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BULLETIN 613 
: 96 9530 +=: KANSAS 
EXPLANATION Thickness —_ ‘ rr 
$e | Cc : in feet ' cA 
$e } A River deposits (stippled pat-  Alluvium 50 Quaternary 
a a tern) 
© Ny B  Limestene Wreford --- ">. D 
= filli aio pce a we ‘fer 
a fil : e Carboniferous 
s \\ | C Shale and limestone Garrison 140 7 (Permian ) 
HA ae ‘ ab rigs 
j ie D_ Limestone Cottonwood «= “#5, 6 J 
1 il i (Shale Eskridge 7 H 
ol! \ E +Limestone Neva 170 | : 
2 i \ ‘ Shale Elmdale 
a | * 
br 4 i b F Limestone Americus -~-—-5_-™. 8 ey 
8 “ | | = G Shale with limestone layers Admire 270 < 
= i uw i st 
Sl i > H Limestones separated by shale Emporia +07***.00 00°". 9 ee, 
> a . és " . So 
Sti Al = | Shale with thin limestone Willard 45 > 
ey | wi : ; ; e 
“Ts i ti J Limestone Burlingame —~~~—~ 10 oe” 
i HN A Shale ‘ n 160 Aes 
Boni i Li Se K-4 Limestone and shale 10 | Carboniferous 
Eel i <* E Shale with coal near top very 50 f (Pennsylvanian) 
‘ Lit Big 33‘ Limestones separated by shale Topeka —“\““VUU,_ 5 : 
i Mn a 
3 Hilt | w 2 Shale and sandstone Calhoun 50 
3 hh i lk re M 4 Limestone and shale Deer Creek 25 
estone-}'l'; i H ew Shale Tecumseh 75 = 
iy > eon 
vi i | -§ N_ Limestones separated by shale Lecompton -~1_/\/ 22 
2 Pi | cs Q Shale Kanwaka 90 
® 1} z J 
“ F2 9 P Limestones separated by shale Oread ----.70 BO 0 
e re Q Shale Lawrence 200 J py S 
Zz 
O8 3 ra ©°000°A pproximate southern limit of Kansan ice sheet of glacial epoch. \ BS sea 
BY e . The lines show the eastern limit of each belt of limestone, not the full width of > ee aed P aK 
& |i za utcrop. ; ye x 
| Fu 1 | pe dk an 
= ao Scale 500,000 j . 
Be Og Approximately 8 miles to 1 inch a \ 
© pte gg ee tin | S213 
Nien ge 2 8 em. tmmees A Ame y <p lt 
itt ze = Cont . | 200 f FE Scranton IY Qverbroo : : ce “Al : 
f 4: = ontour interval 200 feet EL. 700“), i fee “3 RM Le 
He )) ELEVATIONS IN FEET ABOVE MEAN SEA LEVEL ee ee ie oe igo cere CSyt 16 
: EE Op city mt ha, Ay mn . i Yih BSL 
2 < - ; ee 
a GH The crossties on the railroads are spaced | mile apart \ ‘i SS Eg if 
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SECTION SHOWING RELATIONS OF LIMESTONES AND 
8 
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