I 58 KANSAS’ UNIVERSITY QUARTERLY. 
the Florence limestone, so well exposed on the Cottonwood river 
at the city of that name, is the same as the Fort Riley limestone on 
the Kansas river at Fort Riley and. Junction City. 
On the bank of the Little Walnut creek, two miles northeast of 
Douglass, are shaly buff limestones, apparently in the ‘Florence, 
which contain the following fossils: 
Li LANES \COSCMINU La SUATILILA (ELAN ING WD re ie wea dl ruty gn CO) 
vi CPOE eC NG N Ger UNL CL Ate Ne bali g’ ELL CEN Ca avila. & putiomeaye a MAL Meine MCh velvet OLR) 
BL DeP LM TULLE TALE CNN CUT Gliy Wali )) Me LOBIs sere ‘ees Vike nt veg (on) 
A. aorewlopecten, occiwencavis (Shtim.) Mi and Wa cilia sie s (rr) 
Bin ICD EO DORE OLSAPTCELES: 1 0) WELLLO Wr )'s) VVC OM spo airs bisert ctr ev es'gegh vat be CMY 
Wi ULL ESV PLCC Mi NEN MTU UU Chistes ie ue atada liens ede vowyoii Mas eautoate x, CL) 
From Douglass along the valley of the Walnut river to Winfield 
there are frequent outcrops of the Florence limestone, and near 
‘the summit of the bluffs the Winfield limestone. In a railroad 
cut, two and one-half miles south of Douglass, is a good exposure 
of the Winfield limestone and forty feet of lower shales. There 
are numerous small rolls sHown in the cut, both anticlinal and 
synclinal. The section is: 
No. Keet 
3. Massive limestone which weathers rather rough and 11==51 
contains some fossils. No concretions at this locality. 
Winfield limestone. 
Vellowishrareulaceonsiehaligsn sa Wieden pani 2OmAO 
dS 
1. Variously colored argillaceous shales, greenish, ma- 20==20 
roon, yellowish, etc. Some of the maroon layers 2 
feet thick. No fossils found in the shales. Rail 
road level. 
These colored shales below the Winfield limestone correspond 
to similar shales described by the author in the Cottonwood valley 
below the Marion limestone, as the Winfield limestone was first 
called.1 The Winfield limestone above the railroad cut, at this 
locality, contains the following species: 
Te LPOMUCTUS SEWLIPCLCCIN OLS (MLA LLIM CLE VCO Alt wish vn MiiewieN ar nC DYN 
Dil D CRONE CHISSO rn Ww BUCS WEA i)* ante eile Gaiety: Gaaeh ae tate at a voliseaper col (BN) 
Some of the specimens are near D. multistriata (M. and 
Ey Pros: 
Bi WS CALIO AAS VAMECLERE COM EILO Wo WRGEIE (BY us 0 virccade nicinre i eet yc ev CtUn) 
4. Archeocidarts HOLME ad RAPA ORO art NRO GEN ULdiehinGy ony lial OE) 
Spines and plates. 
In a small run on the south side of Rock creek, six miles south 
L: Jour, Goolkiwoli Ulypy tis 
