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 Mi ning 
 
 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 Co lchester 
 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 * f c J» slato"" (one or both of 
 are, except for aVin.bed of coal -^ ^ of drlll _ holC s 
 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 . 
 
 Co al "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^ 
 
 — S 2 ott ^ 11 ^ i^S? Sf ^tE^SS^S- northwestern 
 Apple Crook and its triout-ries in vll i are 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 * ? rto C 22°5 r xeet e of PennsySa^Ln Strata overling the Herrin 
 C 1 °eoal 2 bed f c°™iy shi -o limestones the "pper one of 
 which is undoubtedly the carlinville l«£f°™' ££, re3peo tively 
 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»^ ££££ a g tho3e Um0 _ 
 relationships as dos ; rl ^ ed '.^ s "„ttville limestone lying about 100 
 feerbelow^rcarlinvi^le^nd^about 1 ^ 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 Intere st 
 W ith Respec t 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;wn 7 kti?udr f 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 2 5 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?ed y datum 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 Pre s ent Map and 
 Preparation of Ma ps of Other Areas 
 
 The present map is the fifth of a series of maps showing 
 , hfl qtruc ture 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™ (in n coopJation with U. S. Cool. Surv.) 
 Bull. 51, 1915« 
 
 ~„ ^-r m'c-tT'ipf VTT (southwestern 
 , « -rr „ 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 - u w _, -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. 51-59, 1917. 
 
 ' Oil and gas In the Gillespie and Mount Olive 
 
 quadrang les, Illinois-: .. Illinois Geol. Survey Bull. 5 1,. 
 
 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 - 
 
 1 9 . Worthy A. .H., llf°lll% 2 _ 133 7 , i8 68 ; 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 tne G cSr 7tne year" 
 1930: Illinois State Department of Minos and Minerals: 
 p. 16, 1931. 
 
 22. Fifty-ninth eoal report of Illinois 1 9 ^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 
 
 
 
 ■R 
 
 
 ■• • ' U O 
 
 
 > ^H W 
 
 f^ .. 
 
 c • 
 
 '^ O 
 
 
 > c_ -^ 
 
 £ 
 
 Pi 
 
 
 03 
 
 rH 
 
 fc o ■'.: 
 
 S 
 
 •H 
 
 CD 
 
 H 
 
 Sh o 
 
 ^ 
 
 •H 
 
 
 P &( 
 
 trf 
 
 : i— I 
 
 O 
 
 O 
 
 -P P* 
 
 erf 
 
 , 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 . 
 
 
 •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 
 
 Cm 
 
 -P 
 
 O -P 
 
 
 o O'to 
 
 Cm 
 
 ■p 
 
 
 
 • 
 
 tiOtP 
 
 bO O 
 
 erf 
 
 
 . 
 
 fafl-P 
 
 hfl O 
 
 • erf 
 
 
 <D T3 
 
 o 
 
 <rf • 
 
 erf 
 
 T3 
 
 T3 
 
 o 
 
 rf : • 
 
 erf 
 
 tJ 
 
 
 UO 
 
 |21 
 
 inlti O 
 
 M 
 
 
 bD © 
 
 S 
 
 ^ -d :0 
 
 U 
 
 
 
 £ ,0 
 
 
 CD .0 & 
 
 Q> 
 
 • 
 
 M rQ 
 
 
 © .£5 
 
 
 
 • 
 
 
 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 
 
 13 
 
 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 
 
 f D 
 
 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 r d' o 
 
 cd • 
 
 
 ■ <3 
 
 T3;. , 
 
 CD Td 
 
 
 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 
 
 '• "' , ' 
 
 
 5 1 
 
 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"' 
 
 -5 M 
 
 
 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 
 
 
 
 •H T3 
 
 CL, 
 
 X! CD 
 
 
 -P rQ 
 
 § 
 
 CD <Vi 
 
 -P 
 
 U0 O 
 
 Ctf 
 
 OS 
 
 T3 
 
 5h 
 
 
 
 
 • 
 
 t> 
 
 o 
 
 < 
 
 IS 
 
 181-233 
 
 205 
 
 7 T 
 
 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 
 a 
 
 si ^ 
 
 > ■-H — 
 
 S-. o 
 
 O rH 
 
 -P P* cS 
 
 a o o 
 
 • H P O 
 
 O CD 
 bO-P 
 
 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 
 
 
 
 (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 
 
 
 
 KO Ch 
 erf o 
 
 M 
 
 
 
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-' -6 U 
 
 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 
 
 
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 M 
 
 
 Pi 
 
 
 
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 •H 
 
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 t»n 
 
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 • 
 
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 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'-6 n 
 
 9 
 
 81 
 
 6 ''-6"' 
 
 • 1 
 
 Scottville coal' 
 
 32-49 
 
 40 
 
 0'-5" 
 
 4' 
 
 
 
 
 3 iasa Is.- : 
 
 30-36' 
 
 : 32 
 
 5'' 
 
 11 
 
 . 40 
 
 3 »-6" 
 
 1 
 
 Vo. 7 coal 
 
 24-29' 
 
 27 
 
 l'-2 Tt 
 
 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 
 
 • 
 
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 Cm 
 
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 w 
 
 M 
 
 Ci 
 
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 P 
 
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 C 
 
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 ft d 
 
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 Ti 
 
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 ft 
 
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 T3 
 
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 -p o 
 
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 6 
 
 ■H 
 
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 o 
 
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 3 
 
 Hh 
 
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 <+H 
 
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 d 
 
 
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 o 
 
 d 
 
 
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 d 
 
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 d • d 
 
 
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 s> 
 
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 Bed 
 
 rt 
 
 
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 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'-10 M 
 
 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 
 
 x 52 
 
 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 
 
 x i5 
 
 
 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 
 
 7 il 
 
 • 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 
 
 8 J 
 
 
 
 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 
 
 1 5J 
 
 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 t op 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}"' 
 
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 352 
 
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 1030 965 \ , 
 
 V^ f 
 
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 AMON 
 
 13 
 
 MACO 
 
 UPIN 
 
 578 
 
 -6- 
 
 T 505 
 
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 4 
 
 1586 
 
 1 
 
 1 
 
 1 
 
 i ^ 
 
 1828 
 
 + 
 1487 
 
 + 
 
 328 633 
 
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 [ 
 
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 ,9 
 
 8 
 
 T 
 |7 
 
 1 N 
 RY 
 
 745 
 
 
 
 1076 
 
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 496 
 
 CARLINVILLE> 
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 485 S 50 
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 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 
 
 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) tolin S ton -^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 S i 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\y7temr m ^ reWQS ^^ ever ^ lo ^^'^^P^of : Mie Pennsyl- 
 
 , ni , HloD l he 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. Burto n- 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.h a< ! 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 N orth 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? a nd 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 
 
 .'Without 1 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- • Cto e 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 a nticline . - 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 i n "the Gillcspie-Mt . Olive folio. 
 
 In sees. 20, 29, 32, 33, and yh r , 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. se c. 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 No 4 . 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> J 3> 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. 
 
 U nnamed 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 l r 3> an 0- 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° e t 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 yZb r 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 . 
 
 Su mmary of Fo rmations, Encountered in Deep V/elis 
 
 - — — —■ • ■ ■ — — y - — — • ■■■ ■ ■ • -- ■ ■ - — ■-■ ■- ■ i , '* ■ ■ i . ft i ■ ■ ■> ■■ ■■ + ' - 
 
 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 
 
 h c ) 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 
 Thi c kness 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 
 
 -707 
 
 -807 
 
 -827 
 
 -1012 
 
 -1077 
 
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 UJ Ll) UJ UJ UJ 
 
 uj uj a. u. u- 
 
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 Op'r's. 
 
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 1*11*1 1*1 1*1 Nt xt 
 
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 03 03 02 03 03 
 
 03 02 03 03 03 
 
 03 03 03 03 03 
 
 03 CV 03 03 03 03 
 
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