Section up Swartwood road from 7B to 9C. Aug. 18 to 25th., 
1.* Opposite the house of Jno. Woolever in the roadside, 
. of gray *and olive, iron stained arenaceous shalhs.Two fossils 
one of Spirifer raesacostal^ 'found in talus. ': 1065 to 1077 f t. A. T 
”“‘2T~fne upper or tTi'orTo f t ne s e beds' conti r ues -in . t he “ c r e e k 
wjust west of the second bridge, below the small falls of two feet. 
• ; Where exposed in the bank of thestream, the shales are blocky and 
contain a comparitivelyrich fauna of Rhipidomella vanuxemi? , Leio^ 
rhynchus mesacostal i s, Product ellu lachrymosa f Chonetes scitulus,- 
Scnizopnoha impressa ,Ambocoeiia umbonata, Spirifer marcyi , Lingula 
complanata , Pterineu /chemvtngens i^, ?0 rthetes ‘ chemungensis ,'Camaro 
iia sappho, etc. 
7B2 .1 ' 
1075 to 1079 ft; AT 
3. A 6 M hard sand&to'he 
orms a small 2ft. i'alT over 
7A2 I The shales similar to?Al continue 15 ft 
b ana, but are poor in fossils 
Cl O JL 1 i 1.4 
(V3 & 
above the sandstone 
TOO yds. to trie 
• t 
e crop du t in the roadside 
85 ft. of similar shales, with a fauna like 7A2 characterized 
by Leiorhynchus mesacostalis and Productella lachrymosa; but in 
lien no Chonetes was seen. Spirifer mesacostalis and Sp. marcyi 
are quite common in some bands .There are three or fd>ur 6” or 
Ifcf sandstone with many smaller 'bands of more arenaceous shkl 
.In 1 ' some of the latter fossils are common. There is a dip of 
50 ft. per mile a few degrees east of north. These beds are from 
1090 to 1175 ft, A.T. * 7B3 • • 1 
5. About 15 ft. above the base of thiscliff, at 1105ft, A.T 
