Votuma IX. Prate XI 
University Geological Survey of Kansas. 
COTTON woot 
BURLINGAME- 
TOPEKA _— 
DEER GEING fix coil 
LECOMPTON SS 
OREAD: 
KICKAPOO- 
STANTON=ALLE! 
IOLA 
DENNIS, M2VALLE) 
and BETHANY 
PAWNEE——~ 00 
Fe SCOTT- 
AWRENCE 
MAPLE HILL 
WILLARD 
| LECOMPTOW 
I STATE LINE 
30 20 i a 
90 60 70 oo 59 40 
Se Eee — 
== “= . — 
FIG. 1. < 
A yertical geological section from the state line east of Olathe to and beyond McFarland, 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. 
MAYETTA 
BorLe 
BURLINGAME 
HOWARD 
TOPEKA, DEER CREEK 
LEAVENWORTH 
and LECOMPTON: 
OREAD. 
KICKAPOO 
STANTON@ALLE| 
IOLA 
may MISS/SSIPPIAN 
DENNIS, NaVALLEY, 
and BETHANY- 
PAWNEE. 
Fe SCOTT- 
aso 
—— 
FIG. 2. 
; A vertical geological section from Leavenworth westward to Mayetta, near Holton. It represents the limestones in regular sequence from the 
Mississippian, reached by drilling at Leavenworth, upwards and including the Burlingame. The spaces occupied by interbedded shales and sand- 
stones 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. 
STANTON@ALLE| 
TOLA: 
DENNIS, MAVALLEY) 
and BETHANY 
PAWNEE- 
ROBINSON 
FIG. 3. 
A vertical geological section from Saxton, Mo., to Hiawatha, Kan., showing the limestone formations in regular sequence from the Mississip- 
pian upwards to and including the Burlingame. 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 repre- 
senting the general fact that such undulations exist. 
