o '

ILLINOIS STATE GEOLOGICAL SURVEY

3 3051 00003 5240

Digitized by the Internet Archive

in 2012 with funding from

University of Illinois Urbana-Champaign

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

-P

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 "— '

H

ft d o o -P o

o o

feO -P d

© © > X

CD

w

w

O

a

o

•H

tJ

^!

©

4-'

r"

©

Cm

W)

O

d

fc

O

t>.

«i

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-.

O

i> Cm -—

M

Pi

©

■H

! Sh

o

m

•H

©

>H

M O

M

•H

-p

O, d

: O

rH

o

O

' -P

Pu d

© rH

o

O

13

o o

-P

CVd

•H

T3

ft

a

O :0

-P O-i d

•H

tJ

a

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-P o

PS

o o

^

O

■H

-P O

M O O

^

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•H

-p o

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£>

6

•H -P O

-P

&

g

<*H

O CD

3

Cm

o co

3

O

-p

■o

O CD

O

Cm

-p

O

•P

© O CD

©

Cm

-p

•

IhO -P

t»n

O

d

»

to -P

Wj

O

d

©

tJ o

!d

•

d

Tj

o

T3 O

d

d

T3

hO

©. S

'_

■n o

>H

- uo

o ^

S-, T3 O

Sh

ti

3

O

© s

©

■,

M

,Q

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•

Bj

\>

rQ

>

o

• d

■£ ^

>

o

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

-P

rH "P W

w

i>

<M ^

d ^

©

-P

P

<U ^

d ^ o

-p

u

O

J> <+-< v —

a

C

5-.

o ^^

i> <H v— ' £

d

o

.-)

Sh O

U

•H

CD

r-i

^ o »

•H

-p

ft d

D rH

o

O

•P

ft d

O rH O

O

Ti

o c

■P ftd

•H TJ

ft

a

o o

-p ft d -h

T3

ft

•H

-p o

fl O O ■H +3 O

,d O -P rO

6

■H

-P o

ri o o ^

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o

g

<i-l

o <o

3

Hh

o to

p

o

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o o to

O Ch

-P

o

-p

O O CO CD

<+H

-p

•

&D-P

bO C

d

•

hO -P W)

o

d

o

T3 O

d

d

T3

o

•n o

d • d

T3

bO

o S

S* T3 O

Ih

W)

a S

^ ■« C $-,

d

,o

O O S

o

•

g

£>

o o s ^

•

> rQ

s>

O

>: ^ >,

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

ll±00 11+20 1605 167O 1705

1805

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-807

-827

-1012

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