xt737p8tb92z https://exploreuk.uky.edu/dips/xt737p8tb92z/data/mets.xml Kentucky Geological Survey. 1876  books b92-275-32007847 English Press of J. Wilson and son, : Cambridge [Mass.] : Contact the Special Collections Research Center for information regarding rights and use of this collection. Kentucky Description and travel. Geology Kentucky. General account of the commonwealth of Kentucky  / prepared by the Geological Survey of the commonwealth for the Centennial exhibition at Philadelphia, 1876. text General account of the commonwealth of Kentucky  / prepared by the Geological Survey of the commonwealth for the Centennial exhibition at Philadelphia, 1876. 1876 2002 true xt737p8tb92z section xt737p8tb92z 



           CIF THE



                 Rich Low Soils,
                 50 to 500 feet.

Variabls S.', s, geuterally of good
        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

'. ./ 

= 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









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                  OF THE


             PREPARED BY THE


               FOR THE

    Crntennial K.xbibition at pbilabrIpbia.

               I 8 76.


 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.,



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,
  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
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.




             GENERlAL ACCOUNT

                          OF THE



  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



seventy-five miles from the mouth of the Mississippi, and its
eastern boundary is within five hundred miles of the Atlantic
   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




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.




   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.




   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




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




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.




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.




  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
  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-
  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."




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-




                            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
  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-




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



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 soi