there crops out a very hard band of gray sandstone with some 6al 
cureous 
arid ’iron. 
I hi 
04 
surface this band is colored 
a deep brown by tne iron. The/thickness varies f rom4” to 8 M ,tne 
lower 'portion of the rock hfOTTng been deposited in wave depress 
ions. In these small basins asit we re, fossils are very numerous. In 
the lowest inch there are great 'numbers of a small diehotimose Cer 
dtopora. Just above the Cerat operas, the rock is full of Product 
ell as, Or Inis impressa,5pirifer marcyi , Leiorhynchus mesacostal is , 
while a single modiomorphoid Leptodesma was seen. The upper 2/3 of 
of trie sandstone band are barren, and where the band is thinner, 
at the wave crests, no fossils are found. This band shows a dip of 
60 ft! per mile a few degrees east of north. Above this band ,and 
below the next higher one, there are seme blocxy shales, 5or6 ft. 
thick at the s . w . end the outcrop, but in going about lOOft.n*. e. 
these shales increase over 1ft. in thickness. The higher bands are 
mostly barren. The upper portion of the outcrop is less fossiiifer 
bus than the lower. In a few places there are clusters of Leiorhyn 
chus mesacostal is ,but the lammellose form of Delthyris mesacostal 
is predominant throughout the upper portion of the cliff . Fossils 
from the hard band at 1105ft .A. T. , are labelled 7B4. 
6. In the bed of the creek at 1180 to 1190ft. A. T. , are some b 
a hard band at 1182 ana some hard bands in i he 
the bovver hard band, for 1ft. fossils are 
' * " v *'i . •, .•« • , 4 . Ca- " '2 .■ 7 . w*-. ^ t k 
a band of Productella lachrymosa, Schi zopnorju 
blocky shales with 
upper portion. Just 
nu merous*. There? is 
iupressa, with some Spirifer marcyi/ and Leiorhynchus mesaebs tails. 
A couple of inches higher # but still, below the hard band,, are 
found some inmenses specimens off Spirifer marcyi 3” to4J__wlde, and a 
