7 
156 KANSAS UNIVERSITY QUARTERLY. 
Re A OMUGLULN ILE UP US CE NOLO GD. NET Srv husiniy W sient ans (akin en ale amar iia tee) | 
Ae I CUOLUS LOPSISPLNUS. SON Dei iiiiccal vie Whit a ty siete slilig Wie Wut lon (EH) | 
Ra DITO 62, CONLEM ALIS LINUOMEY wt «signs PEE Mac oR NA Ue iN eonm BRT CRY 1 
6. Spirifer ‘Martinia) wasn ONUEXUS pane Sate teletie MIC ON ES Gr oicer Ahn MCI) 
eS Gmiberevacvcenosac( Vie atic Eoin iin ie cass emia: stan omnia ON) 
) Oe, “a thyris CSeminula): suotelica (Thal Newb iia is ile Wide tal CEE) 
Oy waasLedca wnormon7, CNEATCOUY Fie amg! Giyuaie i vos vce aim tian omaha) 
E GOs 1) GHC CES, CAINMULE IER 0) CNEL) \iulel vay yt suey st Mean it dert ie ends nab 9 (Tap) 
| tt. , Meekella striato-costata (Cox), White and St. John.......  (c) 
12..Husulina cylindrica Fisher...... cichanersanidl wit seaeenetcakeeufataten «ci (BU 
13. Seplopora bisertalis (Swallow) Winhien Sliema ey ty (Ga) 
In addition to the above fist Prof. eee r has oe note 4 the fol- 
lowing species from this cut: 
Aviculopecten occidentalis (Shum. ) Meek and Worth. 
Rhynchonella uta (Marcou) Meek. : 
Spiriferina Kentuckensis Shum. 
Dielasma bovidens (Morton) H. and C. 
Bellerophon carbonartus Cox. 
Pseudomonotis Hawnt (M. and H.) var, sénuata M. and W. 
Phillipsia sp. 
Archaocidaris sp. 
voctdarts Sp. ; 
The bluish shaly limestone of No. 5 contains fossils, dvculopecten 
occidentalis (Shum.) Meek and Worth, dAZvadina sp. and a few other 
species having been noticed. From this cut Prof. Wooster reports 
exfoliated specimens of Sfrrifer sp 
SECTION ALONG THE WHITEWATER AND WALNUT RIVERS FROM 
TOWANDA TO WINFIELD. 
There is a.decrease in altitude of about 325 feet in the sixteen 
miles from the Summit to: El Dorado in the Walnut river valley; 
but the country is comparatively smooth with but few exposures of 
———- 
ea rocks. From Towanda, eight miles south of west of El Dorado, 
in the Whitewater valley, a section was followed in the direction 
of the strike along the valleys of the Whitewater and Walnut rivers Y 
to Winfield,.Cowley county. Four miles northwest of Towanda, 
on the.south bank of the West Whitewater rivér, west side section 
I, Benton township, is the following section: 
No, Feet. 
3. Yellowish shales, which are 40 feet above river level 1==12 
2. Buff limestone containing gypsum concretions, some f==.1 
flint and specimens of Bakevellia parva M. and H. 
: : ‘ : | 
Bri 1. Yellowish argillaceous shales in the upper part and 1o0=r1o0 jj 
shaly limestones at the base. 
