FOSSILIFEROUS LOCALITIES—NORTH SHORE. 353 
‘ Feet 
Comme] OMMET ALE ah ois eles cette ale ae Siseric hac tee erat cata taen teare ois 80 + 
WoallivAShAle Ns: cee sectivee susrcevevansiarciare aie ae eters eee ster anicke 8 
SAVINGS LOM Cb eyne sateen terete tetera cy Aenea Ta ee pea I A 20 
Cenk? SOG) Om siemcamn a Sara mnee aes ni mr arrose atime 10 
SAMS COM Oe etrtyety a icay steps econ cee, oalicnns crekerhat etre eee erste 25 
innysandstones|andicoalsis.qaqq-ers oes eeer aoa 10 
Coarse yellow sandstone and conglomerate ............ 30 
Coalivashrall Cutter yas gietre onsite pneeete oy macorecatore reke eweorseats 1 
@onclomeratesee eee en a ee apts Feta ee ON Ear ates 20 
304.5 + 
_ 074.5 
Dark carbonaceous sandy shale (plant bed ‘C”’)...... 4.5 
The second plant horizon (“‘B” of profile sketch) is west of the fault 
and occurs about 30 feet above the heavy bedded conglomeratice sand- 
stones. It has a clearly different flora from that found east of the fault 
in that dicotyledons are far more abundant than are the accompanying 
ferns, cycads, and conifers, although the number of dicotyledonous spe- 
cies is not great. The following named species occur here :* 
Pieris frigida Hr. KkA. Zamites speciosus Hr.? Kks. 
Aspidium ursinum Hr. Kk. Z. acutipennis Hr. Ks. 
Asplenium dicksonianum Hr. KsA. Pinus crameri Hr. ? Kkps. 
Gleichenia rigida Hr. KksAP. P. eirikiana Hr. Kks. 
G. zippei (Corda) Hr. KkpsAP. Phyllocladites rotundifolius Hr.? A. 
G. nordenskioldi Hr.? Kips. . Populus berggrent Hr. A. 
G. gracilis Hr.? KkpsA. Platanus heeriti Lx. A. 
G. nauckhoffi Hr. A. ; Hedera primordialis Sap.? A. 
Nathorstia angustifolia Hr. Kp. Ficus atavina Hr. AP. 
Cyparissidium gracile Hr. KkpsAP. Cassia angusta Hr. A. 
Sequoia reichenbachti Gein. KkpsA. Laurus n. sp. ? 
S. gracilis Hr. Kkps. Quercus n. sp. cf. Q. rinkiana Hr. A. 
S. schmittiana Hr. Kops. Quercus n. sp. cf. Q. ferow Hr. A. 
S. fastigiata Hr. AP. 
The third locality (‘C ” of profile sketch) is some distance west or above 
the western conglomerate, being about 35 yards east of the third or western 
dike. Here again we find dicotyledons well represented along with ferns 
and gymnosperms of Upper Cretaceous age. This flora has: 
Sphenopteris fragilis Hr.? Ks. Sequoia fastigiata Hr.? AP. 
Dicksonia johnstrupi Hr. K. Pinus eirikiana Hr. Kks. 
Ginkgo multinervis Hr. A. Platanus heertti Lx. A. 
Widdringtonites reichti Hr. AP. Celastrophyllum cf. newberryanum Hollick. 
® 
*For the determination of the dicotyledonous remains the writers are indebted to the kindly 
assistance of Dr F. H. Knowlton, of the U. S. Geological Survey, who has also furnished the lists 
of plants collected at Ata and Patoot. 
