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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 

•H 

-P     o 

PS 

o   o 

^ 

O 

■H 

-P     O 

M      O      O 

^ 

© 

•H 

-p    o 

-P 

£> 

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 

©    ©   S 

© 

• 

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    ^ 

•rl    -p      o       -P 

o 

g 

<i-l 

o  <o 

3 

Hh 

o  to 

p 

o 

-P 

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 


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