Stratigraphy ofl^afisas P$rwJanr~-Bee;c(eand Sellards. i\\ 
than three inc^^lFy*£bc^rt/hi30GFrtk2fer ^Thevlacation of the 
escarpment north o-ivthfiiKanfiasiK riv^r* t .was; taken from 
B > f> T-he third of thes^rnaps is to he found in .the Cotton-. 
wood Kails folio of. the JUL S. r Q'epjpgifal Survey .$ . This inap 
s^ows the details o4-.^he !( s4raj;%rap^ Q^theLropks wjthii^jg 
aj^^iscussed in this. article,, and M>.<iJt, tfre. reader, js referred. 
fo-r an: idea.of the.jntpicale. nature of much .of the ,.outcrop : jO}f 
%^WiF^rA\' imes ^^- : sirfo rbirfw «i 
} G s -f tChj^ data of the fir s,t and -last maps mentioned were usgdj 
if-^-ely in constructing .^he accompanying- map, on which is. 
sbpwm. tfhe outcrop) of • the Wreford, limestone. The lin#!pfrj 
tween Eskridge anfi Junction City is hypothetical ajpart,- $$ 
the way. as it is, lpeally,, jt+ipugh always, in very mu-ch short^F 
distances, in a few other places. The width of the s^r f §ftr% 
e|che4 portions <>f the escarpment t£- purposely- enlargeid for 
^e^-saj^-pf-rcl.earness. Southern Cowley county h^sn-o^r)^ 
been .mapped;. ' >"'g ^rft 
t, t-r&n?: Karik Acad: 'SciV^v'tfi',' 1903. • ' ' " ~~~ ~ ' ~ 
; Cottonwoodr Falls Fo]io.. U-. S, Gepl. Sjirv. Atlas, number 109. Pvos- 
AfJ'anfl Beede," 1904. ' ^ 
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