o '
ILLINOIS STATE GEOLOGICAL SURVEY
3 3051 00003 5240
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in 2012 with funding from
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http://archive.org/details/structureofherri88payn
State of Illinois
Dwight H. Green, Governor
Department of Registration and Education
Frank G. Thompson, Director
Division of the
STATE GEOLOGICAL SURVEY
K. H. Leighton, Chief
Urbana, Illinois
No. 88 CI R C U L A R December I9I+2
STRUCTURE OF HERRI N (NO. 6) COAL BED IN
MACOUPIN COUNTY, EASTERN GREENE AND JERSEY,
SOUTHEASTERN SCOTT, AND SOUTHERN MORGAN
AND SANGAMON COUNTIES, ILLINOIS
By
J. Norman Payne
With Discussion of
OIL AND CAS POSSIBILITIES
By
William H. East on
CONTENTS
1. Circular 88 — Structure of Herrin (No. 6) Coal Bed in Macoupin County,
Eastern Greene and Jersey, Southeastern Scott, and Southern Morgan and
Sangamon Counties, Illinois, by J. Norman Payne; with Discussion of Oil
and Gas Possibilities, by William H. Easton.
2. Tabulated Coal Data to Accompany Circular 88.
3. Plate 1-— Graphic Section from Southeast em Jersey County to Northeast
of Carlinville, Macoupin County. (Filed separately - unbound)
4.. Plate 2 — Graphic Section from Scottville to Northeast of Carlinville,
Macoupin County. (Filed separately - unbound)
5. Plate 3 — Graphic Sections showing Correlations of Pennsylvanian Key
Beds in Certain Wells and Borings in Macoupin and Southern Morgan
Counties. (Filed separately - unbound)
6. Plate U — Structure Map of Herrin (No. 6) Coal Bed in Macoupin County,
Eastern Greene and Jersey, Southeastern Scott, and Southern Morgan
and Sangamon Counties. (Filed separately - unbound)
un
Fig. i
INDEX MAP
LEGEND
COAL MEASURES BOUNDARY
BOUNDARY OF DEEP PART OF BASIN
V/A/\ AREAS COVERED BY STRUCTURE MAPS
MX A OF TOP OF HERRIN (NO. 6) COAL
ACCOMPANYING CIRCULARS 24,42,58,71
AND 88
MAP IN PREPARATION
STRUCTURE OF HERRIN (NO. 6) COAL BED
IN I.IACOUPIN. COUNTY, EASTERN -GREENE AND JERSEY,
SOUTH EASTERN SCOTT, 'AND SOUTHERN MORGAN
AND SANGAMON COUNTIES, ILLINOIS
By
J. 'NORMAN PAYNE
This circular presents a brief discussion of the structural
features of the Kerr In (No. 6) coal bed. in Macoupin County and in
parts of adjacent .counties on the west, and^ north (fig. 1), and also
a brief consideration of the Pennsylvanian stratigraphy of the area
The' north and south boundaries are respectively the north line of
T. li(- N., and the south line of T. 7 N., and the east and west boun-
daries are respectively the- east line of R... 6 W-. and the west line
of R. 11 W of the- -Jrd P'. M. '.-.•'
The area lies within a relatively short distance of St.
Louis and East St. Louis and Is traversed by the main lines of
several railroads that connect St. Louis and Chicago. It Is well
supplied with excellent highways . Thus convenient and cheap trans-
portation to markets is available. :
Coal Mining
This region is an important part of the Illinois coal field.
Most of the coal production, however/ has been from railroad or ship-
ping mines located in Macoupin County. The county's total production
from 1832 to 1930 was 173 ,985., 'Z%k tons (21).*-, -giving it -fourth rank
among coal-producing counties in Illinois." Since 1930> ^ ^s ranked
from second to fifth in various years with a fairly constant annual
production of about 3 l/2 to l\. million tons. In 191-1-0, ten shipping
mines produced coal from Macoupin County (22); In 1920, at the height
of coal-mining activity in Illinois, 17 shipping mines were in oper-
ation. About two-thirds of the coal produced in the entire area Is
from "captive" mines operated by one of the large v/estern railroad
companies, but none of this coal enters the general' market . Until
recently, two other large mines were also "captive" mines owned by
a large oll-ref ining company,- but these- •mines" "have been Idle for
several years. Their recently reported acquisition by a large coal
company presages early increase in coal production. A number of the
mines in the region, however, have been in operation for many years,
several for more than 35 years; mining. in them .is approaching
p For references, see bibliography, page-7
Page 2.
II o new shipping
n1 Q-4.n^ soon. II o new snippet
property boundaries and pr obab ly^ill ^oon^ ^ ^ . ^
Sines have been opened in *ho reg.. ^ rcgervc.
abundant supply of cod suu
Minable Goal Beds
1 <Q mainlv from the Hcrrin (No. 6
Coal production in this area is mainly ir Colchester
oql bed A few small local mines work the No. i+ £ thcsG lov;er
(No: 2 coal bed in the western £?.**£ .'at Me dor a has produced
c'ai bids li^^^^fabout^O JoS below the Colchester (No, 2)
coal from a coal oca iy^b . . »
bed (Pi. 5, Macoupin County No. 17W f
v -, -u ^ ^ « fi-onrrallv absent in tnis.
The Springfield (No. 5) coal'*c* fcJ» slato"" (one or both of
are, except for aVin.bed of coal -^ ^ of drlll_holCs
which probably ^present the No^ 5 |° ^ 1} .
scattered throughout the arc. ipj.
*>,o nxtent of the llo . 6 coal bed,
The following table shows trie cx^ni\ reservc tonnage
of thickness of the coal bed.
' County
Greene
Jersey
Macoupin
Morgan
Sangamon
Average
thickness
Feet .
k
I
I
EL
(hi)
CoalJReservea
(5*0
(6|)
(3f)
(6t)
Area under-
lain by No. 6
coal bod.
Square miles
150
160
Area of
No. 6 coal
r.iinc d out .
Sq. miles'
1+-
1*
58-
1+
10
Reservc
area
Sq. miles
Total Reserve
1,199
Reserve
tonnage.
ilillion
tons
7,086
the reserves ox cod ^^
present •
,, rl.nhprs refer' to map
# County well numbers
and well logs.
(pi. k)f- tabulated well data,
Page 3 .
Coal "beds below the Hcrrin (No* 6) bed. - At Me dor a, a
shaft was sunk to a coal bed lying approximately 130 to. li|.0 feet
below the horizon of the No. 6 coal bed, about 20 feet below the
Colchester (No. 2) coal bed, and a few feet above a thin layer of
limestone. This coal bed, designated as the Mcdora, is regarded
as the equivalent of the thin fairly widespread Wiley coal bed in
western Illinois, where it lies some distance below the Colchester
(No. 2) coal bed and a. short distance above the thin persistent
Seahorno limestone (20).. The Medora coal bed has been reported in
a number of logs of drill-holes located within this area (table 1).
The Colchester (No. 2) coal bed mined in the western part
of the area is believed to be the bed which to the east is reported
in drill-holes at a position 20 to 3° feet above the Medora coal,
which latter bed is identified by reference to its underlying thin
limestone, as noted above. The altitude, depth, and thickness of
No. 2 coal and Its distance below Herrin (No. 6) coal bed are pre-
sented in the tabulated data accompanying this report and in
table 1. These data indicate that this coal bed lies fairly uni- -
formly 80 to 90 feet below the Herrin (No. 6) bed but that locally
the interval Is 100 feet or more. In general, the coal beds are
approximately . parallel . The Colchester (No. 2) coal bed has been
mined for local use at many places west of the line of outcrop of
No. 6 coal bed In Greene County near Roodhouse, as indicated by
the map and tabulated data. Where mined, It Is generally about 30
inches thick.
The designation "No. I4." . is applied loosely to two thick
lenticular bodies of coal, one of which has been 'worked near Rood-
house and the other near Greenfield, and both of which appear to
lie only a short distance below the position of* the Springfield
(No. 5) bed. These lenticular bodies of" coal have been mined for
many years but only for local trade. The coal bed at Roodhouse
was reputed to furnish a block or "cannel" coal of special quali-
ties, possibly because part of the bed is somewhat canncloid. In
the" Greenfield lens, the. bed attains, a thickness of nine feet
(Greene County Nos . 3 and 7^) • The No. J4. coal .bed or horizon lies
between I4.O and 60 feet below the top of the Herrin (No. 6) bed, but
is not recorded in all drill records. In western Illinois there
are locally two lenticular beds at this general position, and it is
possible that the same relationship may exist In Greene County. In
any event, this is a bed of very local commercial importance.
Key Horizons
The general close parallelism of most of the Pennsylvanlan ■
strata make limestones of definite stratigraphio position valuable
as key horizons for estimating the depth to the Herrin (No. 6) coal
bed or other workable 'beds at points where such limestones outcrop
Page 14-.
identified.
Scottvill^imosLono. The li«st- for *i£*to^
— S2ott^11^ i^S? Sf ^tE^SS^S- northwestern
Apple Crook and its triout-ries in vlliare of Scottville.
Macoupin counties in the vicinity of the viii-Se beon
This limestone is lithologloally siniW to one n ^ ^
called the Carlinville Intone (11) and which cr p^ ^ ^
SpoLfof^cnnsnv^iaA ££%&? Macoupin Creek (pi. 1, M»
R. Ball Section) .
£ +-hin bed of coal is present about J+0 feet below the
the Carlinville liracstcne with sandy sh alo beds 1 ^ ^ of
both stratigraphic positions <Pl;;' i*^',?' *ln interpreting the
stratigraphic succession leads to confusion in im, e p u
less than that from the°f^n^^_^s which penetrated more
?f * ?rtoC22°5rxeeteof PennsySa^Ln Strata overling the Herrin
C 1 °eoal2bedfc°™iy shi -o limestones the "pper one of
which is undoubtedly the carlinville l«£f°™' ££, re3peotively
about 100 feet lower. Thus, the t«o ine t ones n v ^
the same relationship to No. 6 coal g^stono near
limestone near Carlinville <~nd the Jcottviii rcportod in
Scottville. The presence 01 two such iik-J or„thor with the field
the records of drill-holes (^•^J»^0££££ag tho3e Um0_
relationships as dos;rl^ed'.^s"„ttville limestone lying about 100
feerbelow^rcarlinvi^le^nd^about1^ fee? abov/the Herrin
(No. 6) coal bed.
i- • n « Tinoo-t-nno is prav to dark gray in color,
The Scottville limestone is gi^ ^ ^nbablv con-
County (table 1 and pis. 1, 2, 3).
TOP OF HERRIN CNO 6) COAL TO TOP OF CARUNVILLE LIMESTONE
TOP OF HERRIN CNO 6) COAL TO TOP OF TRIVOLI CNO 8) COAL
Fig. 2
isopach maps showing
thickness of intervals from
TOP OF HERRIN CNO. 6) COAL TO TOP OF
CARUNVILLE LIMESTONE, TRIVOLI CNO 8) COAL,
AND SCOTTVILLE LIMESTONE
IN MACOUPIN COUNTY
LEGEND
SUBSURFACE DATUM POINT
OUTCROP DATUM POINT
ISOPACH INTERVAL - 10 FEET
LINE OF CROSS -SECTIONS, PLATES I AND 2
APPROXIMATE BOUNDARY OF THE CARLINVILLE LIMESTONE
SCALE
TOP OF HERRIN (NO 6) COAL TO TOP OF SCOTTVILLE LIMESTONE
Pace 5
Carl invi lie limestone, -—The -name Carlinville refers to the
lowest limestone in an exposure of Pennsylvanian rocks along Macoupin
Creek in the S\7 I/I4. SW l/l+ sec. .55 , .T . 10 N., R. 7 17. , about a mile
southeast of Carlinville. The nomenclature reverts to that employed,
by Lee (11+) inasmuch as the limestone has since been called the Shoal
Creek (1 I: 10) . ■":.'■',.
.The name Shoal Greek is reserved for what is believed to be a higher
limestone that crops out along Shoal- Creek in the vicinity of Breese,. described •
by Udden in 1907 (18), and for what is thought to be the same limestone occupy-
ing the uppermost position in the succession of Pennsylvanian beds cropping out
southeast of Carlinville (pi. 1). To this limestone, the name La Salle has been
applied (10), but because definite proof of this inferred correlation is lacking,
the present report reverts to earlier terminology (12, 14). This, upper limestone
at Carlinville occupies the same relative position wTth~respect to the Carlin-
ville limestone that was given to the Shoal Creek in the early descriptions of . •.
geology of the Illinois mining districts, as published in the bulletins of the
Cooperative Mining Scries, particularly that describing the coal resources of
District VII (Southwestern Illinois) (12).
The Carlinville limestone inmost places lies from 1.30 to
20.0 feet above the Kerrin (No. 6) coal bed and about 35 to ^-0 feet
above, a. thin bed of coal ,which has been designated Trivoli .(No. 8).
(20.) (pis. 1-3) • This limestone member is well exposed by erosion
south and southeast of Carlinville, east of Palmyra., and in quarries'
and along streams north of Plainview. It is reported commonly in
records of drill-holes located east of R, 8 W., was encountered in
relatively few drill-holes in R. 8 W., and is not reported farther
west (table 1 and fig*. 2 '.) . r-.: ■ :
Macoupin coal and limestone beds., - The Macoupin (1_0 & 20)
coal bed is a thin layer of coal, generally less than 6 inches thick,
that lies 23O-25O feet above the Herrin (No. 6) coal bed and y0 -1+.0
feet above the Carlinville limestone (pis. 1-3* table 1). Overlying'
the coal bed is usually a black sheety shale ("slate") above which
is a thin layer of f ossilif erous impure shaly limestone. This group
of beds is of value as a key horizon, but it is, likely to be over-
looked by drillers unless they are unusually discriminating in their
observations. Its identification should generally be pos.sible in
cores or in drill-cuttings that are carefully collected*
Shoal Creek limestone. - The limestone herein regarded as
the Shoal Creek limestone lies I4.O to 60 feet above the Macoupin lime-
stone and as much as 535 ' feet "above the, Ilerrin , (No . 6) coal bed,
the. uanal distance helag -about ■ 300 ^feet In the three southern town-
ships of Macoupin County, and from 2^0 to 290 feet in the three
northern townships (table 1). This limestone member is usually about
10 feet thick, : in places being interbedded with shale,, especially
in the upper part,. It is rarely penetrated in drilling except in
the eastern tier of townships , whore it lies immediately beneath
drift, as it is the uppermost Pennsylvanian member. .in the area
(table 1). . , , . ••.' ■
Page 6.
Structural Features of Special Interest
With Respect to Coal Mining
Thp Herrin (No. 6) coal bed has a regional easterly dip of
from 10 to 15 t per mile. An outcrop of the coal bed in the
AMI sec. 15, T. 7 N R. 10 W., (Jers oy County
Wo ?7W has an altitude of 5^6 feet above sea-level, the hignesT;
ta;wn7kti?udr0f the coal bed in the area; the lowest recorded
nltitudc is 250 feet above sea-level, in the SW 1/1+ SVJ L/i\- bu i/M-
sec 15 T. 18 N., R. 6 W. (Macoupin County Well No. 136). The
intervening clistaAcc is about 25 miles, the average dip therefore
being about 12 feet to the mile.
The eastward dip is irregular, but it .rarely exceeds 15
feet per'mile! In a few places, such as ^JiSPSit^S 5lS!
north of Bunker Hill, it is locally as much as.'? £5 feet per mile.
Locally anticlines, domes, terraces, and basins are present. The
ioo«itnn and character of these structures are indicated on the
s^ctSre^ a^comP^g this report and should be carefully con-
sidered in choosing Sffes for mining operations.
From available information it appears that faults are rare,
of small displacement and brief extension, and because they are un-
?Lortant they have not been mapped. Small displacements of the
coal bed have been observed at numerous places in the mines in the
sSaunton - Gillespie region, but these faul t™ely effect £°
limestone caprock and arc usually associated with lenses ol gray
shale ?" soaps tono") occurring between the black shale and the coal
?ed between the black shale\nd the caprock, or adjacent to lime-
stoAo Sosaos or pendants protruding downward from the caprock.
The accompanying structure map has been constructed from
unevenly d?stribu?edydatum points. Drilling and mining operations
" concentrated in the cast half of the area; hence, it is
Possible to delineate the structure with greater accuracy and detail
in the east than in the west half. In order to eliminate the per-
sonal element sS far as possible, the contours have been drawn
mechanically that is, a constant slope is assumed to exist between
Sa?um poSl; and the 'distances between contours have been scaled
accordingly.
Revision of Present Map and
Preparation of Maps of Other Areas
The present map is the fifth of a series of maps showing
,hfl qtructure of Herrin (No. 6) coal bed in southern Illinois
(Circulars 2^^, 5" and V) . Like the others, it is a progress mafl
"ounTTw^ll numbers refer to map (pi. k) , tabulated well data, and
well logs.
Page 7.
on v/hich additions and corrections can bo readily r.iado . Because
of "new drilling and the occasional discovery of records of
earlier drilling, it is expected that additional data will become
available from tine to" time . It is hoped that the maps of two
more areas ' can be completed within the next two years. These maps
will delineate the structural features' in most of Montgomery,
Christian, Fayette, and Marion counties, and adjacent parts of
Sangamon, Macon, Shelby, Effingham, Clay, Wayne, Jefferson, Wash-
ington, Clinton', a'nd Bond counties.
Bibliography
Published information on the' geology of the Pennsylvanian
rocks and on the structure and occurrence' of the Kerrin (No. 6)
coal bed and associated strata in this area may be found in the
following publications :
1. Ball, John R., Some Pennsylvanian limestones of the Carlin-
ville cuadranglc, Illinois: Trans, Illinois Acad. Sci.,
vol. 2o\ p. 97, 193^-. . •
2. Bell, A. H., Notes on oil and gas possibilities, in Payne,
J. N., "Structure .of Hcrrin.(IIo. 6) coal bed in Madison
County and western' Bond, western Clinton, southern "
Maccupin, southwestern Montgomery, northern St. Clair,
and northwestern Washington counties," 111. Geo 1 . Surv.,
Circ. 71, pp. 9-21, 191+1.
5. Bement, A., Illinois 'coal : ■• Illinois Gcol . Survey Bull. ^G,
, pp. 15-14-5, 1929.
I4.. , • The 'Illinois 'coal field: Illinois Geol. Survey
Bull. 16, , pp. 132-202, I.91J4.. ...
5. Blatchley, R. S., Oil resources of Illinois, in DeWolf ,
- F; W., xt al: "Yearbook for l"909'r, Illinois Geol. Surv.
Bull. -16, 1910.
6. . ,, , 0,il and gas in Bond, Macoupin^ and
Montgomery counties: Illinois Geol, Survey Bull. 28, 19lt«
7» ", Oil resources 'of Illinois with special
reference to. the area outside the southeastern fields :
Illinois Geol. Survey Bull. l6, pp. 157, 173-176, 1910.
8. Cbllingwood, D. M., Oil and gas possibilities of parts of
Jersey, Greene, and Madison counties: Illinois Geol.
Survey. Rcpt . Iny. No. 50,, 1 93 3. .
Page 8.
tt t? Pn"i r-psourcos of District III (Western
■. • voi. 25, pp. il£?ik5» 3.953.;
tp tr 0+- ni Oil investigations in Illinois: Illi- -
U- Lay*nois Goo?! S™ (inncoopJation with U. S. Cool. Surv.)
Bull. 51, 1915«
~„ ^-r m'c-tT'ipf VTT (southwestern
, « -rr0„ p t-t Coal resources 01 District vxx ^uuw
12' ^'miSois): Illinois Roo^ Survey Coop Mxnxng Ser.
Bull. 11, pp. 13-Uo, 89-10.1, 216-22., 1922.
,, The Carlinville oil and gas field:. Illinois
*" G^oTT' Survey Bull. 20, pp. 81-95, 1915-
,l t„« v'Mll-ieo Geology and mineral resources 'of the
LLl. Lee, Wallace, UbUJ-uw _, -1 „ . tt q. n.nn . Survev •
4 Gillespie-Mount Olive quadrangles: U.S. Qpoi,n.surv©3
Geol. Atlas, Folio 220, 1926.
■ Coal in Gillespie and Mount Olive quad-
5* r angles, Illinois: Illinois Geol. Survey Bull . ,0, • •
pp. 051-59, 1917.
' Oil and gas In the Gillespie and Mount Olive
quadrangles, Illinois-: .. Illinois Geol. Survey Bull. 51,.
pp.. 7I-10?, 191^. '■
17 Melius L A., A restudy of the Staunton gas pool: I11I-
17 " Myl nois Geol.: Survey Bull. \&*29 VV-i 1919- .
18. Udden, Jon A., Notes on the Shoal Creek l^one : Illi-.
nois Geol. Survey Bull. 8, pp. H7-126, 1 )0 ( , ...
,r- ^ a tt Gpnlo^ical survey of Illinois: Greene -
19. Worthy A. .H., llf°lll%2_1337, i868; Jersey County . ;
™ fill pp. lot-121, i860; Macoupin County vol. J
pp. 2U6-505, 1073; Morgan County, vol. IV, pp. 1H-J 1°*>
1B7O; Sangamon County, vol. V, pp. 5O6-319, 1873-
20. V,anlcss, H. B.^.f^^^^^S^aSl^'^..
21 • A "'SfislroS .nelardresf roc^tf tneGcSr07tne year"
1930: Illinois State Department of Minos and Minerals:
p. 16, 1931.
22. Fifty-ninth eoal report of Illinois 19^0: Illinois State
Department of Minos and Minerals, p. 28, 19W-
16.
Page 9.
Table 1. - Tabulation of --intervals -between- top of -No. • 6 coal
and top of various key beds, and average
thicknesses of key beds in Macoupin County, j
...
- ■ * ' *
•-
T.
7 ft., R.
6 W.
T.
7 N.,- R.
7 W.
-
V
»
•
/
*
- •
, ^— ^
-•»
. > .
P*"^
rH
-p
•*] •
W
*H
p ,
* ! •
CO
'■■ erf
<V(
■ rH 1. -p
W
w
i erf
Cm
rM iJJ
ta
w
> Q-i
' — >
■■ erf • Ch
05
+£
> «H
v. ^ '
ecS Ch
0
■R
■• • ' U O
> ^H W
f^ ..
c •
'^ O
> c_ -^
£
Pi
03
rH
fc o ■'.:
S
•H
CD
H
Sh o
^
•H
P &(
trf
0 : i— I
O
O
-P P*
erf
, 0 rH
o
O
■ ti O
O
-P ,&, erf
•H x)
di
■ Co
o -
+5 P^;crf
•H T3
P^
• H -P
O ' -
M .O O
si 0 .
•H p>
o
Jh o o
^ O
•H fp O
-P rO .'
|
•H 4-3 O
+3 rO
6
Cm O
CO
)
3
Cm O
CO
3
"■ o -p
0) :o <d
0 Cm
-P
O -P
o O'to
0 Cm
■p
•
tiOtP
bO O
erf
.
fafl-P
hfl O
• erf
<D T3
o
<rf •
erf
T3
0 T3
o
rf : •
erf
tJ
UO 0
|21
inlti O
M
bD ©
S
^ -d :0
U
£ ,0
CD .0 &
Q>
•
M rQ
© 0 .£5
0
•
Oj,
> ^
>
A
erf
> ^o •
t>
O
Bed
Pi '
5 '
■ •§?" '
*^
r--«
" <tj
s
(Above
No. .6 coal)
|
Shoal Creek Is.
301-314
306
'19' 3!
; ':■ '--
Macoupin coal
217-241
253 •■
5" 6:'
■ •'•-:-
I i
.
Carlinville Is.
194-212
205
7' 9
202-216
209
, • ■ 6 ',
10.
No. 8 coal
152-165
161
5" 5
160-175
168 '
5T . .
.' 7
Scottville Is.
' *. •
78-93 •
8E
2',
7
Scottville coal
66 •
..■4" 1.
60-71 -
66
6" •
4 .
Piasa Is.
52-55
42
4' 11
35-47
41
4'
26
No. 7 coal
32-40
33
7" 9
26-36
32
"'1V^«''
18
Horizon of top of No. 6 coal from which measurements .are mad'e.
(Below No. 6 coal
)
,
No. 5 coal
26 Bk. si.
1
'
No. 2 coal
91-93
92 2'-3"
2
85-94
8.8
n-6.1*
> 3
Medora coal
134-144
1&6 2 '-5"
3
130-134
132
l'-6"
2
Seahorne Is.
136-138
157 2'
2
135-137
136
5'
3
page 10,
Table 1. - (Continued)
Bed
Shoal Creek Is.
Macoupin coal
Carlinville Is
No. 8 coal
Scottville Is.
Scottville coal
Piasa Is,'
No. 7 coal
rH
crf
>
m
•H
Cm
O
-P
Cm
Cm w
O
rM
Ct, erf
O O
-P O
<o
o xi
m -D
3
P3
T. 7 N., R. 8 W,
198-2Q5
156-168
35-39
18-32
rH +J
erf c_
t> Cm^,
U Q
<D H
+3 cl, erf
a O O
•H -P O
co o
hO-P
erf
Jr. -d
o ©
> ,a
CO
w
co
o
XI
o
-P £>
© Cm
faO o
o
CO
-P
M
• H
O
-P
erf
(Above No. 6 coal)
233 Bk.sl. 1
201 • 8' 3
161 2" 3
37 5' 5
21 l'-lO" 5
T. 7 N., R. 9 W«
erf Cm
i> <m v^
!h O
O I- 1
+3 PU erf
M O O
•H -p O
Cm O tD
O -P
0 13 0
hO O m
M &
Crf
Horizon of top o
f No. 6 coal from which measurements are made.
No. 5 coal
No. '2 coal
Medora coal
Seahorne Is.
(Below No. 6 coal)
139
10''
erf c^
S> Cm w<
U O
O rH
-P Cm Crf
m O O
•H +3 O
CD O
bO-P
crf
U t>
© O
fD
O
No data
CO
CO
-o
M
id
o
•H T3
j3 ©
P r©
5
CO
-P
a
•H
O
-p
erf
O
Page 11.
Table
1.
- (Cont
inued)
T. 8'N.,
R.
Vft."
. . ..; i '
T.
8 N., R.
7 W.
-
* ■ t • x v v.
■s •
i
......... —
A "~N
f
••
rH P
': w •
w
rH •
i .V ^^*
w
1
Crf l <H
rH P
W
• CO ,
oJ - P
■ rH •
w
w
>lH^
a r*n
P.
■ p -
r> <^ <H
i <ri :P
CD
P
?H O ■-
CD rH
(-. o
1
ift '
iu o v-'
•H
+3 ftt-cS
CO ,rH
o
o
+> ft«J
i O rH
CD
O
5 o?i o i
P ft cci
•H Tj
. ,ft
a o o
P P. ej
•H TD
Pu
... 1 ■,
•H P , O
£ O :0
■ -H P O
P ,0
. 1 s
•H p O
£ O O
: -h p o
45 CD
P 4D
g
<H O (O
<H O CO
,
3
op-
p O : CO
' a <h
p
O P
. CD O CO
O <H
p
.
MP
W) o
.Cj', :
.
1 W P
hO O
0$
CD rd' o
cd •
■ <3
T3;. ,
CD Td 0
d
a
•n
MOg
5 O'fe
rH
hjO CD ,2;
!• fc, TJ O
u
a 4> .
0>
* .■
CJ rO
• CD O £3
CD
•
,
ri
P rQ'
i>
o :
3
fe ~'J
!>
o
Bed
pe;
•5
■3
•s .
«
<
e^
(Above
No. 6
coal)
Shoal Creek Is.
303-335 "
! 329
11'
12
300-308
i 3p4
.,.•9' : '■
,2
Macoupin coal
242-272
253
:-5"
m
227w249;
! 236,.
3». ,J0.
.8
Carlinville Is.
189-235
! 214
f $i
21.
201 --2 10,
205
7 ' i ; ■
■
No. 8 coal
159-183
; 169
,:5't
.10.
158-185
! 165
.3" .
Scottville Is,
82-115
95
1'
,3
81-S8,
! 84,
1'
4
Scottville coal
56-75
"■ 64
■•■3"
4
62-66
63. •
Bk,Bl..<
3.
Piasa Is.
32-63
| 47
■5'
23
35-55.
! 44
,4' w>i
14
No. 7 coal
21-47
36
l',-4*
11
2.6-42
i 33
l'5"v
.9
Horizon of top of No. ^6-. coal. from, .which measurements-jare made.
No. 5 coal
| 29-39
i Below No. .6
.33' !♦ '
coal)
' '3
.. ■•
No. 2 . coal
Medora coal
Seahorne Is.
85-112
129-138
135-148
1 96 -2,' -6"
; 133 l'-9"
■ 142 ?i»
■3
2.
3 ; -■ -.'.
j .84
*
i *
f
2»
. 1
Pago 12.
Bed
Shoal Creek Is.:
Macoupin!' coal
Carlinvillo Is.
No. 8 coal
Scottville Is.
Scottville coal
piasa Is.
No. 7 coal
>
u
CO
p
o
p
CO, CJ
o o
-P o
CO
0) T3
fafl o
227-228
198-202
152^165
76-82-
61-69-'
32-46
16-33-
Table 1. - (Continued),
T. 8 N., R. 8 W.
i „ e.
o
PI
u o"^
,y
O H
o
-P &4 d
•H
rt o o
jci
•H -P O
■p
O OtO
o
M-P
bD
a
d
W t) (5
Sh
o o S3
o
> -Q
fe
5
<l
ra
P
Pi
• H
O
I
p
si-
o
S3
■ >
u
o
p
a
-H
o
p
<^ ^
o ^-^
H
o o
p o
O T3
Pi &
s
CD
O
S3
(Above No. 6 coal)
;228
?199
.158
80
: 65
36
26
Horizon of top of No. 6 coal from vh ich measurements are made.
T. 8 N., R. 9 W.
r-\ P
a ■ °n
t> :<U - —
O • H
•+) ftd
«' o o
H .P O
o o
.UOP
CD
2 «
2
6'1
5
5
7
3"
2
'• "','
51
20
•
9"'
16
•32
'27
No. 5 coal
No. 2 coal
Medora coal
Seahorne Is.
O «H
wd o
d
o
t>
5'
5"
to
• H
O
P
T3
O
S3
<w
' "
(Below
No
. :6
coa
1)
»
80-
-95
• 87
1"'
-5M
8
92
1'
1
130-
■ 138
133
6""
6
130
■ 4«
• 1
133-
-140
5.36
9'
7
134
• 7'
1
Page 13.
Table 1. - (Continued)
T. "9 N., R. 6 W.
T. 9 N., R. 7 W.
Be 3
Shoal Creek Is.
Macoupin coal
Carlinville Is.
No. 8 coal
Scottville Is.
Scottville coal
Piasa Is.
No. 7 coal
r—l
-p
a
£<
t
o
CD
rH
-P
a,
CtJ
a
o
O
•H
-p
o
<u
o
CO
o
-p
0)
TJ
o
to
<d.
pes
PI
&
cc!
«
> "+H «.
$H O
(D rH
-P & OS
COO
•H -P O
•H
(D O
fxO-P
© ©
CD
CD ^
fcO O
(h
CD
>
13
«H
O
-p
aj'
294-312
249-263
212-228
154-177
53-68
29-58
(Above No. 6
301 8''
255 6"
221 6'
166 8"
94 5'
59
56
6'
10"
coal)
3
3
6
2
,1
5
5
CD r-t
COO
•r* -P O
Oh O
O -P
CD T3
&0 •©
yj
-p
Cm ^
o ^
H
Ph OS
o o
-P o
(D O
hO-P
to
CD
CO
CO
CO
CD
-p
3
•H
o
0
•H T3
CL,
X! CD
-P rQ
§
CD <Vi
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U0 O
Ctf
OS
T3
5h
0
•
t>
o
<
IS
181-233
205
7T
8
133-161
157
u" ;
., 5
93-115
! 108
5«
5
42-60
54
3"
.5
25-48
36
7'.
29
15-35
! 25
2'
10
HorizpA P-C top_pf ..No.* ..6 coal, from which- measurements- -are made'.
No. 5 coal
No. 2 coal
Medora coal
Seahorne Is.
(Below No. 6 coal)
.29.-34 . . 32 .Bk.s.l.-, 2-
81-105
110-128
115-147
39
91
118
129
l»-3"
2 '-5"
5»
1
10
11
16
Page 14.
Bed
Shoal Creek Is.
Macoupin coal
Carlinville Is.
Wo. 8 coal
Scottv'ille Is.
Scottvllle coal
Piasa Is.
No. 7 coal
Table 1. - (Continued)
T. 9 N., R. 8 W.
CO r,
u o
w
w
CD
£ ■
CD r-H
« o
>J
-p ft cd
. CD t— 1
o
rt o o
4J ft Crf
■H TS
•H -P ©
£ o o
^ CD
: -H -p o
-P ^Q
On ,0 U3
O -P
' (D O (D
CD <+h
•
' hD -P
hO O
(D Ij O
■ cd
cc!
tO CD S
t u •n o
U
fl .Q
: CD CD S
CD
cd
i > ^
i>
pci
;<t;
<!
-.-,•■
.
48-66'
28-38
14-24
ti
o
ft
g
-p
cd
T5
o
(Above No. 6 coal)
159
3"
56
5"
5
32
4'
11
16
l'-3"...
.......3
T. 9 N., R., 9 W,
CO C_i-
Sh o
CD i—l
-P ft CCS
a o o
• H -P . O
Oh O
O -P
CD Tf
hO CD
cd
CD
£ f ^
> Cn ...
M O
CD rH
-p ft cd
fl O O
-H -P O
CD O
hO-P
CD CD
CO
to
CO
G
Ej
M
o
•H XJ
,£ CD
-P P
CD Cm
hO O
cd
Sn
CD
5
30
Horizon of top of No. 6 coal from which... measurements., are. made..
co
■B
•H
O
ft
-P
cd
t3
O
No. 5 coal
No. 2 Coal
Me dor a coal
Seahorne Is.
(Below No, 6 coal)
•107
2» .,;,
104-110
'107
2 '
•
157-160
:159
10'
••- * "" ""
Table 1. - (Continued)
Page 15.
T. 10 N., 3. 6 W.
T. 10 N.„ R. 7
Bed
H 4^
d .. ■<-<
> <Vh w
S-. o
a) i-i
-p a, d
C o o
■H -p O
H -P
d Oh
L, O
ft
O O
o
•H -p O
-o
CD T3
d
o o
■W) -P
a
to
"d
w
CO
o
Cj
o
-P £>
© sn
O0 C
d
ft
>
w
-P
-P
d
-7H . _p
P <Ui
^ o
O H
-P ft d
Coo
•H -P O
tn O
rH
ft cJ
O O
-p o
<«H O
O -P
© -o
E»fl O
to
o o
W-P
d
O O
5-°
to
w
•")
a
o
•H t3
xi o
-p ,£>
O Hh
fcfl O
d
o
>
<
to
-p
C
■ H
C
ft
g
-P
d
o
(Above
No. 6
coal)
hoal Creek Is.
266-288
279
10'
13
263-288
271
4«
A
acoupin coal
225-241
231
2"
13
234-241
238
5"
2
arlinville Is.
189-220
199
6"
20
196-212
203
5'
9
o. 8 coal
151-180
160
8"
14
160-166
162 -
3"
4
cottville Is.
82-110
90
3'
12
80-110
91
2'
10
cottville coal
40-71
56
6"
13
48-68
59
2'
10
iasa Is,
27-47
37
5'
18
25-47
33
6'
17
o. 7 coal
21-32
26
.l'-5"
U 1
1
15-34
27
10"
8
orizon of top of No. 6 coal from which measurements are made.
b. 5 coal
20-40
i Below
30
No c 6 coal)
BkLsl. t
0t 2 coal
91-103
96
3! -6." 3
edora coal
135-146
138
l'-5" 3
eahorne Is.
142-157
147
6' 2
83-102
114-127
120-140
94.
118
131
l'-9"
Page 16.
Table 1. - (Continued)
Bed
Shoal Creek Is.
Macoupin coal
Carlinyille Is.
No. 8 . coal
Scottville Is.
Scottville coal
Piasa-'l"sV
No . 7 coal
T., 10 N., R. 8 W.
^ o- —
O rH
£ o o
•r-T-P o
<M
o
O CO
-p
O t3
ho 0
a
si ^
> ■-H —
S-. o
O rH
-P P* cS
a o o
• H P O
0 O CD
bO-P
0 O . S
w
w
o
o
•rH
-P ,0
0- =H
h0 O
d
u
O. .
>
<
w
a
-p
>
fi
u
•H
o
O
p>
a
£
•H
e .
3
4H
p
o
<sS
t3
0
(Above No. 6 coal)
51
32
T. 10 N., R. 9 W.
Cm
O
o
p
p>
CM
^-^
> <+-< ^t
i— 1
^ o
oS
Q) rH
o
pad
o
a o o
•H -P o
CD
0) O CD
•
ko-p
o
<rf
s
i» -d o
C> © S
.... .. .. -
<
Horizon of top of No. 6 coal from which measurements are made,
No. 5 coal
No. 2 coal
Medora coal
Seaborne Is."
Below No. ' 6 coal)
' 13-6 '
6, ....
O
^ T3
p> o
0
KO Ch
erf o
M
0
Pago 17.
Tabic 1. - (Continued)
. (Above
No. 6
coal)
Shoal Creek Is.
233-265
249
8*
4
Macoupin coal
201-226
213
0»-6"
2
Carlinville Is.
173-200
185
4'
7
179-192
187
4.i.
6
No. 8 coal
132-167
154
l'-O"
7
138-153
149
8"
7
Scottville Is.
82-88
85
l'-4"
2
85-92
89
4'
. 9
Scottville coal
39-64
53
0'-4"
6
41-55
49
9"
9
Piasa Is.
26-55
31
5'
8
26-32
29
3'
8
No. 7 coal
10-30
22
l'-2"
8
Horizon of top of No. 6 ^ coal from which measurements : are' made.
•Ncr. 5 coal ■-
25-37
(Below
- 31
No • 6
0-' -6U
coal
I
No. 2 coal
Mcdora coal
90
135
2 i -O"
2 ' -0"
1
1
91
3k. si
1
Scahorne Is.
143
7' . :
1
143
3'
1
Page 18.
-p
Cm
>
CM
u
o
(!)
r-\
-P
ft
a
£
o
o
■H
-p
o
Bed
o-
CD
CD TJ
hfl O
d
(A.
Shoal Creek Is.
Macoupin coal
Carlinyille Is.
186-194
No. 8 coal
157-158
Scottville Is.
93-100
Scottville coal
61-67
Piasa Is.
32-36
Mo. 7 coal ■••--■
Table 1. - (Continued)
.T. 11 N., R.
W.
r-i -p
& Cm
|> Cm v_.
U O
CD i— 1
-p ft a
P! o o
•H -P ©
W
w
§
o
•H
-P X
© o
hD-P
d
<£>
o
CO
•H
O
ft
-P
d
o
(Above No. 6 coal)
187
158
97
64
34
19
2'
4"
5'
5"
3'
7"
!> =M ^
^ o v-'
© r-\
-P ft d
£ o o
•H --P O
Cm O
O -P
o XJ
to ©
c5
cn
2
2
3
■3
2
Horizon of top of • No. 6- coal from which measurements are made
(Below
No. 5 coal
25
No. 2 coal
82
Mcdora coal
118-125
121
Scahorne Is.
120-131
. 124
No • 6. coal)
Bk.sl. 1
l'-6" 1
l'-4" 2
8' 3
,->!! N.,' K. 9 W.
>
©
-P
•H
•P
Cm <"•
O "— '
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ft d
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-P o
o o
feO -P
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CD
w
w
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a
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r"
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t>.
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Page 19..
Tabic 1. - (Continued)
T.
12
N . , R •
6
W»
T
. 12 H., R
. 7
W.
.....*•> ..
*•
•
/•""N
■i
* — s
'-~^
rH
-p
n
•
w
rH
*
•v •
W
ci
cm
rH
-P
w
w
d
-p
r-l -P
w
CO
>
q-i *- ' "
d
Cm
o
-P
■ t>
Cm «m
d ^
o
-p
$-.
o
>
«M >-"
a
ti
J-.
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M
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m
•H
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M
•H
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: O
rH
o
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o
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13
o o
-P
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T3
ft
a
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PS
o o
^
O
■H
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M O O
^
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-p o
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£>
6
•H -P O
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&
g
<*H
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3
Cm
o co
3
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■o
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O
Cm
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©
Cm
-p
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IhO -P
t»n
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d
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to -P
Wj
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©
tJ o
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•
d
Tj
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T3 O
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T3
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>H
- uo
o ^
S-, T3 O
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ti
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Bed
«
<
-«J
f^i
ot
<
S25
(Above No, 6
coal)
Shoal Creek Is.
248-270
258
9»
4
Macoupin coal
224-248
: 233
0'-2"
4
Carlinville Is.
166-205
181
5'
3
No. 8 coal
136-168
158
Qt-10"
11
"
Scottville Is.
77-94
84
2'-6n
9
81
6 ''-6"'
• 1
Scottville coal'
32-49
40
0'-5"
4'
3iasa Is.- :
30-36'
: 32
5''
11
. 40
3 »-6"
1
Vo. 7 coal
24-29'
27
l'-2Tt
3
horizon of top of No. 6 coal from which measurements arc made,
Mo» 5 coal
Bfo. 2 coal
\fedora coal
Seahorne Is.
'Below No. 6' coal)
21 Bk.sl. ■ 1
94
Bk.sl.
1
136;
Bk.sl.'
1
148
2'
1
95 Trace.
132 13'
Page 20.
Table 1. - (Concluded)
T.
12 N., R
. & w. -
T.
12 N., R.
9 W.
_
•
."— «*
•*
' "N
- — s
rH
-P
^ •
w
rH
•
* • W
d
Cm
■-1 ^
w
M
Ci
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rH "P W
w
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Ti
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■P ftd
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ft
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T3
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fl O O
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3
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p
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o
Bed
rt
<! '
n
S
pel
«i <$
(Above No.. 6 coal)
Shoal Creek Is.
Macoupin coal
Carlinville Is.
No. 8 coal.
160
l'-OO"
1
Scottville Is.
88-91
89
6'
2
88-96
92
4'
2
Scottville coal
53
3 '-00"
1
60-63-
62
0'-10M
2
Piasa Is.
33-39
36
S».
2
24-38 .
31
3'
3
No. 7 coal
Horizon of top of No. 6 coal from which measurements are made
Nc. 5 coal
No. 2 coal
Mcdora coal
Seahorne Is.
(Below No. 6 coal)
86 1J-00" 1
130 4 '-00" 1
136 7' 1
Pa~e 21.
Table 2. - Compilation of intervals between top of
Herrin (No. 6) coal and tops of Scott-
ville limes tone,, Trivoli (No... 8), coal,
and Carlinv.ille limestone in Macoupin County.
(To accompany fig. 2)
Location Interval from top of No. 6 coal to top of
County Scottville Trivoli Carlinville
Twp. Rge . Sec. number limestone (No. 8) coal limestone
212
162 20i|
165 20S
. 20$
152 19U
I65 208
• 209
162 205
200
168 210
205
•215?
216
82 167 • 209
173
20^?
168
175 . 21k
7N
6w
1HS
7N
6w
ih6
7N
6v;
5H7
7N
6w
6e5
7N'
6w
11D5
7N
6w
llp5
7N
6w
17D6
7N
6w
26c6
7N
6w
35D5
1lG8
8a8
7N
7W
7N
7W
7N
7W
9El^
7N ■
T&
10D^
lODLi.
7N
7W
7N
7?;
10E2
7N
7W
10E3
7N
7V7
10E3
7N
7W
10E^
ioe)+
7N
7\7
7N
7w
10H2
7N
7W
12E7
7N
7W
Ikkb
7N
fit
1SF5
7N
71/7
18E7
7N
7W
23H3
7N
7W
27G5
27H4
7N
7W
7N
8w
12F1
7N
8w
2iiG8
36D1
7N
8vj
8n
8n
6v;
6w
Sfi
8n
6w
8G1
8n
6w
9g8
8n
6v/
iicI^
8n
6w
12Eli
8n
6w
l^Alj.
Qk
90
93
86
78
83
6 88
(Continued on page 22)
168 210
209'
160 202
168 205
156 . 198
159 200
22l|.
215
213
235
224
I83 223
Table 2. - (Continued)
Location Interval from top of No. 6 coal to top _ _of
C oiint y
wp .
Rge.
Sec .
numb er
8n
6w
l8A2
158
8n
6w
18c 6
288
8n
6w-
19G6"
13-9
8n
6vj
20A6
289
8n
6w
25A2.;
322
8n
6W
25K3 .
llj.0
Sn
6\7
28D5
lip.
8n
6v;
29D7
Ik2
8n
8n
6w
6vj
29G14.
30A1
:/:$
8n
6v/
30116
lk5
8n
6vj
31A8
11+7
8n
6w
31H8
1JU.6
8n
6w
3^8
1I4B
8n
3n
6w
6v;
35G3
36AI
32t
3n
7V7
[|A3
152
8n
77/
UF7
151
8n
7W
10F5
153
154
6n
7\7
11H7
8n
7/w
13A1
315
8n
717
13EU
156
3n .
7V7
13 Fll-
155
8n
7v/
IS A3
x52
8n
TV/
18A8
158
8n
717
23A2
290
8n
7W
25 Gl
159
8n
7W
2SG2
163
8n
717
29Ali
160
8n
7VI
32DS
3km.
161
8n
8w
162
8n
ll\F2
168
8n
8u
15A5
lj.55
8n
8w
15B7
323
KYI
8n
8v;
22H1+
8n
8V7
23E1
169
8n
8u
2SA1
170
8n
87
36AI
172
8n
8v/
36b6
173
9N
.6yj
18F1
125
9N
6w
21H1
127
128
9N
6vi
50D1
9N
6\7
31A1
129
9N
6v;
32G1
130
9N
6vj
33A2
131
Scottville Trivoli Carlinville
limestone (No. 8) coal limestone
115?
. 215
210
205
■ 166 . • ,215-
. 17.2 217
210
215
168 207
167 213
169 213
173 219
168 211
82 169 210
159 189
159 201
160 202
88 185 208
161 202
160
207
210
162 • 20lj.
80? 158
203
. 201
20 6
167 • 201;
203
85 172 . 208
202
80 152
82 165
81 161 199
158 198
75? 15k 199
80 is8 198
112 233
15I4- 218
21k
98 212
227
91+ 22S
(Continued on page 23)
Page 23
■ Table
2 . - ( Continued.)
... L.OCE
it ion;.
Interval. £r<
Dm top of ..No. 6
coal to top of
County
Scottville
Trivoli
Carlirville
Twp.
Rge.
Sec .
. number
limestone
(No. 8) coal
limestone
9N
fiw
33H2
150
177
22k
9N
7V7
7D1
1|63
93?
9N
T>
10C1
296
161
9N
7W
10F1
112
200
9N
7W
10P5
111
xi5
195
9N
717
17A3
116.
81
9N •
7V7
21E7
275
280
• 135?
9N
7"
21F8
9N
711
22DS
122
II4.8
181
§N
7v;
23A8
123
111
195
9N
7W
23A8
283
12k
107
197?
9N "■'
717
28llk
29 b8
210
9N
7W
21k
208
9N
7v;
3kn8
" 11
9N
8Y7
33GS
31^8
159
9N
8w
US
157
193
ION
6v;
2CS
6H3
190
ION
6v;
te
87
l6l
192
ION
617
w
86
ION
6v;
8H5
K(
82
157?
199
ION
6u
9E7
k8
155
195
19k
ION
6v/
9H1
U-9
86
161
ION
6v;
10H1
. 50
l6l
192
ION
6\7
llAk
51
152
189
ION
6v;
11G5
,?2
160
19k
ION
6x1
12B7
kk5
192
ION
6w
ikok
£
86
20s
20k
ION
6\7
15EL
16E6
162
ION
6v;
55
85
157
200
ION
ION
6w
6ti
17C5
20AJ+
61
88
93
I6I4.
199
204
ION
6v;
21 Ei+
58
151
190
ION
6w
22Gk
59
161;
201;
ION
6V7
23H5
60
83?
160
199
ION
6u
30D1
62
98
212
ION
6V7
32A1
"■ %
102
2lk
ION
6y/
33Ai^
110
180
220
ION
7V7
65
102
ION
7W
12E5
68
86
162
205
ION
?7
13D7
69
196
ION
7W
I7HI4.
■ 70
85
ION
7W
20C5
332
85
ION
7.7
20C6
•' 33I4-
87
ION
7\7
20C6
336
80
(Continued, on page
2k)
Page
Table 2. - (Continued)
Location
Interval from
top of No. 6
coal to top of
County
Scottville
Trivoli
Carlinville
Twp.
Rge.
Sec .
number
line stone
(No. 8) coal
limestone
ION
ty/
2kD2
72
• 201
ION
717
2[^GL
2SF6
7il
• 93
116
203
ION
tyj
210
ION
717
28F7
, ,5
160
ION
T.i
301-11
IU1-6
110
ION
7W
3^B7
^
200
ION
?:i
35F7
• 78
85
. 200?
ION
7TI
3508
79
161
203
ION
E
36EI
81
97
• 212
UN
LlE2
??
':15k
175
UN ,
6v;
537
?f|Jj
167
UN '
6YJ
20A8
36
132
186?
UN
: 6w
25B1
38
158
180
UN
6\v
29E5
P
153
UN
6yj
30A1
88
UN
6vj
33E3
3to
^
82
157
I83
UN
6\7
: fi-3
159
185
UN
6w
35A^
U2
. 200
UN
6Y7
36b1j.
iA
190
UN
7\v
7E1
502
8J
UN
TV/
10G7
22
85
ikk
• 179
UN
7V7
114A6
I
2°
150
11 N
7W
ise8
k
132
186
UN
7VJ
i6e6
25
88
151
190
UN
7W
18H3
57
91
UN
7W
19E5
26
86?
UN
7"
20E3
27
92
153
192
UN
7W
21B1
28
87
15J
192
UN
7.7
23 A7
29
86
138
I83
UN
UN
£
29 d8
tEk
31
19
83
99
^l
13k
UN
8\7
9Fk
15H6
20
100
158
180
UN
8w
3k2
93?
12N
6\7
2Dk
2D6
1
145
12N
6v;
2
' "88
12N
6v/
8A7
2M
175?
12N
6w
i8ei
&
175?
12N
6\7
30A3
88
153
12N
6y;
30111
7
&
161
171?
12N
6y;
30117
5
8?
168
12N
6v;
31B5
6
82
153
205
12N
6w
31F2
10
80
12N
6w
31F3
9
F
158?
12N
6\7
31H1
11
80
158
(Continued on page 25)
Page 25
Table 2. - (Concluded)
Location Interval from top of No . 6 coal to top of
County Scottvllle Trivoli Carlinvllle
Twp. Rge . Sec. ■ number limestone (No. 8) coal limestone
83 I5I4-
8l
91 160
88
12N
6w
32E1
12
12N
7V7
17E1
305
12N
8w
15B7
15
12N
97;
, 3
Outcrop
12N
9V7
,1+to 10
Outcrop
1
H
1
-^-1041
443 .• x
/ \
T.
14
N.
IA
' 487
312'
scott}"'
" " G R~E
352
+
1512
....■•"' 952^
M_0
ENE
■ ■
RGAN
1
i
• -T I860 ^\
1030 965 \ ,
V^ f
.754 f SANG
AMON
13
MACO
UPIN
578
-6-
T505
1 l2
4
1586
1
1
1
i ^
1828
+
1487
+
328 633
,11
[
1 10
,9
8
T
|7
1 N
RY
745
1076
l +
724
496
CARLINVILLE>
NOR TH T
/ 580
485 S 50
535"^
695 ^'j
f -JjERS
1187 J
r-.
1
• 1540
4
37V
+ ^5.
500 A- 1
612^ -$-
^1635
1380^448 1 A
jJfeL -O- 1613
'*r*p''N^578
b0^L^i^CARLI
..,;#T" 507
SPANISH NEEDL
NVILLE
-A. 617
£" T 382
755
-*-•■■
1542
1605
"shipman"
-fife
560 ^
1 93C
>
5 440 p/,/1/
' .'' "f
,' 550
CREEK
^.UNNAMED
T^320
ty UNNAMED
NVi£w2 ^r\
625T "7
546
2563o9
^GILLESPIE
WYEN
575
- -^fjUNNAMED
1 jjfer— ^ 1000,
1 3^ T>-
2235 ,
■4- "^
4(
L
S
' /
1 /
/
/
1
H
1
1
STAUNTON
2307
67,^
GILLESPIE- „
BENLD
-852
R.IIW. '
^ 0
• 0
10
IL OR CAS POO
AS WELL
IL WELL
RY HOLE
RY HOLE WITH
9 8 7
LEGEND
-$- DRY HOLE WITH SHOW O
■^t DRY HOLE WITH SHOWS
1586 TOTAL DEPTH
, CHESTER -IOWA SUBSURF/
HOW OF GAS DEVONIAN- SILURIAN SUB
SCALE
0 2 4 6 8 10 12 MILES
i i ■ i 1 i — i
R.6W.
F OIL
OF GAS AND OIL
kCE BOUNDARY
SURFACE BOUNDA
FIG. 3 - INDEX MAP SHOWING OIL AND GAS
DEVELOPMENT IN THE AREA
Page 27
OIL AND GAS POSSIBILITIES' ,
By
WILLIAM H.'/EASTON, ■■ -
' •• Introduction .' . ■ -
This summary of oil and gas development and possibilities
is based on the structural, features . of coal No.' 6. Prospecting
Is recommended. in several, areas but is discouraged in other areas
in which proof of closure is lacking .... There may be small amounts
Df oil or gas along anticlines that have small unrevealed closure,
but the amounts are. not likely to be commercial.
Most of the drilling has been in the form of coal'tests ■
many of which entered the lower Pennsylvanian sandstones. There ;'
are no records of some of the coal tests or of more numerous oil
ana^gas tests that were drilled years ago. Moreover,, it is not
possible to check up on production of all wells or pools. In the
following report, the records of wells are used as •reported to the
Geological Survey.; some records of shows of ■ oil and gas are prob-
ably omittea and some reports of shows , may be inaccurate, but in '■'
any case, the available information is reviewed herein for the
benefit of the .Industry. "... ... ,. ' .
Possible Producing Formations
Possible producing formations in the region are ten in
number, namely: (1) Pennsylvanian sandstpnes ,■ (2) Chester sand-
stones, (3) McClosky limestone-," tt) StvLbUls' limestone , (5) Salem
stonf °?ft? i:6) tolinSton-^okuk limestones, (7) Devonian lime- '
stone, (b). Niagaran dolomites,, (9) "Trenton" limestone, and (10)
rdovician sandstones and dolomites below the; "Trenton'!.',
Only the Pennsylvanian system has been extensively or
u«n?f Si Y ^JPected in ^e area. Production from .the ^Pennsyl-
vanian has come from sandstone strata in the lower part of the
system. xhese strata have been formerly referred to a,s Pottsville
TniZ\y7temrm ^ reWQS^^ever^lo^^'^^P^of:Mie Pennsyl-
,ni,HloD lhe fester sandstones', which : produce' ;oil;. in central and
°r*T^ern Illlnois* ATS restricted chiefly to. the southeast cor-
of the area where they are thin.,, They are aLso probably
Page 28 »
o
represented by thin deposits left as residual outliers by pre-
Pennsylvanian erosion. Because Chester strata are thin, Irregu-
larly distributed, and close to the surface, they are thought not
likely to produce oil or gas in the area.
The I.IcClosky limestone, which is very productive in the
Illinois basin, is a possible producing formation in part of this
area, especially in the southeast portion where it has a greater
cover of sediments. No shows of oil or gas have been reported to
date in the I.IcClosky In this area. Outside the area of Chester
sediments, it is likely to be absent, owing to pre-Pennsylvanian
erosion.
One well (Macoupin County well No. J4.62) had a show of gas
in the St. Louis limestone. The Salem limestone is the producing
formation in the Jacksonville gas field In Morgan County. Shows
are reported from the Bur ling ton -Keokuk limestones in one well.
The Devonian limestone is absent in the northwest part of
the area. It produces in the Sorento pool In northwestern Bond
County. The IJIagaran limestones and dolomites are overlain, directly
by Pennsylvanian strata in the northwest part of the area. Shows of
gas have been reported from the "Niagaran" in the area, and it is
the producing formation in the Pittsfield gas field in Pike County.
,The "Trenton" limestone is the oldest producing formation
in Illinois. The discovery of very good "Trenton" production near
St. Jacob in southeastern Madison County in , July 194-2 makes the.
prospects of other areas in western Illinois look more favorable.
It should be noted, however, that "Trenton" structural "highs" may
not extend Into younger beds because such "highs" may have been
formed before the younger beds were deposited. Shows of oil were
reported in Lower Ordovician beds in one well (Jersey County well
No, 5) . .;• :
Structural Features
The names of the' geological structures (pi. 'I4.) used in
this report arc listed below, with a note as to whether the name
is old or new.
1. Staunton dome: (old)
2. Anderson anticline (new)
3. Burton anticline (new)
5A. Carlinville North dome (new)
L|_. Carlinville anticline (old)
i|A . Carlinville dome (old)
. > 5 • Grimes anticline (new)
6. Hickory Grove anticline (new) '
6A. Macoupin dome (old)
6B. Spanish Needle Creek dome (old)
7. Lowder anticline (new)
Pace 29.
8. Modesto anticline (new)
9. Nilwood anticline (new)
10. PTainview syncline (new)
11. Shipnan anticline "(nev;)
12. South Litchfield dome (old)
13. Thayer dome (new) •..„•.. :
llj.. Waver ly anticline (nev/)
15. Weyen anticlinal nose (nev;)
The discussion of oil possibilities in.T. 7 S., Rs . 6, 7?
8, and 9 V/., is given in Circular 71,'pp. 9 and- 12, and is quoted
below. The present. map omits the small closing contour formerly
shown in sec. ll+, T. 7 N.,.R. 8 V7.; other slight shifting of con-
tours is too minor to warrant discussion.
"(1) Staunton dome , sec. llj. and adjacent sees.,
T. 7 N., R. 7 W.,. Macoupin County.
"The Staun ton dome is "described in: Bulletin 28,
p. [p.; Mining Investigations Bulletin 11, p. 37 > an(^ Bulle-
tin i|i|A . • A gas field which produced for three years from
1916-1919 was located on this dome. Production was from
Pennsylvanian sandstone, and the average depth .to top of pay
in l8 gas wells was i^6l feet. Average thickness of pay was
30 feet. The deepest -well J on the structure, drilled in -lQJl,
had a depth of 2571 feet and tested the 'Trenton'- limes torie.
"The fact that mine levels were "used in the -::--::-:h:-
structural interpretation insures a greater degree of accuracy
than was possible in previous maps.
"The dry hole to the 'Trenton' has undoubtedly dis-
couraged further test -drilling for oil -or gas on the Staunton
dome ."
2. Anderson anticline. - The Anderson anticline, named
from Anderson School in the SE corner sec. 2, T. 10 N., R. 7 Y/.,
is a mild warping at Modesto and terminates about three miles
south of South Standard. . It has not been tested to the lower
Pennsylvanian, although- several coal tests have been drilled on It.
Drilling is not- recommended- because the structure has no closure.
3. Burton- anticline.. - The Burton anticline, named
from the Burton School in the NW l/lj. sec. 3]+, T .. 10. N., R. 7 W.,'
is terminated at the west by the Carlinville, North dome and extends
eastward about five miles in an arc between the Anderson anticline
and the Carlinville anticline.
Two.'V/eils In sec. 35.ha<! gas shows , -one . (Macoupin
County No. 77) had gas in shale and sand at 395-^05 feet, and the
other (Macoupin County No. 78) had a shov; in shale, .from lj.07-i;13
feet. The well in sec.- 2I4. (Macoupin County No. 72) had a possible
Page 30. .
show of gas below ^hjj feet and a very slight show of oil at 550
feet (total depth). YJithout known closure, further drilling along
this anticline does not seem advisable.
3A. Carlinville North dome . - ' The Carlinville North dome,
named for the Carlinville North pool, lies one mile northwest of
Carlinville, occurring at and near the common corner of sees. 17,
18, 19, and 20, T. 10 N., R. 7 W.
Production has been obtained from the east flank of
the dome in sees. 17 and 20. Oil, with which some gas occurs, is
obtained from the lower Pcnnsylvanian at about 500 feet. The well
in sec. 17 (Macoupin County No. 71) was drilled in 1913* and at
least 'one well was' drilled in 1921. The recent drilling began late'
in 19^4-1? and there were three producing and eight abandoned oil'
wells in July 19U-2 • This pool was 'formerly 'included with. the. Car-
linville pool, according to Blatchley (Bull. 23, p. 11), who
reported one well to have made 10Q barrels daily. .
I4.. Carlinville anticline'. - The' "Carlinville anticline
extends from northwest of Chesterfield eastward to southeast of
Carlinville, then .swings north to about .four miles south of .South
Standard. In sees. 11', ll;, 10, and .15, T. 9 N.,K. 7 ',7 . , is a
fairly sharp nose without known reversal of dip. A coal test
(Macoupin County No. 296) did not reach the lower Pcnnsylvanian,
The broad "high at the east end of the Carlinville anticline in
and about sees. 32 -and 33* ^ . 10 IK, R. 6 II., sees. I4. and j?,
T. 9 *N»> R« 6 v7.,i has hot been tested by any well reaching the lower
Pennsylvanian. Doming or reversals of dip are not known but may
occur. This is a possible producing area, but not . enough data are
available to suggest a location. . . •
i|A. Carlinville dome . - The Carlinville structure was
first mentioned as an anticline in 1910 by Blatchley (Bull. l6,
p. l6i) who' discussed the finding of gas in the Carlinville field.
Kay reviewed the Carlinville field in 1911 and presented a partial
structure nap (Bull. 20, pi. VIII). The Carlinville field v/as
mentioned by Lee (U.S.G.S. Gillespie-Mt . Olive folio) as being on
a dome, here designated the Carlinville dome. It' has ' long been
known' to have about 20 feet' of closure.
The most comprehensive discussion of the Carlinville
pool to date is in Bulletin 31* PP» 91-99° Drift gas, discovered
in the "early sixties," led to the discovery of gas in the lower
Pennsylvanian strata in 1909 and oil in the- lower Pennsylvanian in
1911. The gas had an initial pressure of 135 pounds; the oil had
a specific gravity of* 28.69b. Although the pool was abandoned in
1925 ? it is now producing again from three wells and a fourth well
is being cleaned out.
5° C-r ime s anticline . - The Grimes anticline, named from
Grimes School in the IIV7 corner sec. 11, T. 8 N., R. 7 W?> extends
ixi an arc from Shipman to just north of Gillespie. Although gas was
obtained at Shipman in( 1907* "V* was n°t until January of 19^4-2 that
further drilling v/as done. The first well of the three (as of
;
Page 31.
July 191+2) in sec. l8, T. 8 N., R. 8 Y/., made 1 l/2 million cubic
reet per day from the lower Pennsylvanian, -. the top of which ^lies
it 365 feet below the surface. •, . *
Lee mentioned a possible dome (Bull. $1, p. 105) in
she N l/2 sec. TO,- TV 8 N-. , R. '8 -V/., but the' structure is not indi-," .
jated by the- present* map'.'. He. also . suggested that a slight. upward
mrping may exist somewhere near the comer of sees, 3 and- if,
I 8 N.., R. ? W.-,- and '33. and 3k, % .- ,9 N.,-..R. 7 W3 (Bull. 31, p. 105) '
Dut.it is not supoorted by this mao.. . ■• <- ' '."."
- -■" > '■ ' ' ' ' ."."',..' ■ ■' : .• . ..' '■ ' '■ ■'■ ' .. '
' The Holmes - Watk ins well . in sec:. ■ 2^ , T. 8 N.,R/ 9WV, ,
lad two shows- of oil from I+3.O-I4.33 feet and::'45°-455- -feet- in the; :
jower Mississip'pian-, topped ' at l\l 8 feet . . The.YJ. R. Holmes and
Jraham - Kulenkamp 'No. 1, Ml/4. SE l/k SW lA -sec* -7, -T . '8 N.,'
m 8 W., made 150,000 cubic feet of gas from the lower Pennsylvanian,
vhich was topped at 31^4- feet, -,-■. :„v.'\... ., ...- '■ . V
.'Without1 indication, of closure,, further drilling is not .
warranted in this region. • ' . -': -.■;■.'
6. Hickory Grove anticline. •- The general anticline" on
/hich the : Spanish Needle Creek and the Macoupin domes lie is called ... •
:he Hickory Grove anticline, "named from Hickory Grove School in "
;he center E l/2 sec. 28, T. 9 N., R. 6 W. It extends east-south-
jastward from the common corner of Green© »: Jersey, and Macoupin
counties at. least to the cent.er.-of the .east, edge of T. -9 N.,.R. 6 W. •
?he west end is more Tike an" Anticlinal nose,: but there . is a ■
sharpening of the structure' in see's . .21, ■ 26, and «27> "T. -9- N., R, 8 ¥.,-
/hich has- been partially, test.ed; .'. this, is. discussed, below under, the.
lame Macoupin' dome . ■',■•., ( -
Eastward from the Spanish Needle- Creek dome : the
[ickory Grove anticline 'becomes broader. The well in the SY/'cor-'
ler of sec. 23, T. 9 N., R. 7 W. (Macoupin County No. 1J+8) had a
small show of gas at I4.7I4. feet -(lower. _ Pennsylvanian?) and gas shows .
it 508 feet (lower Pennsylvanian) and 6I4J4- feet (Lower Mississip.p'ian
.imestone, .top 628 feet). Of the two .■wells - in sec.; 33 , T«. 9 N-r
I, 6 Y/«, one (Macoupin County ./No.. 131) 'had a sTight show of oil .
"rom 115.-127 'Tee t (lower Pennsylvanian); the other (Macoupin County
Jo. 150) had a good show of gas at 596-o05 feet, a show of oil at
)05-6lO feet, and shows of gas . and oil at 6l-0-£l5J...f ee.t.,..-all in. -the
.ov/er Pennsylvanian. «. It ■ is- possible ■ that-, a well drilled, up-d'ip:
.n the E l/2 .sec. 29, or ■ in the til l/2 sec .. :28^. T. -9' N. ,;. R. 6 .17.,
/ould be more favorably located for obtaining .commercial production
)f gas and oil. A reasonable location for .a test well is in the
•-enter of the NW l/l\. sec. 28,' T. 9,'.'N'., R.. 6-.V/. . The lower Pennsyl-
vanian, which Includes the most favorable possible producing
lorizon, lies at about 580 feet.... , ... . ■ '_ ...
6A . Macoupin dome. - The Macoupin, dome has been des-
cribed (Bull. 31, p. 101+) . 'It lies mainly in sees. 26 and 27,
'. 9 N,, R. 8 V/., and is elongated east-west. The area including
;his dome was mentioned in the Gillespie -lit , Olive folio, ; p. 9> as
)robably a. region of . warped strata. ..The Impromptu - : Rinak'er and
Page 32.
Benson well in sec. 27 O'lacoupi'n County No. 87). had a. show of gas
at from [[Z^-liJiO feet In the lower Pennsylvanian. The Ohio -
Mutzbauer well No. 1 (Macoupin County No.. 8I4.) in see-, 23 had. a light
showing, of oil at. 3.il3V£ee*t; and a gas show at 322 feet, both in the.
Pennsylvanian. (This well is mentioned in 'Bull'. 31 / P-' IOJ4.*, as
being one mile northwest of the bridge in the N2f corner sec. 27,.
which would place it In sec. 22; apparently northeast was meant In-
stead of nbrthwes't) • The Macbuplh dome is not yet adequately 'tested-.
For further testing, the S l/2 NVJ l/I|_' sec, 26, T. 9 N.,'R. 8 Y/.,
would be the most reasonable location because, it would be higher than
the other well (Macoupin' County No. O7) to the west which gave, a shov/
of gas. The lower- Pennsylvanian there lies at about I4.OO feet.-'.!!.'-,
Present studies indicate .'that the' dome- has. about ten. feet 'of closure
on the Herrin (No. '$) coal. , !-.•'•"..'"
6B. Spanish Needle Creek dome. - The Spanish Needle Creek
dome as originally described (Bull. 31> P« 102), was located in the
NE I/I4. SW 1/1+ sec. 21, T. 9 N.,' R. 7 V/*, but more, recent data indi-
cate that the crest lies in the SE I/I4. NW l/k sec. 21. The dome
was mentioned in the Gillespie - Mt. Olive folio, p. 9*. A sub-
ordinate "high"- in- sec , 28 is not substantiated -by. present -data'; also
the axis of . the structure trends nearly east-west .instead! of north-
west-southeast .
Production' on the Spanish Needle ' Creek dome . was from
the lower Pennsylvanian sandstones. The deepest well (Macoupin
County No. 28l) on the dome Is the '7. E. Schmidt et al (Hercules -
Oil knd Gas) ' - Miller* No . 1, which was dry and abandoned at a total
depth of 5^4-5 feet but was still in the Pennsylvanian. The field
was discovered in 1915 (the same year its structure was pointed out
by Lee) and was abandoned in 195^4- • Ctoe well is reported to have
made 3 million, cubic feet of gas per day. ( Gillespie-Mt . Olive . .
folio, p, 13 ) . ; " • .
, « , « . ...
No deep test has been made on the dome. .There are no
Chester strata within the area of the Spanish Needle Creek dome,
hence possible, deeper production would have to come .from, rocks of
early Mississippian age or older.. Probably the dome is too small* to
justify such deep drilling.
7* ■ Lowder' anticline . - The Lowder anticline 2 named' for
the town, lies between the V/averly anticline and the Modesto anti-
cline. It" is . in line with the Thayer dome and appears to be a
branch of the Waver ly anticline. No tests have been made on the
Lowder anticline . Until evidence of doming can be substantiated,
further drilling does not appear ' advisable .
8. Modesto anticline . - The Modesto anticline, named for
the town, extends from .the northwest .corner of Macoupin County,
through Modesto and then eastward to the -northeast ' corner' of, the
county. ...
There has been only one Important well drilled -on this
anticline, and that is the 0. G, Hayes"- Alders on No. 1 (Macoupin
Page 33.
County No. 305) in sec. 17, T. 12 N., R..7 Y/. , The well ended in.
the St. Louis limestone, topped at 565 feet, but no shows of oil
or gas were reported.
There is* no -present indication of closure on" the anti-
cline, hence prospecting is not recommended.
9. Nllwood anticline .'• - The'. Nllwood anticline:, named for
the town, extends from about two miles northwest of Nllwood in an
arc to the south, to about two miles south-southeast of South
Standard. The south end of the' NilwoOd anticline is in line with
the trend of the Carlinville anticline., '
The coal test in sec. 29, T. :11 N., R. 6 VJ . , did not
test the lower Pennsylvanlan sandstones.' 'In sees. I4." and 9,
T. 10 N.,. R. 6 W., several coal tests have "been, drilled but only
one (Macoupin County No-. i|9)< tested the- lower , Pennsylvanlan sand-
stones. There were no shows reported, . and the well was' completed .'.
in the St. Louis limestone at' 695 feet.
To the east of the latter region, two wells had shows
of oil, one (Macoupin County. No. 1+1+2) in sec. 35, T. ll'N.,,
R. 6 W., and the other- O'lacoupin County No. )])\ %) in sec. 2,'.
T. 10. N., R. 6 W., which 'produced' a little oil but is temporarily
abandoned. •--•'• • ■• . • « ; -
There is no known reversal, .of . 'dip on the.-Nilwood anti-
cline, but additional data may prove the presence 'of one or more,
domes. The presence of anticlinal noses along the east margin of
the structure might be an indication of the presence of domes up-
dip. Recommendations for drilling cannot be made.:
10. Plainview syncline .' - The Plainview^ synclihe, named
for the town, extends completely across Macoupin County between
the Hickory Grove anticline and the Grimes" anticline and has an
east-west trend, ' plunging 'eastward. It has . a closed low spot in
sec. 3^, T.. 8 N., R. 9 W. '•' '
The Plainview gas field lies in sec. 35, immediately
east of the closed. low. -Production Is from- the lower "Pennsylvanlan
sandstones. One well made 1 l/2';mlllion cubic feet per day.
No closure- is known, 'hence, further drilling Is not
warranted at present.'
11. Shipman anticline. - The Shipman anticline, named.
"or the town, extends from Shipman to Mount Olive.'- At \ the west end
of the anticline in sec 25, T. 8 N;, R. 9'W.,' is located the well
(Macoupin County No. 175) which Was reported as having had a show
of gas (Bull. 16, p. 176). ^he gas was encountered at J4.18 feet in
the Lower Mississippian .
In sees.- 15 and 22, T.'S N. , R. 8 \T. , is a small gas
field which produced from the lower Pennsylvanlan. Although not
Page 3I4..
specifically named, it is sometimes called the South Plainview field.
Two wells entered the Lower Mi's'sissippian "but no deep tests were
drilled, the deepest being 550 feet.
The' Gillespie - Bcnld gas field is in sees. 29 and 30 »
T. 8 N., R. 6 VJ. Production was from the lower Pennsylvanian sand-
stones. The number of wells drilled is not known, but there were
reported to be at least three producing gas wells and one dry hole.
The production of one well (Macoupin' County No. 1J4.3 ) was reported
to be 5 million cubic feet of dry gas per day from 53^ feet (lower
Pennsylvanian) at 155 pounds pressure. The field had been partially
drilled by 1925 an<l was abandoned in 1955* The structure has been
indicated in Bulletin Jl, p'l . II, on the Gillespie quadrangle geo-
logic map,- and on page 9 in "the Gillcspie-Mt . Olive folio.
In sees. 20, 29, 32, 33, and yhr, T. 8 N., R. 6 VJ.,
there are five small domes. The one of these which Is mostly in
sec. 20, has been tested (Macoupin County. No .. 289) by '. a gas well
completed in 1931* production coming from the lower Pennsylvanian
at 565-575 feet. The field' was not named because of its small size.
The amount of gas obtained is not known.
Of the other. domes, the east one (In sees. 33 ana 34)
has had a coal test (Macoupin County No. llj.8 ) drilled on it which
did not reach the lower Pennsylvanian, having only gone to 3.6 1 "feet.
Another very small dome in sec. 23, T. 8 N., R. 7 W., has had a
nearby test (Macoupin County No. 290) which had a show 'of oil at 595
feet in the lower Pennsylvanian. These low domes may contain gas in
the lower Pennsylvanian, although it is impossible to know whether
or not the gas would be in commercial quantities. The fact that pro-
duction was obtained in the Gillespie - Bcnld gas field nearby is
somewhat encouraging. If the small domes are drilled, the most favor
able locations are the NW l/lj. SE I/I4. SE l/k SE lA sec. 23, T. 8 N.,
R. 6 W., the SE I/I+ W lA NE lA sec. 32, the center of the E l/2
sec. 32, the NE lA SW 1/4 NE I/I4. sec. 33, and' the center of the S
line sec. 32, all in T . 8 N., R. 6 W. The lower Pennsylvanian sand-
stones, which would be the most probable producing formations, lie
about 250 feet below coal No. 6, or about 660 feet deep In sees. 32
and 33*
12. South Litchfield dome . - The South Litchfield dome
was described (Bull . 3 1 > P» 1031 ^s occurring partly in sec. 25,
T. 8 N. , R. 6 W., but the west portion which should occur on this
map does not appear from the data at hand. The coal test (Macoupin
County No. ll+O) In sec. 25 went to ' \ ) 1 ) ; feet and reported no shows of
oil or gas .
13. Tha ye r dome. - The Thayer dome, named 'for the town,
occupies most of secT 2~7 parts of sees. 1 and 3* 1. 12 N., R. 6 Y7.,
and parts of sees. 3I1 and 35* T. 13 N., R.,6 VJ. It is probably an
extension of the trend of the Lowder- anticline .
The Thayer dome has not been tested, as the coal borings
on it are alJL shallow holes.' The structural conditions are similar
Par,e 55.
o
;o those in the Staunton gas field f arther .south," but' the Chester
series is absent on. the Thayer 'dome-". ' The chances of obtaining
production from the lower Pennsylvanian^seem good. The first test
veil should be drilled in the center of the SE, 1 A NY/ l/l+ sec. 2,
C 12 N., R. 6 W., in order to place it at the highest point of
:hc structure. The top of the lower Pennsylvanian is probably
ibout 200 feet below coal No4. 6, or about 5^0 feet deep*
A mile and a half west of the Thayer dome is a struc-
:ural depression which underlies the north part of Virclen.
lij.. Waver ly anticline . - The Waverly anticline, named
Tor the town, extends from Waver 1$ at least to Auburn. Near
Vaverly, in sec. 2, T. 13 N., R. 8 VI., a well ( Morgan ^ Count y_ No .16)
iad a gas show from 32I4.- 31V7 feet in the ' Pennsylvanian' and good shows
Df oil at 800 feet, and from 912-965 feet in the Keokuk -Bur ling ton.
Dther . than the ."-veil (Sangamon County No. 20) in sec. 7> T. 13 N.,
1. 7 W«, which did not report any shows,, the anticline • has not -been
:csted. A sharpening of the structure at Auburn is the next most
significant structural * feature on the ' anticline . Examples of clo-
sure are not known, hence recommendations; for drilling cannot be
nade at this time.
15. V/eyen anticlinal nose . - , The Wcyen anticlinal nose,
lamed for the old gas production on ' the Vfeycn farm,' lies chiefly .
m
sees. 8 and 9>J3> 8 N., R, 6.V/,, between the Hickory Grove
anticline and the Grimes anticline^ ' It is .somewhat in line with
:he Grimes anticline and may be structurally related to it . The
structure is small and appears to have been adequately drilled.
The Gillespie - V/yen oil pool was drilled in sees.
I, 8, and 9> sometime between 19IQ and 1915 and was productive at
Least during 1930-193 &, 'after which "time It was abandoned until
Vugust 19*4-1 • ' There, were seven prbduc ing wells-, and others were'
scheduled to he cleaned but in July l'9l_j.2. Only 12, wells' are known,
ilthough it is said that there, were once about 22 wells in th-o
pool. Eleven of them were producers and two of the producers, were
abandoned shortly after completion,' leaving nine commercial wells
In the original pool. The deepest well of which there is record
La the Duncan Bros. - J. V/eyen well No. 9 in the SW l/k NE I/I4.
IE I/I4. sec. 8, which was drilled to 2560 feet and ended in the
'Trenton" limestone, which was topped at 2198 feet. Production is
?rom the lower Pennsylvanian sandstones.
Unnamed anticlines, anticlinal noses, and domes
1. Sees. 8, 17, 16, 21, 22, and 15, T. 11 N., R. 7 ¥/.
\ southeastward-plunging anticlinal nose.
2. Sees. 16, 15, 23, and 2l±, T. llj. N., R. 7 W. , and
sees. 19, 20, 25, 26, 27, 28, and 36, T. llj. N., R. 6 W. An east-
southeastward-plunging anticline .
Page 36 •
5. 3ccs. 15, lk-t lr3> an0- 1^* T. 13 IT., R. 9 r'»» an<3-
sec. Id, T. 13 II., R. 8 VJ. An eastward-plunging nose. This was
tested Toy a v;cll (Morgan County ITo . 21) which had shows of gas from
695-703 f°et an(3- at 735 feet in the Lower Ills sis sippian and a
slight oil show in Osage ' siltstone between 085 and 895 feet. It
ended : in -the Devonian-Silurian limestones at 1150 feet.
I4.. Sees. 5> 6, 7»' an<^ &> ^'« lU N"«* R"« 3 VJ. A broad anti-
clinal nose plunging southeastward has 'been tested by one well
(Morgan County .No. 1), which reported a show of oil from 20 [[.-20 8
feet "in the Pcnnsylvanian. Another well (Ilorgan County No. lO) in
sec. 2, T. 15' N., It. 8 V;., had a gss' show from yZbr to 3^7 feet in
the Pcnnsylvanian and good oil shows at 800 feet and from 912 to 965
feet, both in 'the Lower His sis sippian. "
• 5* Sees. 53 and 3k-'t T« 1'U N., 'R. '8 U. A small' dome with
very small closure. This was tested (Ilorgan County No. 2) to l68Q
feet and had a show of gas from uOO to 812 feet in the Lower
Llissis'sippian, a* show of oil at* 9^4-5 feet in the Lower his sis sippian,
and a show of oil between 1590, and l680 feet in the ."Trenton" lime-
stone. A well (Ilorgan County No. 20) in sec. % T. lp N., R." 8 ".'I..,
had reported chov/s of oil at 735 feet and 885 feet in the Burlington-
Keokuk limestones.' The possibilities of this small dome do not seem
very favorable.
• 6. Sees. 30,' 31, and 32, T. 10 -N.-, -R. 9- 17 . - Thi-s- small east-
ward-plunging nose has been tested by a well '(Macoupin County N0.I4.66)
which had ah oil show from 227. to Zhfi: feet'., probably in the Perihsyl-
vanian. ' It presumably entered the "'Trenton" limestone, as it went
to a depth of ' I5I4.O feet'. '
The' well (Jersey County No. llj.) in' sec. 32, T. 7 N.', R. 11' -.7.
had a reported oil show in the lower Jefferson City dolomite at 1770
feet. The well' .(Greene County No. lj.8) in sec. 19, T. 9 N./R. 11 7.,
had an oil show at 850 feet in* the "Trenton" limestone, Neither of
these wells is within. the area of outcrop of coal No. 6, hence. 'struc-
tural data for this map are not available at their localities.
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Page ii.1 .
Summary of Formations, Encountered in Deep V/elis
- — — —■ • ■ ■— — y - — — • ■■■ ■ ■ • -- ■ ■ - — ■-■ ■- ■ i , '*■ ■ i. fti ■ ■ ■>■■ ■■+ ' -
Macoupin County No. 1I4.5
Madison .Coal: Corporation . - Diamond Drill Hole No. 15,
S17 I/I4.' NV/...I/I4- .NEl/Vsec. 35, T. 8 . ., R. 6 \7.
Elevation 678 feet.
Formation
Pleistocene sA'-stem
Pennsylvanian system
Top coal No. 6 at q£)8
Missis slppian system
Chester series ■■
Iowa sori es
Stc. Genevieve formation
St. Louis limestone
Salem limestone
Warsaw formation
Burl ington-Kookuk 1 ime s t one s
Fern Glen formation
Chouteau limestone
Hannibal shale
Louisiana limestone
Grassy Creek shale
Devonian system ;.'•''••■'• \
Cedar Valley, Wapsipi-nicron,
and Ba i 1 ey' (?) 1 imes ton e*s '
Silurian system
Niagaran dolomite
Thickness
113
509. l
25
136
161).
Depth to
, bottom
113 .
. 702 , .
'727
lOLS
H87
1512
1^57
1S62
1586
1662
1670
1700
1836
2000-
Altitudo
of top
+ 678
• + 5^5
+270
■ • - 21^
-1022
-115&
Macoupin County No. J4J4.O
Hcttick Oil Development Association - C
No. 1, W 1/2 NI7 l/\+ S\7 1/k sec. 36, T
Elevation 535 feet.
P. Starkweather
UN., R. 9 17.
(Pleistocene system -
(Pennsylvanian system
Mississippian system
Iowa. series
St . Louis limestone
Salem" limestone
Warsaw shale
Keokuk limestone
Burlington limestone
Fern Glen formation
Hannibal shale
Louisiana limestone
Grassy Creek shale
Devonian system
Cedar Valley-YJapsipinicon lime-
stones
-2.97-;
81
75
297-
1076
+535'
3-ii-O
[00
f 238
■>195
539 ■
+105
616
'" - ' h
730
- 81
796
-195
911
-261
915
-376
1001
-360
-k^
Page
1*2.
I la coup in County No.
Ohio Oil Co. - G. Groves, NE lA s^
T. 7 N., R.
7
VJ.
587
Elevation 374- feet.
NY/ 1/1}., sec
5,
Thickness
.t Zl\2
Louis, and
Pleistocene system
Pcnnsylvanian system
Top of coal No. 6 'i
Mississippian system
Chester series
Iowa series
Sto. Genevieve, St
Salem limestones
Warsaw formation
Burlington and ?Ieokuk limestones
Fern Glen formation
Chouteau limestone
Hannibal shale
Grassy Creek shale
Devonian - Silurian systems
"Sand"
"Lime"
1*35
90
300
115
205
88
27
65
25
25
50
Depth to
bottom
15
510
6oo
900
1015
1220
1308
1535
llj.00
11*25
.iltfb
1500
Altitude
of top
+5714-
+559
6k
- 26
-326
-73>
-761
-626
-851
-876
Macoupin County No. I4.63
0. Z. Smith et al - Klein No. 1, NV/ 1/4. Ml I/I4.
SE lA sec. 7, T. 9 N., R>. 7 \7. Elevation
5^2 feet.
Pleistocene system
Pcnnsylvanian system
Top of coal No. 6 at 283
Top of lower Pcnnsylvanian
sandstone at 553
Mississippian system
Iowa scries • -
Ste. Genevieve, St. Louis, and
Salem limestones
Warsaw format ion'
Keokuk, Burlington, and Fern
Glen limestones
Chouteau limestone
Kinderhook shales
Devonian system
Cedar Valley and VJapsipinicon
limestones
30
i**3
,3°
1+-93
282
100
258
21
1I4.2
81+
775
875
1133
115U.
1296
1580
♦51*2
1-512
4.259
4-189
t 14.9
-233
-333
-591
-612
-15k
Page k'j*
Macoupin County No. 372.
Adams and Lagers - A. Bristow No. 1, SE I/I4. SE
.NE lA-.sec. 7, T.-ll N., R. 7 Vf. . Elevation
..:':' . }■'. - '• unknown.' ■ •
iA
Thickness
Pleistocene system )
Pennsylvanian system )
Mississippian system . .:
Iowa series
Ste. Genevieve limestone
St. Louis and Salem limestones
.. ■ Warsaw shale
Burlington and Keokuk lime-
stones ..,,,.-..,
>■ Hannibal, shale
Grassy Creek shale
Devonian system
• Cedar Valley and VJapsipinicon
1 ime s t one s
565
10
285
135
230
100
100
62
Depth to Altitude
hot torn of top
565 .. ',-. .:
575
680
995
1225
1325
1)425
1I487
.. I.I org an County No. 21.,
Y/erner Drilling Company - U. H. Diller No. 1, \'J l/2
,S\7 lA NW lA'sec.. 18,, T.,.;13 N.,.R. 8 Y,\ '
, ... Elevation 666 feet.-
Pleistocene system
Pennsylvanian system
Mississippian system
Iowa series
St. Louis limestone
■Salem limestone
Warsaw formation
Burlington and Keokuk limestones
Osage siltstone
Hannibal shale
Grassy Creek shale
Devonian and Silurian systems
Limestone and dolomite
60
3I4.O
"1°
160
110
I85
13
60
1400
1430
590
700
898
1015
1113
1150
+ 666
+606
4-266
4-236
*■ 76
- 3l4
-219
-2^2
Page hjjt*
Geo.
Greene County No. I4.5
Burruss well in NY/ corner, SW 1/4 NE l/lj. sec. 15 ,
T. 10 N., R. 11 VJ. Elevation 630 feet.' .
Thickness
system
Pleistocene
Pennsvlvanian system
Top coal No. 2 at 155 feet
Mississippian system
Iowa', series ' . .
St. Louis limestone
Salem limestone
Warsaw formation
Keokuk and Burlington limestones
Kinderhook shales
Devonian system
"Sandstone"
1*0
170
10
80
68
2^2
1H0
Depth to
bottom
ko
210
220
$00
$68
600
7I1O
71+5
Altitude
of top
+ S30
4-590
♦l*-75
+i|20
riao
r350
t 30
-110
Jersey County No. ll].
A. 17. Gerson - Knight No. 1, SW l/lj
sec. 32, T. 7 N., R. 11 V/.
'655 feet.
Peter sandstone
sandstone by Miss
NW l/lj. NW
Elevation
1/k
of St
Peter
Correlations to base
Survey and below St.
Pleistocene system
Mississippian system
Iowa series
Salem limestone
Warsaw formation
Keokuk and Burlington limestones
Fern Glen formation
Chouteau limestone
Hannibal shale
Louisiana limestone
Grassy Creek shale
Devonian system
Wapsipinicon formation
Silurian system
Dolomite
Ordovician system
Maquoketa formation
Kimmswick limestone
Dec or ah limestone
Plattin limestone
Joachim dolomite
Glenwood-St . Peter sandstones
Powell dolomite
Cotter dolomite
Upper Jefferson City dolomite
62
by Illinois Geological
ouri Geological Survey,
62 +655
10
72
+ 593
78
150
+ 583
200
350
L05
+ 505
55
+305
35
U.0
+250
50.
k.90
4-215
5
hc) 5
+165
5
500
1-160
25
525
a55
120
%5
+130
160
805
* 10
100
905
-150
ko
9h5
-230
160
1105
-290
95
1200
-450
175
1375
1400
-5fo
25
-720
150
1550
-71*5
70
1620
-895
(Continued on page
hh)
;e 4.5
Jersey C oun t y N o . 1I4.
A. W. Gerson - Knight No. 1, SW l/ij. NW l/'j. NW l/I).
sec. 32, T. 7.N., R, 11 W. Elevation
.655 feet. .
Thickne ss
Continued)
Depth to
Altitude
bottom
of top
1785
19^0
1980
-965
-1130
-1295
2190
2230
-I.325
-1535
Lower Jefferson City dolomite 165
Roubidoux formation 165
Upper Gasconade dolomite 30
Lower Gasconade - Van Bur en
dolomites 210
Gunter formation I4.0
lambrian system
Emmlnence dolomite (?) 5 2235 -1575
Jersey County No. 5
E. II. Gould & Son - G. Pearce No. 1, SE l/ij. SW l/ij. NE l/Ij.
sec. 27, T. 8 N., R. 10 W. Elevation 593
feet.
Depth to Altitude
Thickness bot torn of top
his well reported a show of gas in the Silurian and oil shows in
he Devonian, Kimmswick, cither Plattin or Joachim, and Glenwood.
'leistocene system
'ennsylvanian system
iississippian system
Iowa series
St. Louis limestone
Salem limestone
Wa r s aw f o r ma t i on
Keokuk and Burlington limestones
Fern Glen limestone
Chouteau limestone
Hannibal formation
Louisiana limestone
Grassy Creek shale
'evonian system
Cedar Valley limestone
V;apsipinicon limestone and
dolomite
ilurian system
Niagaran dolomite
rdovician system
Cincinnatian series
Maquokcta shale
60
60
t593
20
80
*533
235
315
[1.05
+513
90
^•278
95
500
+i6g
220
720
+ 93
35
755
-127
$2
787
-162
83
13
8cJ3
-19I4-
-277
22
905
-290
20
925
-312
25
950
-352
188
1138
-357
162
1300
-5^5
(Continued on page I4.5 )
Page I4.6.
Jersey County No.. 5
E. M. Gould & Son - G.'Pcarce No. 1, SE l/\ 5W lA
NE lA sec. 27, T.'8 N., R. 10 W.
Elevation 593 feet.
Thickness
Depth to Altitude
bot torn of top
(Continued)
Mohawkian series
Kimmswick limestone
Decorah limestone
Plattin limestone
Joachim limestone
Glonwood formation
Chazyan scries
St. Peter sandstone
100
20
185
65
35
100
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33333
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of
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33333
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on iv mm
mm on on
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Depth
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L0 L0 V0
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L0 L0 L0 LO L0
L0 L0 L0 L0 L0
L0 L0 L0 L0
L0 L0 L0 L0
L0 L0 L0 L0 LO
Op'r's.
Number
CO
rr
UJ
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CO CO
UJ CO
UJ
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Z _J Z Z
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03 03 03 03 03
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CO O X
x e> o o u_
O O O O
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c c c o o
o o o o o
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O UJ o o o
o o o o
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Z X — z z
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Z _| z z z
z z z z s z
UJ h- _l z o z
Z U_ <_3 Z CO Z
I J J JCDZ
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CO CO CO CO CO
Z) Z> Q o a
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CO S CO CO o
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3 31 a 3 Q Q
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