING ROCK IRON REGION. The Kentucky division of the Hanging Rock Iron Region at present embraces the whole, or parts, of Greenup, Boyd, Carter, and Lawrence Counties. The ores are stratified Car- bonates and Limonites, occurring in the lower coal-measures, beginning with the ore just described, resting upon the Sub- carboniferous Limestone, and extending through six h undred to seven hundred feet of the coal-measure strata. The ores are mineralogically similar, but differ somewhat in their physical character and circumstances of deposition. They are popu- larly known as Limestone, Block, and Kidney ores. They usually occur at well defined geological levels, but do not always form connected beds. They also differ in thickness, ranging from four to eiht inches in some of the thinner beds to fourteen feet in one local deposit. This latter is the Lam- bert ore of Carter Coumity. The most common thickness is from six inches to one foot. There are from ten to twelve ore 67 THE IRON ORES OF KENTUCKY. beds which are of more than local extent in this region. In addition there are numerous local beds, one or more of which is found at nearly every furnace. This region supports eleven charcoal and two stone-coal furnaces. The Hanging Rock iron bears a reputation for excellence for general foundry purposes, which is unsurpassed by any iron in the United States. The iron produced is mostly hot-blast charcoal iron; but some of the furnaces are worked with cold-blast for the production of car-wheel iron. The reputation of the iron of this region is, however, chiefly founded upon its excellence for castings of all sorts. The iron combines in a remarkable degree great strength with fluidity in casting, and non-shrink- age on cooling. The stone-coal iron of this region is used almost entirely for the manufacture of bar iron and nails. The stone-coal iron is made from the ores of this region mixed with a considerable proportion of ore from other States. The fuel used is the celebrated Ashland, or Coalton coal. It is a dry-burning, non-coking coal, which is used raw in the furnace, and is of such excellent quality that no admixture of coke with it in the furnaces is necessary, as is the case with mnost of the other non-coking furnace coals of the \West. The charcoal iron is manufactured exclusively from the native ores, which vield, as shown by the books at a number of the furnaces, for periods ranging from one to four y-ears, an average cf between thirty-one and thirty-two per cent. of iron. The ores of the region are known as Limestone, Block, and Kidney ores. These names are due to peculiarities of struct- tire or position, rather than to any essential difference in chemical composition. As a rule, however, the Limestone ores are tie richest and most uniform in quality. The Kidney ores are next in value; while the Block ores present greater v ariations in quality than any other, some of themn being equal to the best of this region, and some so silicious and lean that they cannot be profitably worked. The following analyses by Dr. Peter and Mr. Talbutt, of the Kentucky Geological Survey, show the composition of some of the ores of each class in this region:- 68 ORES OF WESTERN KENTUCKY. Iron Peroxide. . . Alunmina . M,-an,_. Brown Oxide Limie Carbonate M a-nesia Phosphoric Acid Stiluhliuric Acid Silica and Insoluble Silicates. Combined Water Total Metallic Iron. . Sulphur . Phosphorus No. z. 67.859 i. i6o .980 .120 1.275 .143 . . . 15.560 1 2903 100.000 47-501 .062 No. 2. 7'.68o 4.155 . 090 .380 .050 .084 .270 T2.65o 10.800 100.159 50.176 .108 .036 No. 3. 54 530 2.120 1.380 .040 1.823 .908 .336 28.360 10.900 100.397 38.171 .134 .428 No.4. No. 5. No.6. 68.928 61.344 66.200 2.768 4.236 3.907 .290 . . . .030 .68o .750 430 .641 .208 .345 .249 .795 130 .74S .o041 182 15.240 21.480 16.530 11.100 11.200 It . 730 100.643 100.054 99.484 48.249 42.941 46.340 .298 .o06 .072 .098 347 .057 And loss. No. i. Lower Limestone Ore, Kenton Furnace, Greenup County. No. 2. Upper Limestone Ore, Graham Bank, near Willard, Carter County. No. 3. Lower Block Ore, Kenton Furnace, Greenup County. No. 4. Upper or 'Main Block Ore, Laurel Furnace, Greenup County. No. 5. Yellow Kiclney Ore, Buena Vista Furnace, Boyd County. No. 6. Yellow Kidney Ore, Mount Savage Furnace, Carter County. THE IRON ORES OF WESTERN KENTUCKY. The most extensive and best developed ore region of WVestern Kentucky is called the Cumberland River iron regrion. It embraces the whole, or parts of, Trigg, Lyon, Livirg-stone, Crittenden, and Caldwell Counties. The ores of this region are Limonites found resting in the clay and chert above the St. Louis or Subcarboniferous Limestone. They occur in de- posits of irregular shape and uncertain extent, but in the aggregate the amount of ore is immense. The ores are distributed with great irregularity throughout this region, but they seem to be found in greatest abundance and quantity where the Limestone has been most extensively worn away, and where, as a consequence, the clay and chert w1hich are the result of its decomposition are of greatest thickness. The ores are, perhaps, found in greater abundance in the country between the Cumberland and Tennessee Rivers than in any other portion of this region, although- there 69 THE IRON ORES OF KENTUCKY. are extensive deposits on the east side of the Cumberland River which have been largely worked. As a rule, however, the deposits decrease in size and frequency in going from the Cumberland River toward the east, and, after a few miles' distance from the river is reached, they are scattering and small. The ores are of excellent quality, being almost en- tirely free from sulphur, and containing but a small amount of phosphorus; but they are sometimes mixed with chert and sand. The quality in this respect is as variable as the size of the deposits; the ore in the same deposit frequently showing all degrees of admixture with chert, from a chert breccia, to a rich, pure ore with only an occasional lump of chert enclosed. The average yield of iron from the ore at the furnaces of this region, where it is not very carefully selected previous to roasting, is between thirty and thirty-five per cent. WNith careful sorting the yield can be brought much higher, from forty to fifty per cent. The iron produced from these ores is of a very high grade. There are three active furnaces in this region which use char- coal fuel cxclusively for the production of pig-iron. From this iron is manufactured the celebrated Hillman's boiler-plate, of which it is said, by the manufacturers, that no boiler con- structed oL this iron has ever exploded. This iron ranks equal, or superior, to any other boiler-plate manufactured in the United States. It is used largelv for steamboat and locomotive boil- ers, for which latter purpose it finds an extensive market, even as far as the Pacific slope. Considerable ore from this region has been shipped to fur- naces at a distance; but within the past two years the depressed condition of the iron market has rendered this unprofitable. This region is well situated as regards transportation facilities, -it being drained by the two navigable rivers, the Cumber- land and Tennessee, and on the lower border by the Ohio, so that the iron manufactured here can be very cheaply placed in market. The following analyses of two samples of ore from the Suwannee furnace-lands, Lyon County, will show the charac- 70 ORES OF WESTERN KENTUCKY. ter of the ore from this region. The analyses are by Dr. Peter and Mr. Talbutt of the Kentucky Geological Survey: - No.x. No.2. Iron Peroxide.. . . . . 59.370 70.5I8 Aluminia. . . . . . . . .622 .045 Man'ganese. . . . . . . .090 . I90 Lime Carbonate... . ..I70 .090 Magnesia. .... . . . .100 trace. Plhosphoric Acid .... . .179 .275 Sulphur ... . . . . . .212 045 Silica and Insoluble Silicates . 30.000 I8.910 Combined Water. . . . . 8.400 9.850 Total. . . . . . 100053 99.923 Metallic Iron... . . . . 41-559 49 363 Phosphorus. . . . . . . .077 .120 This same variety of ore is found, in greater or less quantity, in many other counties where the St. Louis Limestone is the prevailing rock formation, but in none of them, save those mentioned, has any extensive iron industry been established. In the Cumberland-River iron region there are many furnace- sites unoccupied where iron can be cheaply and profitably man ufactured. This region is capable of, and destined to, a much greater development than it has yet attained. The charcoal-iron man- ufacture will always be an important and extensive industry, for over a large part of the region the most profitable use that can be made of the land is the production of timber for char- coal. There is destined at no far-distant day to be a large stone- coal or coke iron industry established here, using the ores of this region with the coals of the Western Kentucky coal-field, either raw or coked. The best known of the Western coals at present are too sulphurous for use in iron-making, without previous separation from sulphur by washing and coking. It is through the introduction of modern machinery and ovens, by which these operations can be cheaply and thoroughly effected, and a coke fit for iron-smelting produced, that the coal and iron ore of Western Kentucky will be most profitably and extensively developed. The Louisville, Paducah, and 7 I1 l THE IRON ORES OF KENTUCKY. South-western Railroad affords direct communication between the coal and ore fields. Already measures are in progress for the erection of extensive coke-works on the line of this railroad, which will doubtless prove but the first step in the successful development of a different form and more extensive iron in- dustry than any yet established in Western Kentucky. THE NOLIN-RIVER DISTRICT. In Edinonson and Grayson Counties, north of Green River, between Nolin River and Bear Creek, is an area of considera- ble size called the Nolin-River District. The ores of this region are stratified Carbonates and Limonites, found near the base of -he coal-measures. The ore of most value occurs above th(e Conglomerate. It is about four feet thick, and, so far as present developments indicate, underlies an area of large extent. It is almost wholly undeveloped. A number of years since a small charcoal furnace was established on Nolin River, but it was so far from market, and transportation of the iron was so uncertain and expensive, that the enterprise soon failed. It ran long enough, however, to establish the fact that an excellent iron could be made from these ores. The following analyses, by Dr. Peter and Mr. Talbutt, show the quality of a sample of this ore from near the head of Beaver- Dam Creek in Edmonson County: Iron Peroxide. Alumina. Mlanganese. . . . . Lime Carbonate. Magnesia. Phosphoric Acid Sulphuric Acid . Silica and Insoluble Silicates Combined water . Total Metallic Iron. . Phosphorus . . Sulpl Our . ..... ......... 52.926 4.792 .210 .1 8o .425 355 .143 . - - - - 30-580 10.400 .1.. .I00.0 I I .... . 37.048 .I54 .057 72 . . . NOLIN-RIVER DISTRICT. In addition to the great amount of timber available for charcoal, stone-coal in abundance occurs in the same region. This coal is the lowest of the series, and is of most excellent quality, -analyses showing it to be far superior to the higher coals of WVestern Kentucky, which are the ones more generally mined. This region is now more accessible than formerly, as it lies within fifteen miles of the Louisville, Paducah, and South-western Railroad; but the lack of transportation facili- ties directly to it has prevented its development. The aggre- gate amount of ore, coal, and timber suitable for charcoal in this region, is immense, and it offers great opportunities for development. It is one of the most richly endowed undevel- oped iron regions of the State. In many other localities in the WVestern coal-field iron ores have been found, but they have not been thoroughly pro- spected, and little is known of their extent. One of the best- known localities of this sort is in Muhlenburg County. In this county are found, at Airdrie Furnace, on Green River, and at Buckner Furnace, near Greenville, deposits of so-called black-band iron ore,-a ferruginous bituminous Shale, yielding about thirty per cent. of iron. At Airdrie Furnace this ore rests immediately above an excellent coking coal, and the two can be mined together very cheaply. At this place iron can be produced very cheaply by bringing ore from the Cumber- land-River region, and using it in admixture with the native ore. For a more detailed description of this locality, see Report in the second volume, new series, " Kentucky Geolo-i- cal Reports, on the Airdrie Furnace." The above described localities embrace all the most impor- tant iron-ore districts of the State. There are numerous ore deposits at other places, some of which have been worked, but, in comparison with the others, to a small extent only. For more detailed information in regard to some of these districts, the reader is referred to the volumes, first series, "Kentucky Geological Reports ;" to the " Report on the Iron Ores of Greenup, Boyd, and Carter Counties," in the first volume, second series; to the " Report on the Geology of the I0 73 74 THE IRON ORES OF KENTUCKY. Nolin-River District," in the second volume, second series; to the forthcoming reports on the iron ores in the vicinity of Cumberland Gap, and on the iron ores of the Red-River iron region, in the fourth volume, second series, " Kentucky Geo- logical Reports." CHEMICAL GEOLOGY OF KENTUCKY. THE Geological Survey of Kentucky has given very especial attention to the study of the chemical conditions of its products, -the soils, ores. coals, &c., on which industries could De founded. In the following tables will be found selections from the work of its laboratories, done by [)r. Peter, the chief chemist of the present Survey, as well as of that under I)r. Owen, wivth the assistance for the last three years of Mr. John H. Talbutt. Attention is called to the fact that these tables represent analyses made with a high dlegree of care to securing trustworthy results. In the first place, a great deal of care has been exercised in procuring average samples representing the actual character of the several substances considered as workable deposits. Usually such analyses are made from selected specimens, or at best from a rough selection of several fragments believed to represent the average of the beds. A series of experiments has shown that, taken in this way, the samples lead uniformly to too favorable results. The Survey has been to the trouble to have carefully-averaged samples obtained from a number of important de- posits of coal in neighboring States. The analyses based thereon have shown the general untrustworthiness of the usual method of collecting the specimens from which the analyses were made. The errors of this imperfect method of sampling are particularly striking in the case of coal analyses, where it is easy to halve the amount of sulphur, and greatly diminish :he ash by a careless selection of the specimens. The reader is, therefore, requested to be on his guard in comparing these analyses with those from other regions, and to remember that the quantities of the several substances given in each analysis recorded in these tables are as near to the average amounts found in the deposits whence they were taken as it wvas possible to make them by a very great care. In the several reports from the Chemical Laboratory will be found various practical recommendations concerning the use of the materials represented in these tables. Any further information can be had by addressing the Secre- tary of the Geological Survey, Lexington, Ky. CHEMICAL GEOLOGY OF KENTUCKY. re - C 0..) -' 2 .1.., N - '7.. '-.0 - .05 CtO J' Op 0t...I''0 p 0 - Jj IlIO.IJ pal)C.'IX'.I '.j 0' i' 0; r 0 t t '0 -- e re _ .sI'3ezlus 3 t aPIls olSI ] et Isol 'V . d. 6 0 ,00.00 00 - 'Opo OOOOO eirs 95 -00 00 0 0r0 f0 J f o - f f- asuu LIStIOtI -S rIr ' r. . 1'- r Nv, l - O 0 1 c1c - 00 0-0'- 1 co 0 d 6 d i6;fo d oi _ 6 - iuid ut- 0 " '- o -0 0r eOsr v OIPIXOl0.. 00- lo r-.'fl N. Ivl r l _ vI N 0O - O t O0 '0 t -slalleLp: aLimt Xx Ov--, Nor f Ovr ,I" - 8 0 0e r.0 ' 0 rs- f _[......... o.'. -.-...... ; 4-. ......... . . ... .. ............ . ............p....... . __A- ,- ,,_ s__ _ _, AD P .0-Io2 ':z t N I., ".0 0 0 76 U) UZ 4 H F, rn U) :r. 0) ol- 0) 0 .R ,,' vi 0) I OF COMPOSITION OF SOILS. . ': " . Id V Es_;4 r; _n W. r 75 F, . : ; .E n - C N EN ./4O .C 1. 44 44fl) -44 -.0 N 4. 44. 44 0 C - 44 C 44C N - 4, - .CC 4,9 4, .0 - C --4N4'.C 1. - CN 'C4, .41.C4.1.)N.2)-, - .. 4,1.-.4N0.. C .N N -- C C' C C 12 r 'C___ ____ J 6 .CC4, 6o 94,4,4,) C3 4, N- C' 43 .C'C'C' CNN- 4, 0N1'C .40 'C 'C C..N-"''C44-'C NC' _- 4,'1D_N5 t,C'N1. -ws._CN.4. N-. C0 _ A -; _A L N -1.4,Y ' ,OC.,_ d_ 44 - N N ito d5o 6 d.5o6 6 6 d 66 d -dJ o d3 666 C - C , dd3d odt : _ O :o CY_L.NNL. O N - 1N : X , r . C r. ,C C -S Hru. r4N r C-t .- C'C' CAC CC C._L 0' Cn C' ' r00-r' u-. u, O J'N.) N O .U _ _ _O COAO-nuur .'r . i _ i'r 44N i f4,4,4,0.o- CC 4, N'N4N- C-O 4 N 4 .. r, J. i ,NS 0. _ CCC o ' 4,4 r_ 3r,. Nr - C' rJ_ N S 77 I - - 6 ;, , Z Z. '. C/: -, -'r , .E.: " 2 = -E , C: n, '-='5 11 11 CHEIMICAL GEOLOGY OF KENTUCKY. '4 E X- . . C -= E CI _ Ir u ;a c: , xr i .;:, ;5 0 P: _ ,I -.:_ . t O 7z Oa 'a 7 - .-- - ,qp..t IC. Pg11'd. a a 'a a i,,r.Ce n u q u I-qstclOd 1VO 0 e r uNJ q_ . 6 o . . . ,' dw0.. . . .. pt3 3unqdnS o r 0 Id Z- 0 5 p!p z)Uotldsoqj F 'IO- . o 1o . r d N- d ' - da 0 6 6 0 alruoq g -ajtuoqn'a ' . u' ' U3 00 . . . . .a. . . . . . .n.q . . .tc.. . . . . . . . . . 75 . . . . . a.. . . _uE - . eq_C A auuneSedu .rCrA o a S6. _ 78 U3 w C7) 94 1;e UX1 4 No -f 0 - a a Ca- - IRON ORES. C" z (----.4-b' - Jo1- I3.,Ia jSC - 0 30 0 0 0 0 0 C- 0 e- - 0 ,, 0 J01CICCOAd o.00oo0- ,oo c- I j. i I 000. pub ).bfl')pJ 0 0 0 60-c 0 0 0c 0 00000 0000 C C0"000b c -0Jo llii , -j '. r2S.e i,T a 0 0-0 e 0 o-0o. .. .C C Z poy euqdn c uoqIt3t'uula )Cac ' e - _ _-' o oC- _ t "all-!:!R"00 0C 00' .r,.r,....r,....U')tb-. t.t" . . w - - - t- - - - -.'4 - --- 00.bo1 0 C'P!X: CcUOI -)'0 0'0 '.0 '0''0 0 -0 6c O .01 Cr_ Z yCt n cz CO er O CA jt C ue -A C alE palulO ". C .. -o cE - of o Z- eiOC d' ve -d I _ _ __ _ _0 __ I_ -_ _ _ C5 s Kz of _. t oAz.st. NU C -" - - -- -ojruoqxcD E Ci .... -.O...A ... v. e. r_,u .Qpxox;)_ r_:1 _ u, .,trxu , 'C.ue. e;.r_..c..... e..... e... . ..d-..s ri......d Z __-5 - --S---.. -.- . .. . 79 't0. (Z) lz 0 0 P4 _ 0- 1- 0) CO Lt I ._ 0) I CHEMICAL GEOLOGY OF KENTUCKY. 00 -0 0 ) - 0 'e to,![!S Jo -ja la: 4 s: S.,- g3OC,, qeCa0 S J O - Cm :t0.400.00. 0 p. 0 ..0. .- -.I00- 0X jSo-I Nu lal" 8... c 3V DpnlSgIAjadjl Z c1 Qf eN. -- _ _ _ _ _ _ _ _ _ 0 - 00 .-O 0 0 rn r55 d 5 d o d..3 _ w 1sljoO oc- 0 0d o 0 -_o odd dddo 6o c T6 5 UOAz _ O1U0.0.).. C..T 00 XO ommO V1 YsC O- -O , A O_ _ I 00Ntem.0.OeN'. -0 0 .) SW- p e )10A N 000 OO a .0..0..aOC 0...0 N TSPUL ,, 00t , 0-0'N 0 I .;t, p O -'E !S Ia N 0 00 ,0)tto. N ... .. r ..J m......s.. . .A......... 0 CZ;-1g p .uoojd u!N 2 Z-O CI32 e tttV -N -0 500000000-0 _00.'. ; 0 -.)00j0)S0)[I1 CJA trZ' 00' z wx0 4-. l ._ .N 0 wEd 00N0000N) N. N0: r o cO.00)0 R1C0 0 - c oN 00 00t0OJl OAv 000 N - N 00 N0 'rO : _ . ..II N..00 NN Y 0 0N 000 ._ PletoI0Je UOI m N 0 N0 000t N i0l 00.0 00 00 _t0UiO.CC00.0 N0 00V1 00 w0's 1 '0 00. .00 . . r00' Hilvl gad . ...0.0 .00 0 00._.0 I ,: . ..- ......0... 00. .0.0.........-.00 .)dI.. 0000 ............ -4 '--4 "IZ 0.0 tt 0.. I-' or 0 4 C) H: ) 'a E - 6 0)0) 0)0) 0:0 -6 0 00 E - 3 - i.00- - (.1- 0) 0). o '3 0 o0- 0J00000 C - JO '1U0)0 -ad) - Jo Jau 'd O 0 0 0 p f_ ppy mnqdInS c 0 0 t00U0l0 U -. 0 00 0wI UOq 0-) ) Ouf o0000 I I N000 pue in[Vo, .;P otade I v0 o AIA).O 09O0dS 0)- 0 I1 dU. ,. . . I t) 9 JVU I 4 __.) 0 . _ I _ _ IK i a o nUU 0 - -- t -t I I O t flOI [3p X 11) It,' S0 ; liaDa N_ tN .,o N- -, _ N -NON i..,......... ...E., C& -t DS. Dcc t ='t C n-E I7- 4 Mi..E.t.t........t.._.....- = ...............--.''.-..-. ....- 0 CdtS t t C sC 2 X1 C0 I IX O fCO+O C, - qBU zw ftew ) r.u u su.tu u, u uo uo sallqli 0 o, od , o0 0, -0 _, 2 e0 0 .tCX- I I-. 2 Cc 0, t n,2 0 0 2O 0 C. .._ .. X .1 Ir. I I- U) Z -I 0N9 OoC Os S .XiAll u-aqUt,,,Ker(re,e]N8NNe r rNre I 8I COALS. ,t u zZ V F; -41 I-j 11: 0 u -4 0- 82 CHEMICAL GEOLOGY OF KENTUCKY. TABLE VII. MINERAL WATERS (a. Sulphur Walers). Composition; in iooo parts of the Waters. Number in Report. lz lz z; z z4 Z z z v4 ] o t Specific G(rait... n. e.oi.oot loon i.ooi; r.oox6n. e. n. e. n. e. .-05 1.007 10. e. Free Cabo-ic Acid . I. e 0 1)5 o.1234 o.150 o.l65 0.3256 0-360 0 ..263 02772 11. e. 0.355 n. e. Free Sul. Hd70te1 l n. e. .020 .024S .0203 .410 I). e. n. e. n. e..0343 e .0395 n. e. Lime Carbon.te . . 0.23) 1.73 0.1952 o.lSo6 0.2002 0.2020 c.303 1- 3 0.1397 0.1223 .3855 0.2178 Magnesii Carbonate. I.124 05trac.012 .0002 t ace. I.oS32.0- j.027 .1029 .0253 .003 .499 Iron Carbonate . . trace. Mangganee C race M aniganese .arbollate n . e. C.oo27 .ooi4S .0073 .oo66 trace. trace. .069 a. e. .0013 .oo6 .ooo9 and PIo.,sphates . Il. e. Silica. .. . . e.- .00-22.0094 -o28 .oo5 n. e. -i e. n. e. n. e..0112 n. e. n. e. Organic Matters ann d Loss. n. e o. e 1n. e. .0022 .0268 0I. e.It. e.n. e. 0I. e .. . n. e. n. e. boiliscg. . .175 ,.26ot 0.1914 0.034 .. . .. . . . . .. . i6o Lime Suphate. . . trac. -.1649 2.441 1 4520 ,.6291...i56 553 0-0617 Iron Ma nese anld I Alumina Snlhhilte s.trace. .0034 .0007 .0192 n,. e. o.. ..I6 .1023 . . . . .. trace. Magnesia Sulphate. .5774 .3768 .4616 .6)3 0105 .105 .o18 ....4329 . . . .0570 Potash S,.lphate.I. e. t. e.. 0024 .0023 .1026 .072 .017 .2535 - - .152 .1 0042 Soda SulFhate.. . e. 0.26 j0374 tI723 0o43 -.35 ... . . 1433 Sodium S Ilphlde. . ne .0521 04,c) n. e n e e I. e. . e.. 057 n. e. I). e Soda. co.bined witt Orga.nic Acis . . n. e. -.044 j .oo66 Potash, combined ,ith i j Organic Acids . . .. e. 300).003 Potalsiuu Clloride 3 0.13.795 trace. .223 Sodium Chloride . . 2.847 . 0200 -.53 .0542 .009 .036 -.0152 3.3647 8.347.2760 Mfagneciutir Chloride .950 .1598 .0145 .228 Calcium Chloride.. ... ; CalciuClilorce.. 8.. . 1.. . . .. . . . .. . ..,. , . . . .. ..0713 Silica. . . . . . 8 .0034 .0145 n. e. n. e. .oo6S .004 .013 .0343 1.. 8 0176 Lithium . . . . . It. e. trace. trace. trace., trace.. . . trace. .I. e. trace. Iodine and Brom ne. trace. trace. trace. trace. trace.... .trace. f.0015 .00-7 t trace. Soda Carbonate .. .. .. 3o 6.. 04 Total Saline Matters . 709 2.07 [ SI- 6o) 11.325211.5740 o.71; 6 0.410 1.0250 4.54'04 1.-355 Temnperatit eof Sl.rlng n e. 61c j)')j (o f4 I 11. e. n. e. t11 e ii. e. Organic M ttters . n. e. It. e. a n. e.n. e...020 -.040 1.051 0.) trace. n. e. = ilft -ti,lated. t :Alaguesi,,m lodide. Alagnesiulm Bromide. MINERAL WATERS. 83 TABLE VII. - Con/inued. (b. & c. CGalylea/e and Saline Wafers.) Composition; in tooo parts of the Waters. Specific Gravity . . . . Free Carbonic Acid . Linie Carbonate .. . NIagesia Carbolnate . Iron and Manganese Carbo- -lates. With Phosphates, Silc. . Silica. . . . . . . . Total bheld in solution by Carbonic Acid . Lime Sulphate .... Magnesia Sulphate . . Potash Snlphate . . . Iron SOlphate (per basii) Copper Sulphate . Alumina Sulphate . Manganese Sulphate. SodiLno Chloride . . . Potassium Chtoride Calcium Chloride . Magnesiunm Chloride Iodine and Bromine LithiuLm ...... Silica ....... Soda Carbonate Soda Sulphate . Total Saline Contents . Number in Report. z n. e. 11.0031 1L- 0.269 . 159 0.046 0.032 .. . o.286 . .011 trace. . .oog n. e. n. e. .032 .012 0.896 3 0. 5996 -.3330 . ooog .1.246S .0032 .0031 i. e. trace. s.' . 1.0016 n. e. _ ,- 0.3271 .2513 .0074 .1460 .3500 .0721 .o6S 1 n. e. trace. .C.221 .. ne. 0..1 155 .0046 .0260 .0107 0. -563 0 . 0204 .0763 i .040; 0.195 .041 .o26 n. e. .056 .-13 C ,X n. e. n. e. .02. .033 ... 0.0 15 .112 .028 n. e. n. e. 1.0012 0.093 0.0438 .01l45 .0145 n. e. 2.0731 0.0029 .0036 ..,I 0.0247 -.0179 n. e. .0336 .o3 3 I -4.001 -.oo68 n1 e. n.e. .1 0.673 0.9-2 -6 .131 .0297 trac:e. I trace. I tr.ce 0.0218 .0042 0.0538 . 1S7 .1.09 .0 129 0.203 3.454 .067 .0146 .013 .oI8 .0026 .0026 .0-3 .o.S .304 .0013 . . . .0142 .040 .04761.. . I . . I 1364 ! 1.4090 10.3720 ' 0.384 Chloride. , I I tracen. e. ' n. e. .o46 I.0128.0010 .02-4 -... .oS6 0.442 .053 !3 .0205 .50-9 0. 1451 0. 1290 0.9041 '774 1.0 13 5.42S 06.884 3.520 .170 I I I I I l I I I I I I ., c . j Wr'4 _, n. e.. n. e, n,. e. - CHEMICAL GEOLOGY OF KENTUCKY. C V Z. C C C C C I C Z; V O. C, OOC u(- UIV _z; C C a. C C CCc C C _ C N - Cc ECOC C C C. C C.C Et. C C a C N .z Cc 'C'C N N CCC Z.) C.) C C C C C C CcN N CC C.) C.) 6 .0 C IC Cc C N' C g C V E.E C C C C 0 0 M11 Z V C .- t, C. 0. _. VV= Z'Z _1 I I I u: u 3 CS Cc d C Q C.) C cr - '- g -:-C' 'C'N -Cs o o N r C S 0 : -vl Nt., ' ' CN N N N N OC' Ie. Cr q!SauoN N C'C ' N0 . dd d - d d - CCd - - d - N p p!y 3lnqdlns " C C C s CB 6 J Q C Ci C P!:)Y t!odso o N ot 6O 6 e C - C g L QJCN C C't e . cu C; C)Q t C)CJe O X a''N N'NC C 'CC'C- 1 _ -'C e Juu!'IC _C _ nS ' ]b -NC N C 'N _o 66 6 6 6 .ap!xoUOJIg_ ___ Yg2 O _- 'C'C - C' x s tr 'C en'NCIE oNNCO C''C 4oN N outLunty' N - 'C N 'CC 'C C -e.Nr'NN N1 rN el4NJ C_ C0 C 0CO C0 0C ' C 'LID I I I. + s N0 'C' '0C tC'NuNNo'N c'. - a''C w --: 'Ct T _.0 . . . . . . C. o . . . . .. . v.. . . _.. . . 'C 4-NN' 'N N C C 'C'C 0 N 'C ' -rOjf)quE'Ijo aoulJ-1 N1'N'N 'A ' C . _ qNO v OC N C' e C '', 'Cw tt t = . C _i - 1 84 _ 4. - N H I I i I ai BUILDING STONES. 2 AS . 5: I . o c3 c.E5c-t_:5 2 Eco c, 0 cr 0 cv 0 v - 0 O 0 0. 'd_ ; .0 _,-' _ - 2 - 0 0 0I-5. C 0. 0 , 0;d r: . 0- U L. C4CC s ./cr3 oj f 0. , _.. cr C C; JOS-uaIj 0' ' 1 Jo s1.0j'al 6o SD d, C't Ch 0000 0 0000 0 0 o p luao Ja t o__ sttr 02 0 13sloil'2 -. '0 I 00d un N O _ - - -C; t s a eiflqIfl S - - - eXs pl1 PuO eiI g- -sC i e - unO t eSPI2L L' e ____d ___r_- _________ 5 L'IS eN&... ---........t. . .O....... . .xl4 n............ . -uou tj )uI -I 6' ' n .n" 4 I"- 0' X " 0'Crse apl'0 ;)c I-aa ue e --II cI I It!o UOw, I nr ,,,OLr nOtj AIC3Ei end un O _-t S - _ - : O OC 'O : -tllx 'UI- o ""'0 rn -s st s 0NC 85 .2 CL z 0 H z C CO C) 1- C: E- H CHEMICAL GEOLOGY OF KENTUCKY. A! 41 N C) N N 0 U) 0.0 0 0J 0. U) 000 IN 2' i ' O1N ' 0 0 JO 'lUC1N,13 lad ' 6 - 'ElSilqtI5[ CA : sI' r t ' -s rio'3Io i o oo o _ O 0 00 6 oNu - o 6 6 r Nwuoqir N N. r r a O! , 0r r, V P rr, 'It ; OOr . _ 000 00 C.)C N sr _ _ _ _ XNOj N00oq-1 u O O IuO t -t 1t lz U) ul) V:i 0 Of xt -0C, -!I'S pue uS - .;r s C -1 'epos 0I 0 c- o0' o o 0 0-dd o66 iv oundn 3 3' 0 0 .IN)'0 'ptpV opntjdjnS '0 -- ', 0 3!.toqd1'.oqjj 6 do 6d asm 1uI 00000 _jx IMI r1su21jv 1 w- ar I le'o 's. 1S I uoo ! I S I Ut'XC - NI -F C' Is-'alluNa19 if Aq ..',i lp[pd r 3 -ppu qtuliu - p)JIt1)N 0000 1 Xq suuuwooo rq)N1I3'N r.Nrq I Io0u Ot I LUO.Ij PalN 'C g0 'I i 0d;)IU! a0N 3,3: 86 U:I ;4 z ;4 -v ;4 00 1-0 ;t:: 1 r- p ;Z . -V i i I I DESCRIPTION OF TABLES. SOILS. (See Table I.) Soils on Blue -Limestone. - Lower Silurian Formnation. No. 574. (Vol. III. p. 2i8, Rep. Geol. Surv. Ky., 0. S.) Virgin soil, from wood-pasture on Win. Buckner's farm. Cane-ridge land. Primitive for- est-growth, - large Buckeye, Oak, Honey-locust, Sugar-tree, &c. Lower Silurian or Blue Limestone formation. Bourbon County. No. 826. (Vol. IV. p. 85, Rep. Geol. Surv. Ky., 0. S.) Virgin Tobacco soil ; hill-side, north exposure ; Blue Limestone formation. Near Au- gusta, on Mr. L. J. Braclford's land, Bracken County. No. 27. (Vol. I. p. 276, Ky. Geol. Rep., 0. S.) Virgin soil wood-past- ure. About seven miles south of Lexington (Meredith farm); farm of late Mr. Dallam, head-waters of North Elkhorn Creek. Blue Limestone formation. Fayette County. No. 6i9. (Vol. III. p. 263, Ky. Geol. Rep., 0. S.) Blue Limestone soil, from a field thirty to forty years in cultivation, near Big-Lick Creek, Gal- latin County. No. 621. (Vol. III. Ky. Geol. Rep., p. 265, O. S.) Virgin soil; wood- pasture. J. S. Hoskins' farm, forks of road. Some of the best soil in the county. Lower Silurian formation. Garrard County. No. 622. ([bid., p. 266.) Same soil as next preceding, from the oldest field in Garrard County, sixty to seventy years in cultivation. Over the cherty beds of Blue Limestone, Lower Silurian formation. Garrard County. (The second samples fromn the samne locality exemplify a loss of avail- able essential mineral fertilizing ingredients, resulting from cultivation.) No. I134. (Vol. IV. Ky. Geol. Rep., p. 217, 0. S.) Virgin Tobacco soil. From hill-side near Dover, Mason County, about a hundred and fifty feet above the Ohio River, in the midst of the Blue Limestone. Growth - Sugar-tree, XWainut, Black and White Ash, Buckeye, &c. No. 68i. (Vol. IIL. p. 322, Rep. Ky. Geol. Surv., 0. S.) Virgin soil, from woods near Cornishville, on Ch-etetes beds of Blue Limestone, western part of Mercer County. Characteristic forest-growth, \White Oak. No. 682. (Ibid.) Same soil, from an adjoining field, fifty years in cultiva- tion; now in corn, &c. No. 550. (Vol. If. p. 28r, Rep. Ky. Geol. Surv., 0. S.) Virgin soil, from Judge R. C. Graves' farm. Water-shed between Greers' and Clear Creek, near Versailles, Woodford County. Natural growth - Hackberry; Ash, Walnut, Mulberry, Box-elder, &c. One of the best soils of Kentucky. 88 DESCRIPTION OF TABLES. No. 55I. (Ibid., p. 282.) Same soil as the preceding, from a field in con- stant cultivation since i8o8. It has been fourteen years in Hemp. Aver- age of the last year's (1855) crop of corn, eighteen to twenty barrels of five bushels each to the acre. It has produced thirty-five bushels of wheat to the acre. Soils of the Siliriouis MA/ds/one. - Lower Silurian Formation. No. 5c4. (Vol. II. p. i62, Rep. Geol. Surv. Ky., 0. S.) Virgin soil, from a Beech ridge on Robert Wickliffe's farm, two and one-half miles from Lexington, on the Richmond Turnpike. Much less productive than the neighboring Blue Limestone soil, Fayette County. No. 1204. (Vol. IV. p. 245, Rep. Geol. Surv. Ky., 0. S.) Virgin soil, from. woods on the first farm after ascending the hill from Harmony to Stamping-Ground, southern edge of Owen County. Forest growth, White Oak on the top of the ridge; some Beech on the sides of the hill. Soils on t/ie Upper Silurian Formation. No. 805. (Vol. IV. p. 73, Rep. Ky. Geol. Surv., 0. S.) Genuine Clinton group red soil, from over the encrinital, flesh-colored, ,vag-nesian Lime- 'stone (see No. 797), two miles west of Owingsville, Bath County. Prim- itive growth - Blue Ash, Sugar-tree, Hickory, &c. No. I070. (Vol. IV. p. 192, Rep. Ky. Geol. Surv., 0. S.) Virgin soil; eight inches of the surface, taken immediately under the sod of native BlUe Grass, in wood-pasture. Farm of Theodore Brown, six miles east of Louisville on the Lexington Turnpike, middle fork of Bear-Grass Creek, Jefferson County. Primitive growth - Walnut, Black Locust, Wild Cherry, Elm, Ash, Hackberry, BDx-Elder, Bickeve, Pignut and Shell- bark Hickories, Coffee-nut, Red and Over-cup Oak, large Sugar Maples, and Root-covered Beech. Upper Silurian formation. Some of the best Bear-grass land. Soils on the Black Dev'nzian Shale. No. 583. (Vol. III. p. 227, Rep. Ky. Geol. Surv., 0. S.) Soil from the flats near Shepherdsville, derived chiefly from the Black Devonian Shale, at the base of the knobs and overlying the ash-colored Shales; considered almost unfit for cultivation, except for grass, because too wet ; but little cu tivated. Primitive growth -Oak, Beech, Black Hickory, &c. Bullitt County. No. II25. (Vol. IV. p. 213, Rep. Ky. Geol. Surv., O. S.) Virgin soil, de- rived from the Black Devonian Slate, taken from the level tract of land about half way between Elliston and Richmond, Madison County. No. 12I5. (Vol. IV. p. 249, Rep. Ky. Geol. Surv., 0. S.) Virgin soil, from Moses S. Conner's farm, near Red River, Powell County. Principal for- es: growth-ssmall White Oak aud small Hickories. Soil chiely derived from the Black Devonian Shale. SOILS. 89 Soils on, the (Vaverly Sandstone. No. 1222. (Vol. IV. p. 253, Rep. Kv. Geol. Surv., 0. S.) Virgin soil, near Morehead, Rowan Ccunty. Forest growth -White Oak, Chestnut, Hickory, Beech, and some Sugar-tree and Black Walnut. No. 1405. (Vol. I. Second Series, Ky. Geol. Rep., p. 6o.) Old field-soil. Farm of Wim. Abbott, west branch of Tygert's Creek. Field fifty-five feet above the bed of the creek on a bench of Waverly Sandstone. Tops of the hills capped with Limestone ; surface soil ; has been cultivated sixty years; was once an orchard. Carter County. Soils on the Szubca-bom w/ozes Limestone. No. 229. (Vol. II. p. 272, Ky. Geol. Rep., O. S.) Average quality of the Wavne County " Barrens " soil, based on a reddish ferruginous sub-soil. Head-waters of Meadow Creek, Wayne County. Hickory and Black Oak land. No. 81g. (Vol. IV. p. 78, Ky. Geol. Rep., 0. S.) Soil from east hill-side of McCormick's Valley, from field nine years in cultivation, &c. Geo- logical position on the Subcarboniferous Limestone, &c. Bath County. No. 839. (Ibid., p. 99.) Virgin soil, from 'Mr. Dent's land, two mniles north of the base line, one mile west of Sinking Creek, Breckenridge County. The waste of the Limestone, two hundred feet below the base of the Mill- stone grit, &c. No. 960. (Ibid., p. 145.) Virgin soil, taken from the north side of the house of 'Mr. Jas. Townsend on Billy's Creek, a branch of 'Miller's Creek, Estill County. Geological position on a terrace of Subcarboniferous Limestone. No. I473. (Vol I. N. S., Rep. Geol. Surv. Kv., p. 234.) Soil three years in cul- tivation to the depth of seven inches, on Louisville and Paducah Railroad, about one thousand feet west of the twenty-sixth mile-post, &c., in Gray- son County. Timber-Red, Black, and White Oak, with Sugar-tree and Poplar. No. 1549. (Vol. I. N. S., Rep. Geol. Surv. Ky., p. 256.) New soil, five years in cultivation in Corn, Wheat, and Oats, taken to the depth of eight inches. Farm of Daniel Klingelsnutte's heirs, 11,350 feet wvest of Elizabethtown, on the Elizabethtown and Paducah Railroad, and 250 feet to the north. Yield of Corn, thirty, of Wheat, twenty, and of Oats, twenty-five bushels per acre. Hardin County. No. 1029. (Vol. IV. Ky. Geol. Rep., p. 175, 0. S.) Labelled "Soil, top of hill, woods ; farm of CGeorge Smith, Esq., waters of Blackfard Creek two and a half miles in the rear of Lewisport, Hancock County." No. i05i. (Ibid., p. 184.) Labelled "Soil from east side of Whiteside's Creek, Hopkins County." No. 1052. (Ibid.) Labelled " Sub-soil from east side of Whitesides Creek, Hopkins County." DESCRIPTION OF TABLES. No. io08. (Vol. IV. Kv. Geol. Rep., p. i86, 0. S.) Labelled "Virgin Soil, on (Lividin, ride between Jackson and Estill Counties." No. i i6. (Ibid., p. 226.) Labelled "Virgin Soil from the coal-measures of Canev Creek of Licking River, Morgan County. Forest growth- WN-hite Oak, Beech, Sugar-tree, and Black Walnut." Soils on ftze Subcarbonif'rous Sandstone. No. 8i2. (Vol. IV. p. 77, Ky. Geol. Rep., O. S.) Virgin soil, from the valley of McCormick's Run, Bath County. Tlhe soils of this locality show ddbris from the Conglomerate, Limestone, Olive Sandstone, and of the Iron and Coal horizon. No. I469. (Vol. I. N. S., Rep. Geol. Surv. Ky., p. 233.) Soil of an old field, fifty years in cultivation, lying fallow for the last fifteen years, 2500 feet west of the twenty-first mile-post on the Louisville and Paducah Railroad. Timnber, mostly Black Oak, some White and Red Oaks, and a few Poplars. No. io5i. (Vol. IV. p. i87, Ky. Geol. Rep., O. S.) Virgin soil; land of Mr. Sloani, Indian Fork of Rockcastle River, Jackson County, four miles from, McKee on the Big Hill and Richmond Road. Soils on t/ie Tertiary Formation. No. i. (Vol. I. p. 259, Ky. Geol. Rep., O. S.) Soil from heavily timbered land, southern part of Ballard County, between the waters of Bowles and wvest branch of Mayfield Creeks. No. 2. (Ibid., p. 26I.) Soil from the north-western part of Ballard County, near Colonel Gohison's. MARLS. - MARLY SHALES. (See Table II.) No. 5S7. (Vol. III. p. 232, Ky. Geol. Rep., 0. S.) Marl from the line between Bullitt and Spencer Counties; in the Favosi/es maximuis beds. Lowver Silurian formation. No. 14.31. (Vol. I. Geol. Surv. Ky., N. S., p. 21i.) Green Marly Shale from below the Arsenal at Frankfort. Bed eight inches thick (Lower Silu- rian). Franklin Countv. No. 1432. (Ibid., p. 212.) Marly Shale. Same locality as the preceding, but lying above that. No. I433. (Ibid.) Marly Shale. Used as mineral paint at Frankfort. Franklin County. No. 1434. (Ibid.) Marly Shale. From Armstrong farm, Bridgeport, Frank- lin County. In Cincinnati group, just below the silicious mudstone. In same position as the marl near NewvpGt, Ky. Used for paint. No. 971. (Vol. IV. p. i50, Ky. Geol. Rep., 0. S.) Marfy clay from Daniel go IRON ORES. 9' Brink's place. One hundred and two feet above Phillip Brink's branch. Fayette County. Lower Silurian formation. No. i446. (Vol. I. N. S., Geol.. Surv. Ky., p. 220.) Marly Shale, from Sun- set Lick, a mile and a half west of Litchfield, Grayson County. Geo- logical position, the Chester group. No. 1446 a. Same marl analyzed by fusion. Page 496 of Laboratory book (unpublished). Marly Shale, found just below the Upper Limestone. Haycraft's Lick, Grayson County. Page 492 of Laboratory book (unpublished). Marly Shale, four feet thick found below the Upper Limestone. Hat branch of Bear Creek, Grayson County. IRON ORES. (See Table III.) a. limonite Ores. No. i269. (Vol I. N. S., Ky. Geo. Rep., p. 152.) Limonite iron ore from the Block-House Ore Bank, one and a half miles from the Old-Slate furnace, Bath County. Bed ten to twelve feet thick, on the Clinton group. No. 782. (Vol. IV. p. 63, Ky. Geol. Rep., 0. S.) Limestone ore, from the east side of Clear Creek. Clear-Creek furnace, Bath County. No. 1373. (Ibid.) Potato-Knob ore. Average sample. Iron-Hills fur- nace, &c., Carter County. No. 1274. (Vol. I. N. S., p. 155, Ky. Geol. Rep.) Yellow-Kidney ore, sampled from a number of places. Star furnace property, Boyd County. No. 1275. (Ibid.) Limestone ore; average sample. Bellefonte furnace, Boyd County. NO. 1277. (Ibid.) Yellow-Kidney ore, or Kidney ore below the No. 7 Coal. Straight Creek. Buena-Vista furnace. Average sample. Boyd Countv. No. 137I. (Ibid.,p. i88.) Limestone ore, from Horsley Bank. Boone furnace property, Carter County. A cabinet specimen. NO. 1375. (Ibid.) From Royster-Hill Lambert ore bed. The ochre from the lower part of the bed. Iron-Hills furnace. No. 1376. (Ibid.) German ore. Smith Hill. Iron Hills, Carter Countv. No. 138. (Ibid., p. i89.) Main-Block ore. Old Mount-Tom ore. Car- ter County. No. I384. (Ibid., p. i90.) Red-Limestone ore from the Graham Bank. Average sample. No. I385. (Ibid.) Yellow-Kidney ore. Mount-Savage furnace, Carter County. Average sample. No. I41t. (Ibid., p. 200.) Procter Ore Bank. Sycamore Creek, Edmon- son Countv. No. I509. (Ibid., p. 244.) Limestone ore. Samuel Wamock's land, DESCRIPTION OF TABLES. Tygert Creek. Bed one foot thick. Not an average sample. Greenup County. No. 15i6. (Ibid., p. 245.) Shover-drift Limestone ore. Average sample. Kenton furnace, Greenup County. No. I521. (Ibid., p. 246.) Main-Block ore. Little-Morton Bank. Laurel furnace, Greenup County. No. I598. (Ibid., p. 274.) Limonite. Old Suwannee furnace. Bank close to the furnace. Subcarhoniferous. Lyon County. No. i6oo. (Ibid.) Old Suwvannee furnace property. Iron-Mountain Bank. Subcarboniferous. Average sample. No. i6o5. (Ibid., p. 277.) Iron ore from near No. 4 entry. Airdrie furnace, Muhlenburg County. No. i6o6. (Ibid.) Limonite iron ore from Jerry Hope's land, near Middy River. Average sample of the surface Limonite from the upper part of the bed. No. i6o8. (Ibid., p. 278.) Martin ore from near Greenville, Muhlenburg County. Average sample. b. Clay Ironstone and Black-band Ores. (See Table IV.) No. 1271. (Ibid., p. T54.) Blue-Block ore from Wilson's Creek. Average sample from the Star-furnace stock pile, Boyd County. No. 866. (Vol. IV. p. io8, Ky. Geol. Rep., 0. S.) Blue-Kidney ore from Star furnace, Carter County. No. 1363. (Vol. I. N. S., p. i86, Ky. Geol. Rep.) Kidneys in the Shale below coal; layer four inches thick ; Old-Orchard diggings. Boone furnace property, Carter County. No. 1365. (Ibid.) Average sample of Limestone ore at Horsley Bank. Boone furnace property, Carter County. (Clay iron-stone and Limonite mixed.) No. 1369. (Ibid., p. i87.) Gray Limestone ore. Mount-Savage furnace, Carter County. Average sample. No. 937. (Vol. IV. p. 136, Ky. Geol. Rep., 0. S.) Gray iron ore, asso- ciated with the rough ore. Cottage furnace, Estill County. No. i644. (Vol. I. p. 300, Ky. Geol. Rep., N. S.) The Glady ore on the old Brownsville and Litchfield road, west of Bear Creek, Grayson County. No. 1503. (Ibid., p. 242.) Blue-Kidney ore, locally replacing the Main- Block ore; from a drift one mile south-east from Laurel furnace, Greenup County. No. 1507. (Ibid., p. 243.) Gray ore, or Main-Block ore. Baker drift. Laurel furnace, Greenup County. Average sample from the stock pile. No. i6iI. (Ibid., p. 299.) Bitumimous clay iron-stone, or so-called Black- band ore. Labeled Slate-iron ore, from Buckner furnace. Weathered thirty years. Average sample. Muhlenburg County. 92 COALS. 93 No. 749. (Vol. I. p. 347, Ky. Geol. Rep., 0. S.) Black-band ore from WN'illiams's Landing, Muhler.burg County. No. i5o. (Ibid., p. 348.) Shaley Black-band iron ore from the waters of Battist Creek, Muhlenburg County. An extensive layer of Black-band ore, from two to three feet thick, has recently been discovered in Lawrence County, some samples of which on preliminary examination are found to contain from thirty-three to thirty-four per cent. of iron, and from a half to a third of one per cent. of sulphur, much of which could be removed by roasting. c. Red Hemzatite Ore of the Clinton Group. (See Table V.) Page 533, of Laboratory book (unpublished). Dyestone iron ore from near Cumberland Gap, Tenn. ; from Old Clinton furnace. Page 540. (Ibid.) Clinton ore (Dyestone or Fossil ore) upper bed. Poor Valley Ridge, Cumberland Gap, Tenn. Average sample from a number of exposures. Page 54T. (Ibid.) Clinton ore; upper bed. Foot of Poor Valley Ridge, on a branch clown fromn the Virginia road. Cumberland Gap, Tenn. Page 542. (Ibid.) Clinton ore; middle bed, twenty-six inches thick. Cumberland Gap, Tenn. No. 1594. (Vol. I. p. 273, Ky. Geol. Rep., N. S.) Red Hematite iron ore; found on top of hill near Louisa, Lawrence County, Ky. In this locality it is in nodular lumps of various sizes; but it is doubtless to be found in regular layers in other localities in this State. COALS. (See Table VI.) No. i2So a. (Vol. I. N. S., lKy. Geol. Rep., p. 157.) Coal No. 6 from Lurkey-pen Hollow, Old Clinton track. Bellefonte furnace, Boyd County. N\. I230 b. (Ibid., p. 149.) Selected sample of same coal. No. i2S5. (Ibid., p. 157.) Coal No. 6 from Horse Branch (or Run), near Catlettsburg, Boyd County. Average sample. No. i286. (Ibid.) Coal No. 7 from the Ashland Company's mine No. 4, Coalton, Boyd County. Average sample. No. i2S9. (Ibid., p. i58.) Coalton coal No. 7. Two hundred and fifty yards from the west end of No. 4 entry. Average sample. Boyd CoUIty. No. 835. (Vol. IV. p. 96, Ky. Geol. Rep., O. S.) Cannel coal from Mr. South's coal bank (three feet thick) near Jackson, Breathitt County. furnace, Carter County. No. 871. (Ibid., p. iii.) Cannel Coal, twenty-one inches thick, Stinson Bank, Carter County. 94 DESCRIPTION OF TABLES. No. 13.t8 a. (Vol I. N. S., p. i82, Kv. Geol. Rep.) Coal No. 7, Coaltori. Average sample from Wiley Pritchard's bank, near Mount Savage. No. 134t8 b. (Ibid., p. I49.) No. I35o. (Ibid., p. 182.) Coalton coal (No. 7), from a drift on Gum branch of Straight Creek. Mount Savage Company's drift, lower part of the bed. Carter Countv. No. 1353. (Ibid., p. 183.) Coal No. i from Graham bank. Little Fork of Little Sandy River, near Willard, Carter County. Average sample. No. 1356. (Ibid.) Coal No. 2 from Kibby drift, Everman's Creek, a mile from Gravson, Carter County. Average sample. No. 135;7. ([bid.) Coal No. i from Stone branch of Tvgert's Creek, Carter CountV. No. I4T3. (Ibid., p. 201.) Coal from Tar Lick, Davis's Creek, Edmonson County. Five and a half feet thick. No. I4T1. (Ibid., p. 202.) Coal from Shoal Branch. Nolin coal. No. 1448. (Ibid., p. 222.) Tar-Lick coal. Dismal Creek, Grayson County. Average sample. No. I484. (Ibid., p. 238.) Coal No. i, used at Kenton furnace, Greenup County. Average sample. No. I486. (Ibid.) Coal No. 3. Average sample of the main coal of Raccoon furnace below the Slhale parting, Greenup County. No. 1493. (Ibid., p. 239.) Coal, probably No. 3; thirty feet below the Kidiey ore. Laurel furnace, Greenup County. Average sample from the coal-shed. No. 1496. (Ibid.) Coal No. 3 from a drift near Pennsylvania furnace, Greenup Coun ty. No. i649. (Ibid.. p. 302.) Hunnewell Cannel coal. Hunnewell mines. Greenup County. No. I579. (Ibid., p. 266.) Coal from St. Charles mines, Hopkins County. Average sample. Coal D. No. I588. (Ibid., p. 27I.) Coal No. 3 from dIcHenry's coal-bank, six miles south of Louisa, Lawrence Countv. Average sample. No. i589. (Ibid.) Coal No. i from near Henderson. Bogg's Mill, Cane's Creek, Lawrence County. No. I59I. (Ibid.) Coal No. 3. Holbrook's coal, Brushy Creek, Law- rence County. No. i6or. (Ibid., p. 275.) Subconglomerate coal, forty feet above the Subcarboniferous Limestone. Hawkins's Creek, near the line of Powell County, AMenifee County. Average sample. No. i6i8. (Ibid., p. 283.) Coal No. I2 of Owen. Airdrie furnace, near No. 4 entry, Muhlenburg County. Average sample. No. I620. No. ii of Owen. Mluhlenburg County. No. i623. (Ibid.) Coal from Muddy River coal-mine, Muhlenburg Cou Sty. No. i8y. (Vol. I. p. 49, and Vol. II. p. 286, Ky. Geol. Rep., 0. S.) Mul- ford's main coal, or five-feet coal. Union County. MINERAL WATERS. 95 MINERAL WATERS. (See Table VII.) No. 798. (Vol. IV. p. 69, Ky. Geol. Rep., O. S.) Salt Sulphur-water from a well ten feet deep, about sixty steps from the main house, Olympian Sprinigs, Bath County. No). 1456. (Vol. I. N. S., Ky. Geol. Rep., p. 225.) Sulphur-water from the Centre Spring, a naturil spring, the most popular of the Grayson Springs. Grayson County. No. 1457. (Ibid.) Sulphur-water from the 'Moreman Spring, Grayson Springs. No. 1458. (Ibid., p. 226.) Sulphur-water from the MN.cAtee Spring. Gray- son Springs. No. I459. (Ibid.) Sulphur-water of the Stump Spring. Gravson Springs. No. 952. (Vol. IV. p. r42, Ky. Geol. Rep., 0. S.) Red Sulphur-water near the saloon, Estill Springs, :iear Irvine, Estill County. NO 9-3. 9 White Sulphur at the saloon. Ibid. NC) 956. Black Sulphur-water. Ibid. No. 1436. (Vol. 1. p. 2I5, Ky. Geol. Rep., N. S.) Sulphur-water from a bored well, ninety-six feet deep, at the Fleetwood farm of Colonel J. XV. Hunt Reynolds, near Frankfort, Franklin County. Page 525, of Laboratory book (unpublished). Salt Sulphur-water, from a bored well, I34 feet deep, on the premises of -Mr. John B. Trice, Hopkin- ville, Christian County. No. 733. (Vol. III. p. 36I, Kv. Geol. Rep., 0. S.) Salt Sulphur-water, of the Lower Blue-Lick Spring, Nicholas County. Pagle 583, of Laboratory book (unpublished). Sulphur-water, from Sebree Springs. (b.) Clzavlibeaze Wi/lers. No. 954. (Vol. IV. p. 142, Kv. Geol. Rep., O. S.) Chalybeate water, north-west sice of Sweet-Lick Knob, near Irvine, Estill County. Page 5SI, of Laboratory book (unpublished). Alunm Spring (No. i0, Crow's Station (on the E. 0. and N. Railroad). Coal-measures formation. Da- viess Countv. Page 5SI. (Ibid.) Sweet Spring (No. 6). Ibid. Page 524. (Ibid.) Chalybeate water, from 'Murray's Spring, near Lewis (E. 0. and N. Railroad), Daviess County. No. 53I. (Vol. II. p. 233, Ky. Geol. Rep., 0. S.) Chalybeate Mineral- water, from the Grove Spring, in the yard of the proprietcr of Crab- Orchard Springs, Mr. Caldwell, Lincoln County. No. 532. (Ibid., p. 234.) Chalvbeate water, from the Brown Spring. half a mile from Crab-Orchard Springs, on the Lancaster Turnpike, Lincoln Countv. Page 527, of Laboratory boo., (unpublished). Chalybeate water, from Rock- DESCRIPTION OF TABLES. castle Springs, Pulaski County. From a natural spring on the west side of Rockcastle River, near its margin. L. Renfros', near Cumberland Falls. Page 584, of Laboratory book (unpublished). Chalybeate spring, Sebree Springs, of Webster County. (c.) 5a/ilze Wa/eders. P'age 58I, No. 4, of Laboratory book (unpublished). Water from the Brick Spring, at NMr. Hickmnan's Springs, Crow's Station (E. O. and N. Railroad), Daviess County. No. 535. (Vol. II. p. 236, Ky. Geol. Rep., 0. S.) Mlineral-water, from the Epsom Spring, one mile from Crab Orchard, on the Lancaster Turn- pike, Lincoln County. No. 536. (Ibid., p. 237). 'Mineral-water, from the Epsom Spring at Foley's, half a aiile from the centre of Crab Orchard, on the Fall-Dick Road. C L A Y S. (See Table VIII.) No. x337. (Vol. I. p. 179, Ky. Geol. Rep., N. S.) Fire-clay. Average sample from thie upper four-foot bedl; the whlole bed eight to ten feet thick; on both sides of the hills ; ridlge between Grassy and Three-Prong Creeks Boone furnace propcertv, Carter County. No. 1338. (Ibid.) Fire-clay, from same locality. From the lowver bed. N-O. I339. (Ibid.) Fire-clay, from same locality; the rougher part of the upper aver. No-. 1340. (Ibid., p. i8o.) Fire-clay, under coal, Old-Orchard diggings, Boone furnace property, Carter Count!y. -No. I34I. (Ibid.) Fire-clay, from same locality as Nos. I337, 1338, and 1339,-- the dlark-colored clay from the lower portion of the deposit. Carter County. N-O. 1342. (Ibid.) Fire-clav, tinder the twelve-inch coal, on Geo. Ossenton's land(, near Gravson, Carter County. Page 5oo, of Laboratory book (unpublished). Clay, from a bed seven to eight fe!et thick, in the Chester group of the Subcarboniferous Limestone, on SowNder's farm, one mile north of Green River, on Caney Branch, Ed- monsort County,-tthe upper or light dove-colored portion of the bed. Page 5oi. (Ibid.) Clay, from the same locality,-the second layer; li-ht-gr-L' or nearly white. Page So2. (Ibid.) Clay, from the same locality ; the third or gray layer. The lowvest layer is of an olive-gray color, and contains about 2.5 per cent. of Potash, and nearly one per cent. of Lime. N-o. I477. (Vol. I. p. 236, Ky. Geol. Rep., N. S.) Fire-clay. Louder's Bank, near Kenton furnace, Greenup County. No. 1479. (Ibid., p. 236.) Clay. Fourth bed above the Limestone and 96 BUILDING-STONES. 97 Limestone ore, on Pea Ridge, Greenup County. Thickness of this bed, two to two and one-half feet ; weathers, white ; two hundred and fifty feet above the railroad at the depot. Hunnewell furnace. No. 1481. (Ibid., p. 236.) Clay. Second bed above the Limestone ore, on Pea Ridge, &c., Greenup Cumnty. No. 1483. (Ibid., p. 237.) Fire-clay. Thomas's Bank; upper layer; an average sample; five feet above the cherty Limestone. Head-waters of Wing's Branch of Schultz Creek, Greenup Count)'. Page 668, of Laboratory book (unpublished). Clay, from the head-waters of Green River, in Lincoln County, from a bed represented to be of great thickness, resting on Black Shale. Page 65i, of Laboratory book (unpublished). Potter's Clay; No. X quality Upper Silurian formation. Waco, nine miles east of Richllond, Madison County, Ky. Page 65I (a), of Laboratory book (unpublished). Potter's Clay; same lo- cality; of quality No. 2. BU[LDING-STONES. (See Table IX.) Linmes/ones. No. i638. (Vol. I.p. 291,Ky. Geol. Rep., N. S.) Magnesian Limestone, used for the foundation of the Court-house, Paris, Bourbo-l County. Lower Silurian. From Cane Ridge, five miles east of Paris. No. 494. (Vol. II. p. 143, Kv. Geol. Rep., 0. S.) AMagnesian Limestone, on the road from Shepherdsville to Mount XWashinton, Bullitt County. Upper Silurian formation. No. 1314- (Vol. 1. p. i69, Ky. Geol. Rep., N. S.) Limestone, from Barren River, near the mouth of Gasper Creek. Subcarboniferous formation. Butler CouLnty. No. 1388. (Ibidl., p. 192.) Limestone, used as a flux at Boone Furnace, Carter County. No. 1421. (Vol. I. p- 152, Ky. Geol. Rep., N. S.) Odlitic Limestone. Glasgow vFunction, Barren County. Upper layers of Upper Subcarbonif- erous Limestone. No. 1422. (Ibid., p. 152.) Compact Limestone. Upper Subcarboniferous Limestone. Glasgow Junction, Barren County. No. 512. (Vol. II. p. i69, Ky. Geol. Rep., 0. S.) Limestone, Building- stone, from Grimes' Quarry, on the Kentucky River, near Clay's Ferry on the Richmond Road, Fayette County. Lower Silurian, Magnesian Limestone, used in the construction of the Henry Clay Monument in the Lexington Cemetery, &c. No. 6i6. (Vol. III. p. 259, Ky. Geol. Rep., 0. S.) Magnesian Lime- stone, from Harris' Quarry on Elk Lick, about one mile below Clay's Ferry, and about one and one-half miles in a straight course from Grimes' Quarry on the Kentucky River, Fayette County. 13 9s DESCRIPTION OF TABLES. No. io9. (Vol. I. p. 323, 0. S., Ky. Geol. Rep.) Limestone from Brushy Fork of Tygert's Creek, utnder the Limestone ore. Used as a flux at New Hampshire furnace, Greenup County. No. 1500. (Vol. I.p. 241, N. S., Ky. Geol. Rep.) Limestone, Subcarbonifer- ous average sample ; used as a fltux at Kenton furnace, Greenup County. No. 530. (Vol. II. p. 227, 0. S., Ky. Geol. Rep.) Magnesian Limestone, building stone ; Upper Silurian formation. \Vh'ite-Oak Ridge at Pleasant Grove meeting-house, Win. Galey's farm, Jefferson County. No. io65. (Vol. IV. p. iS9, 0. S., Ky. Geol. Rep.) Variegated Lime- stone, near the base of the Upper Silurian of Jefferson County. Three miles from Middletown, on the Shelbyville road. NO. 1123. (Ibid., p. 212.) Magnesian Limestone, a good building stone, from Mr. Covington's farm at Elliston, Madison County; where the Red-bed soil was collected. (Devonian) No. i64. Marble. (Vol. 1. Kv. Geol. Rep., p. 358, 0. S.) Coon Creek on the Ohio River, opposite to MNarble-Hill quarry of Jefferson County, Indiana. Quarry of Dr. Hopson, Trimble County. No. 776. (Vol. III. p. 409, 0. S., Ky. Geol. Rep.) Limestone. The lowest rock in the bluff at Slhryock's Ferry, Kentucky River, Versailles road, Woodford County. Lower Silurian formation. There are also some good building stones in the Clinton group not yet analyzed. Sands/ones. (See Table X.) No. 496. (Vol. II. p. 144, 0. S., Ky. Geol. Rep.) Sandstone. Building stone from the Knob at Bullitt's Lick, Bullitt County. Waverly formation. No. 467. (Ibid.) Sandstone. Building stone from a quarry on the top of Button-mould Knob, Bullitt County. No. 468. (Ibid., p. I45.) Sandstone from seventy feet above the Shale at Bellemont furnace, Bullitt County. N'o. 1221. (Vol. IV. p. 252, 0. S., Ky. Geol. Rep.) Sandstone. Knob building-stone mouth of Triplett's Creek, edge of Rowan County. HYDRAULIC CEMENT. Limestones. (See Table XI.) NO. 4_6. (Vol. II. p. 208, 0. S., Ky. Geol. Rep.) Magnesian Limestone. Hydraulic Limestone. Two miles west of Grayson Springs, Grayson Countv. No-. 522. (Ibid., p. 220.) Hydraulic Limestone (unburnt) from the falls of the Ohio River at Louisville, Jefferson County. HYDRAULIC CEMENT. 99 No. io66. (Vol. IV. p. 189, 0. S., Ky. Geol. Rep.) Hydraulic Limestone. Chenowick Creek, Jefferson County. No. 1137. (Ibid., p. 2i9.) Hy( raulic Limestone from Mitchell's Spring, Meade County. C(liff three hundred feet above the Ohio River. No. ii65. (Ibid., p. 23i.) Hydraulic Limestone from Bardstown, Nelson County. Nuo. 1201. (Ibid., p. 244.) Limestone from one mile north-east of La Grange, Oldiham County. Upper Silurian. No. 1202. (Ibid.) Hydraulic Limestone, Curry's Fork of Floyd's Creek, Oldham County. DESCRIPTION OF THE MAPS ACCOMPANYING THIS PAMPHLET. Two mrps are given herewith, one a general map designed to show the position of the Commonwealth of Kentucky, with reference to the other parts of the Coitinent of North America. It will be seen from this map that the most important points are as follows: - I. Its central position, with reference to the whole country; it being very nearly in the middle of the great fertile section of the continent. The pres- ent centre of population is probably at or very near the northernmost point of the State. 2. The relation of this Commonwealth to the natural transportation routes of the coUntry,-its great rivers. There can be little doubt that, as this countrv becomes more and more peopled, the commerce will become more limited to the north and south channels. This will necessarily give a con- tinuallv-increasing importance to the commercial relations of Kentucky. It should be noticed that the shores of the Caribbean Sea and the Gulf of Mexico are in peculiarly favorable relations for commerce with the Missis- sippi Valley. A geological map would show that the most favorably-situated deposits of coal and iron for the supply of this great region lie within the central district of the Mississippi Valley, of which Kentucky has so large a share. The large map of the State of Kentucky, bound with this pamphlet, is designed to show the special geography and geology of the State. It is a compilatiol from various sources, but is largely based on the work of the present Survey. Geologically and topographically it is much in advance of any other map of the State that has been made. Where the geological indi- cations are given by coloring or shading, they may be trusted as approxi- mately cor-ect. All such work is from the results of the Kentucky Survey. Some parts of the outcrop lines are left undetermined. These, it is ex- pected, will be surveyed within two or three years. The topography of the State is still the most doubtful part of the wvork. This region has never been surveyed in its entirety in any fashion. There was no Government Survey in the beginning. During the war some lines of roads were run. The Geological Survey has mapped in some detail about five thousand square miles; but it is not possible to construct an accurate map at present. The errors at present may be reckoned as putting the position of nearly every point in doubt. The average error of position will not fall far short of two miles. The general relations of streams, towns, and roads is, however, given with sufficient accuracy for the purpose in view. For the better understanding of this map, the reader is referred to the first pages of this pamphlet. COLLECTIONS AND PUBLICATIONS OF THE KENTUCKY GEOLOGICAL SURVEY. THiis survey, begun as a preliminary reconnaissance, in 1854, was interrupted by the war, and its records destroyed by fire. InI 1873 the work was resumed. The collections and publications herein re- ferred to leave been prepared since the close of the year 1873. The specimens shown at the Centennial Exposition comprise only a part of the total collections made (during the progress of the work. The large map exhibited with the collection shows the distribution of the rocks of the State, as far as yet determined. The specimens of coal, ore, &c., represent only the beds and other deposits that have been opened, in the present state of the industries of the State. It is lprobable that, when complete explorations have been made, the aggre- gate mineral wealth will be many times greater than is shown here. Attention is called to the following publications of the Kentucky Survey, already issued or in preparation. These reports, memoirs, maps, &c., will be furnished at the cost of printing. Applications should be made to the Secretary of the Geological Survey, Lexington, Kentuckv. List of f/he Pulicalions of the .Surzc) a/readi printed or in preparation. Reports of thie Geological Surey of Kentucky, all in royal 8vo. VOLUME I. NEW SERIES. I. Report on the Timber Growth of Greenup, Carter, Boyd, and Lawrence Counties, in Ealstern Kentucky. By N S. Shaler, and A. R. Crandall, Assistant. II. Report of the Botany of Barren and Eclmonson Counties. By John HusseN, B3otanical Assistant. With an Introduction tby N. S. Shaler. III. Report on the Iron Ores of Creenup, Boyd, and Carter Counties, the Kentuckv Diivision of the Hanging Rock Iron Region. S Plates. By P. N. Moore, Assistant. IV. Chemical Report of the Soils, Marls, Clays, Ores, Coals, Iron Furnace Products, Mineral Waters, &c., of Kentucky. By1 Robert Peter, M.D., &c., Chemist to the COLLECTIONS AND PUBLICATIONS. Kentucky Geological Survey. Assisted by John II. Talbutt, S.B., Chemical Assistant. The First Chemical Report in the New Series, and the Fifth since the btginning of the Survey. V. The Iron Manufacture of the Kentucky Division of the Hanging Rock Iron Region. I Plate. By P. N. 'Moore, Assistant. VI. Report on the Geology of the Region adjacent to the Louisville, Paducah, and South-w-estern Railroad, with a Section and 4 Plates. By Charles J. Norwood, Assis z:ant. VII. Report of a Reconnoissance in the Lead Region of Livingston, Crittenden, and Caldvell Counties, including a sketch of their General Wealth. Map and 4 Plates. By Charles J. Norwood, Assistant. VOLUME II. NEW SERIES. I. Report on the Geology of Greenup, Carter, and Boyd Counties, and a part of Lawrmnce. With Map and Sections. By A. R. Crandall, Assistant. II. On the Geology of the Edmonson Coal and Iron District. With 'Map and Sections. By P. N. Moore, Assistant, and J. R. Proctor; with -Map by XV. B. Page, Assistant, and C. NV. Beckham and John B. Marcon, Aids. III. On the Chemistry of the Hemp Plant. By Dr. R. Peter, Principal Chemist of the Survyv. IV. On the Airdrie Furnace. By P. N. Moore, Assistant. V. Topogiaphical Report of IV. B. Page, Assistant, for the year 1874. V O. On the Geology of the Line of the proposed Railway from Livingston Station to Cumberland Gap. Wdith Sections. By A. R. Crandall and C. J. Norwood, Assistants. VII. Geologv of the Henry County Lead District. W'ith Sections. By N. S. Shaler, and C. J. Norwoocl, Assistant. VIII. On the Geology of the Route of the proposed Lexington and Big Sandy Railway. WNith Sections. By A. R. Crandall, Assistant. IX. A General Account of Kentucky. By N. S. Shaler and Assistants. Maps and Sections. VOLUME III. NEW SERIES. I. Report of N. S. Shaler, Director, on the Conduct of the Survey for 1873. II. Biennial Report of N. S. Shaler, Director, for the years IS74 and 1875, giving a summary account of the principal economic results of the Survey during those years. III. Notes on the various Scientific Problems encountered in the prosecution of the Kentucky Geological Survey. By -N. S. Shaler, I)irector. IV. Plan for the organization of a State Cabinet. By N. S. Shaler. V. Description of the Preliminary Geological Map of Kentucky. By N. S. Shaler, Director. VOLUME IV. NEW SERIES. I. Second Chemical Report of Dr. R. Peter and John II. Tallbutt, Assistants. II. Report: on the Geology of the Counties of Bath, Menifee, Powell. and Lee. With Map and Sections. yv A. R. Crandall, Assistant. III. Report on the Iron Ores in the Region near Cumberland Gap. XWith Sections. l,v '. N. Moore, Assistant. IV. Repor-: of the Results of a Reconnoissance of the State Line from Cumberland to Pound Gal), and on a Line from Abingdon, Virginia, to 'Mount Sterling, Ken- tucky. B-y P. N. Moore, Assistant. 102 COLLECTIONS AND PUBLICATIONS. V. Report on the Breckinricdge Coal M'ines. By C. J. Norwvood, Assistant. VI. Report on the Geology of the Kcntucky Red River Iron District. With Sec- tions. ,v P. N. Moore, Assistant. VII. IPreliminarv Report on the Geology of Martin County. With Sections. By A. R. Crandall, Assistant. VIII. Report on the Geology of the North and South-running Railways of Weszern Kentucky. With Sections. By C. J. 'Norwood, Assistant. IX. To)pographical Report of WV. B. Page, Assistant, for I875. VOLU'ME V. NEWY SERIES. I. Report on the Building Materials o5' Kentucky. By N. S. Shaler, and J. R. Proctor, Assistant. W\ith Map and Sections. II. Report on the Geology of the Sec;.ion from Grayson County to the Ohio River. Be 1P. N. Moore, Assistant. Map and Sections. III. Report on the Improvement of Kentuckv Rivers, with special reference to Navi- gation, Water Power, and the Prevention of Floods. By N. S. Shaler, and W. B. Page and J. R. Proctor, Assistants. IV. Report on the Geology of the Region adjacent to the Louisville and Nashville Railway and its lbranches. By C. J. Norwood, Assistant. WVith Map and Sections. V. Report on the Geology of the Region adjacent to the Cincinnati Southern Rail- wav. By N. S. Shaler and Ass;stants. W!ith Map and Sections. VI. Report on the Mineral WVaters of Kentucky. By Robert Peter and J. II. Talbutt, Assistants. V II. Report on the Coal Measures Section between Slate Creek and the Virginia Bor- der. By A. R. Crandall, Assistant. Map and Sections. VOLUME V-(. NEW SERIES. This volume will be devoted to a special class of Reports, prepared with reference to the International Exhibition at Philadelphia, and designed to bring the results of that Exhibition to hear on the questions of mining, commerce, and other interests in Kentucky. It is not possil)le to announce the precise limitations of these Reports; but, as far as pos- sible, they will be made to include the fo'lowing classes of facts:- I. Th e Managremnent of Surveys, Topographical, Geological, &c. II. The Arrange- ment of Collections to illustrate resources. 1II. The Working of Coal, Iron, and other Ecornomic 'Mineral Deposits. IV. The Use of Building Materials. V. Agricultural Geology. History of Soils, Marls, &c., Commercial Manures. VI. Metallurgy of Iron, Lead, &ic. VII. The Improvement of Navigation in Rivers. IMEMOIRS OF THE GEOLOGICAL SURVEY OF KENTUCKY. VOL. I. All in 4to. I. On the Antiquity and History of the Caverns of the Ohio Valley. I Plate. By N. S. Shaler, Director. II. On the History of the Buffalo, with special reference to the Fossils found at Big Bone Lick. Mlap and 12 Platcs. By J. A. Allen. III. On the Fossil Brachiopods of the Ohio Valley. Part I. S Plates. By N. S. Shaler, Director. IV. On the Prehistoric Remains of 'Kentucky. Part 1. 7 Plates. By Lucian Carr, Assistant, and N. S. Shaler, Director. 103 COLLECTIONS AND PUBLICATIONS. MEMOIRS. VOLUME IL. I. On the Prehistoric Remains of Kentucky. Part II. By L. Carr, Assistant, and N. S. Shaler, Director. Map and Plates. II. On the Fossil Corals of the Family Calceolidx. By N. S. Shaler, Director. Map anc 4 Plates. III. On the Cavern Animals of Kentucky. By A. S. Packard and F. A. Sanborn, Assistants, and others. 4 Plates. IV. On the Fossil Brachiopods of the Ohio Valley. Part II. By N. S. Shaler. Maps. 8 Plates. V. On the Cavern-dweiling Races of Kentucky. By F. W. Putnam, Assistant. 6 Plates. VI. History of the Investigations into the Affinities of Cavern Animals. By H. A. Hagen. VII. On the Dynamic Geology of Kentucky. By N. S. Shaler, Director. Maps and Plates. A few copies of the volumes of the first series of Reports made between 1&54 and I860, now out of print and extremely scarce, can be furnished to those who desire to complete such sets of Reports. Persons desiring information concerning these Reports, or any other information concerning the natural resources of Kentucky, with a Xview to immigration or to the investment of money in the State, should address Kentuckv Geological Survey, Frankfort, Kentucky. The order of arrangement of the Reports in the fourth and fifth volumes, as well as their titles, may vary somewhat froni the list as above given ; but the changes will be only matters of (detail. It is expected that all of the above described matter will be printed by December, 1 877. These Reports wvill be furnished, each part separately, in paper bindings, or as volumes bound in cloth or paper, as may be desired. The first volume of the Reports, and the first of the Memoirs, will be ready July 1o, 1876. The second and third volumes of the Reports will be ready October ist, I876. 104 I I I I IIivf I I I ft; k 7f24' 4A 2 i i I