Tulsa daily world. [volume] (Tulsa, Indian Territory [Okla.]) 1905-1919, 1913-08-31
By CHARLES y, GOULD, Oklaho-
ma CITY. Olla)

ma CITY. OIlal
M. ,,it ...,,f,,,.rt. ,I f,,rd as tho
,..,., is ,.,.r..Ir, 'us.J inrludas an
INK. ,,,,,.,.,.i,,,t.Iy oou ,niI.s Ipnp
49,, IN. 49,, ,,,, ..5 IAN ,,,il,s
,,.d, I..St.d in s,,tb,Yst.rp IIYusa.
,.J ..t.r,, ptl.n.,r,, ,rna LIMITS
,,r''i,,.t,,,.. AKA how, mot vet
.f.., .,.l ,,,..l..ll,.
yiu n1i hS for many Years. l'he
most northern nnipt at which oil has
~ l,,.,, , ,,,. p,.,l,
-, . ttt,, ,,il., sn,,thv..st oi
80 ,., ,r,,, 80, .,,,tb,,eta,,,
, ,,,,I o,,ti,.ont fioId av-
'", ~ ,,.I.r.,,,., irta enc r.,,ot
'",' w." ,r,, 800, nh
VI ~ '',''''' - ,,.,l,to Mi, Tbo
,,'a.,'.,,,,,.gt 1t,,it os ot nrosant de-
,i,,,l g. ,t l,I, ,llr,,oII K t,, county
Lb ~ rn. ,.,,., ,,.,tnf,, v.nich
-, .',,.,.i ~ ,o,,,
on Hun E"S MY n'ot i"u,t" trg ,nnrnvt-
me- ','' ''. - i ~,
h'lely @o'ouu sP"'Ic "',i.' ,,'
pI'' 'iv nv w., ~" ,1,'1,, c,,,,,t,os
,'SH ~
J." N'"'"'' -. ..Li.. .,,o b,.i,.o...,,,-
Nv - 90 - 49,, ,,,,o stotas
p'NS "'' II. w ''1 'it.,,+, ~ por,-
consist thII''N "l lI''"'7 W
.l,, ,sf
c'hl"rIi"nIN' "UuNr ',l' '., ''u'''o ,,nt.
n limestone ol Ml9S'SS'pPl"n as ''.,, ''l9
limestone, "hlCh IL p"p"". NJ" ni
|" Il' on me" az ~, ~,
Ilhr' 'uICI"pa ~" ','' '"i ~ ,, ~
region 'aSl ol ''I'''u W. 81, ,,,',, ,'o,',
t''''Ii 'r ,'""i'.' % %"uT ,,,.,,,o
h'''7'S' NV .'''3' -, ,.i,,,,+
u"h7' Us 'Nl'''u J." '''' ''''
tleId consist OF an hll'iuau S'' 10
of Spudstones, ShalcS ana hinCSlunT'
WIN an "v'1s ',I"' ,,,,..t,,,,,.. a.,L
I<o,sae tbe peunsvlyania rocks DIP
yast at rather constant ancles. vary
irg Cr.n, ufy feet To ,he mile near
tho cqStern exposure {" less than
twenty fnct TO the mile Ia the western
,,,,, ~ IN, or,l In tho southern part
~ IA, r,id-rnntincnt field the rocks
bov, .aa1 folded into series Of anti
cIi,os and evnclincs
ON n4ssing TO the south and west
from the region Of the exposures ot
tbo Roone ebert, the PENNSYLVANIA
sediments thicken rapidly, particular
IL I'm the basal norton ol the series
This fact may be illustrated by com
uaripe the thickness of the Cherokee
shales the loWcrmOst formation OF
p,noevlroni1 age. which lies below
tha Fort scott limestone in various
r,rts of the area. In southern Kan
s,s the thickness Of the Cherokee
.b,Ins. .anproxinate I5O feet on pass
,r.. eouthward the PENNSYLVANIA rocks
rolov. the Fort Scott limestone thick
cn sradu9IN until IN tho region of
NcA1.star i'm east central oklahoma
Tho con,biuad thickness of the Penn
s,.l,.ania sediments below the Calvin
sandstone. which is the approximate
sn,,tbcrn couivaIent of the Fort Scott
,,,,oYtrno nrrroxotcs 10 600 feet
Thickness oi ihm's'o''s.
In southern Kansas 'onSlueI"pl'
part Of the rocks of the FehnSylta-
nian series CONSISTS OF IinleS'ont' ~"
passing south mo Ii,'' oNI'io',a' ,ao,.,,,o
ruus limestones gradualy peC"I'l
thinner ana many "l lne'" VS. ~, anc
while sandstones beSoin' in',t az"
more prominent, an" sl"l'a 80, ~.
relatively thlckPr. a tl"SS - Syo,'',i ,ift,
wv -, .,n ns ,hn Kansas line would
Hl'I'S .u' +" ~ ,h,. ,iar. moro than
snow ulI' ~. ,,t,t,,,ass of mo Penn
oh'-l'uI'" .ii, n,,., .,,,' - not, ~ rma.
syIN''''H ,,,,t,o
stone cross ssc,.u,, .'',i,b t'NJ" ~ he Kan.
'h''" S'N'l a., ,,,,,,ld do,non-
s'N-' ''Nl''.'l" ~ ~, ,,,ortiotb of
strale in"l n''t ~ ia. ts com.
IN l'',ht'S9 ~. '''e
n'sru Oh lII'es'"ll'' ,a,rr,i g,e
s Int p't' '''s"l, az - ttaid oc.
lolnd III 'n' 'l'u ,"' ,.', W., s,rd.
ours un, 'SAlIN J.. '.,.',t,,,,, ,,.itp
stone W" T." 80, H., ,b, graa