Votums IX. PLaTa X. 
Untyersity Geological Suryey of Kansas. S 
= 
eA 
° 
Zz 
ie 
WAVERLY 
GARNETT. 
PLEASANTON, 
STATE LINE 
DENNIS, MAVALLEVend BETHANY LIMESTONES> 
6 
& 
3 
Z 
o 
fF] CENTERVILL 
BURLINGAME Te 
I— s 
TOPEKA 
(LS CRON — = 
= = —— = = - = == = SS ——_—_— 
LECOMPTON == SS Sea SS SS SS SS SS — —_——— 
= ——— —— == == SSS se —————— 
OREAD: —= Sas = al = Si SSS S54 eee SS SERTEVED 
STANTON=ALLEN~ |= ————- SSS == Sa aa ~ SS SS SS SS SS EEE er 
SS SS SS ae 
DENNIS, Mé VALLEY. ax, 
a 
a 
is 
a 
NEOSHO 
H 
\ Leeo 
y 
\ 
vs 
a 
1 
1 
a 
x 
4] 
iy 
4 
ARETHANY. 
ALTAMON 
PAWNEE 
Fe 6COTI— 
2000) 
. 
ites 60 : 60 70 60 50 40 80 20 10 
o + — 1 + — — 1 J n 1. 1 + ooo ——e 1 —. see Se i 
FIG. 1. 
‘A yertical geological section from the state line east of Pleasanton to about one mile west of Emporia, passing through or near to the several towns and cities named in the plate. This section represents the several 
limestones in sequence from the Fort Scott below to the Burlingame above. The spaces occupied by interbedded shales and sandstones are left vacant to avoid confusion. It should be noted that while the limestones are 
represented accurately as regards sequence, the slight undulations are diagrammatic, merely representing the general fact that such undulations exist. 
= 2 
8 5 
BURLINGAME w =) ia ONE one > = = SS 
Nia nN ST ‘ow 
ae XG 35 9 ures 5 ner ences Mon wnesre™” < res & z a <one ® 
OREM 2 vi res ERO coor § © pach? = STANTON-ALLEN LIMESTONES = nies) 5 
DEER GREEK : : : eat = =O & x = SS = = LE Of 
= = THES 
OREAD— = ee a 
a = oa: 
STANTON@ALLEN = = <== iz === SSS eo 
12LaA———_ == SSS SS SSS SS = — — 
DENNIE,MeVA!.LEY, - ea Ste 
aw! BETHANY- F Byes ais 
PAWNEE 
SCOTT. 
Fis00 
E2000) 
70 60 ow 40 30 20 10 
pe IL nl a San i ee abn 1 fn = AGS 
FIG. 2. 
A vertical geological section from the state line east of Paola to about ten miles west of Osage City, passing through or near to the several towns and cities as shown in the plate. This section represents the several 
limestones in sequence from the Fort Scott below to the Burlingame above. The spaces occupied by interbedded shales and sandstones are left vacant to avoid confusion. It should be noted that while the limestones are 
represented accurately as regards sequence, the slight undulations are diagrammatic, merely representing the general fact that such undulations exist, 
