SS ere 
D7. KANSAS UNIVERSITY QUARTERLY. 
Orisa OeCMMOnerten Oocrdened len Co mUittha\, UCC « Gigs aay iiey nanan soy ts NGLIM) 
NO, LO LAO POL UO LEDLLOMEOPOLIES. MUGE Kis ere usr bs n'e viv ye lacnl pines aust Can) 
Elis SCO70 207 @ CLSerLAL1S (OW ALLOW} VWWAECeM vied value a doula vetwan Ws 1 UK) 
TAY ACLU RP CULO No LVULtULeCatn ch cteen ol taus ele ay igianucie nn idcaiaen aise Nitrest te Cat) 
13. Mdmondia subtruncata Meek. (>) DEA dhe Me Chats gical CON aie ie a (el 
14. Chenomya Coopert M. and Ty 0). PVA CUO TETRA ec eatedync oh conn ia ent eins alate) 
Broken specimen, impossible to identify specifically. 
15. Crinotd, calyx and numerous segments of the stem...... 
LOn AMANO AAMI OLACES: ATC SPIMES Gi init. (Olu We ead Wid mnie (ic) 
DULCE ALO CER AMINO LUC 1B KN EDLC C Do )ise. uh doghaatntoin th -oheieiisht oa wey GAY Mian Hy etn) 
Specimen identified by Prof. Hyatt. 
It seems probable that No. 2 of this section is the Winfield lme- 
stone, though it was not traced by the writer from Winfield to 
Arkansas City, and scarcely any flint or concretions were found at 
this locality. 
SECTIONS NORTH AND’ NORTHWEST OF ARKANSAS CITY. 
On the hill, two miles north of the city, Mr. Beede measured the 
following section belonging in the Marion formation: 
No. leet. 
COR Soil aie ll itch ala lil atin cfulbal Goealc\sanebalci= eo Mia eR eea ARE SNR Steen yh 8==404 
2) (MMe StOM eS CON tATNIME TOSS SN Hii di dmys Wainy nen law 
Do) Cire I RNSS oh vein wir eCinre Koa Gepttn a: Asta nts MUR beswealfuniec( Abie ie pug uide eat Sema A 
In the limestone of No. 2 Mr. Beede collected the following 
fossils: 
1. Myalina_aviculoides M. and H. WAT RN isin toatoct GoM i ag tO) 
2. Aviculopecten occtdentalis (Shin, , Mee Meant oi aticue yam dr Sane COGN) 
BO OM ROU CIEE DOFUG  Wuy HOTEC Piyis e ni isin Pudi tsle on Sie rsir mORl ky haen (leh) 
Ave t WSEPLOBOIL MIC Hrd SCHNELL VIN CN al phatar Ciulve Yawn Wray u otnieil Gtare anc Ea)! 
&. . Gastropod ct, Warchisona sp. OY LOKonema Sp... i. se se GN) 
Internal impression showing at least ten whorls. The 
largest Gastropod seen in the Marion. 
Oe LIPO OID IST i het darley v8 ly ole eonve eM) Mleth elas veM a URE AINE wh du tue eon sipREONt tr a/c Ga) 
Poorly preserved. 
On the eastern side of the Arkansas river, about two and a half 
miles northwest of Arkansas City, is a buff, soft limestone which 
has been quarried to some extent. This outcrop of the Marion 
formation is near the ‘‘head gates’ of the canal where the follow 
ing section was measured: 
No, Feet. 
FL CLG WITS” SIEVE Sey hyivin taki sr en, ucg vain a MMH nA ar vik MM EAN Vict) 
