/ 
Reet 
166 KANSAS UNIVERSITY QUARTERLY. 
Ae’: PEOUUELUS COPA, COUNT hal hentia seantie, (Rnn RURIRG And oie (r) 
Len dy a POD USE a ( Tl ealipy Ble ean Clie Ge Go Naika ee Naha 
Similar to eer, play Pals Yow VEE, Me bed 
Oy Derdya: crascac( Ms aman ibaa Cen tis wey eM rcuminy toate aCe) 
7. Septopora bisertalis (Swallow) Waagen.. 6... 0.85.0. (Ce) 
8. | Meekella striato-costata (Cox) White and St. Johu...... (rr) 
QO. Khombopora ‘lepidodenmpoides Neeley eh iawn ae ete CEE) 
DOs! AM ASCULE POLE AGUUIT Endy MICE Is: Cue notia tie Wace aigsii tihalc. KCEE) 
A flat specimen which apparently belongs to this spe- 
cies. 
LL) CHOROtd SORA T TS). side iy tentemgeh Pe Wiese catie wn oen a deyse wt ocr hay st. AIRES) 
In No. 10 the seven species of the succeeding list were obtained: 
Le SREY er CamEP ALAS NUCLEON Hele ie eie mun Gaius i (c) 
2. Athyris (seminula) sudtenia (Eval bi New Dian yin dnvien (rr) 
8. Aired Ucaus\ cor Md OE DID aston UMA mr atonal eRe ChE) 
He | CHOMECEN SPOMUITENT OM ERE A Mertibe doin aehinke babe nety core rn yt CC) 
Be LUSHLINA CV RAKOCH ATION Gt Ui Navarre Wayne) 
Abundant in layers. 
OCF) Wistulipora nodalefera NCB ss Wh cael boo alms ee uit) CEE) 
Tal MICEROBORI FT OSSEPT WG ETCH Matea Me tre fee emir Miya Cc) 
Identified by Ulrich and described in MS. 
From the bluish shales at the base of No. 1, on the bank of Big 
Caney creek, the following species were collected after a hasty 
search: 
Ly QUAL] CF COMED CULES LOM Ue ule) Win das Reale a RNG er toon i hati ne ere CGY 
Qs ET OCUCLUS: CORE. Cr COLD IRD iit salle AiMaMvtuia aay ay wlan seyne eaten (CEL) 
Bet LPOUUClaSY REOKUSCHHSDS KI WET ict n tla nielne critica api Kae) 
4. Aviculopecten carboniferus (Stevens) Meek rin... Cr) 
Prof. Broadhead regarded No. 11 of his section—No. 5 of mine 
as ‘undoubtedly of Permian type and the strata may be considered 
Permian,”! while I would locate provisionally the base of the Per- 
mian some sixty feet higher, perhaps at the top of No. 18, which 
equals No. 5 of Broadhead. 
CAMBRIDGE SECTION. 
The Strong limestone may be readily followed from Grand Sum- 
mit to the southwest along the Cedar creek valley to Cambridge 
and the Grouse creek valley. At various places along the Cedar 
creek valley or its bluffs it forms a prominent ledge, and about one- 
fourth mile west of Cambridge is an extensive quarry in the lower 
part of the Strong limestone. In the Grand Summit cut the base 
} Op, clt., p. 487, 
