REPORT OF THE STATE PALEONTOLOGIST 1902 1029 



In the 500 or 600 feet of shales and flags exposed along the 

 bed of this stream above the horizon in which the brachiopods 

 occur, and below the highly fossiliferous Chemung sandstones 

 3 miles east, plant remains are common, but other fossils have 

 not been observed. 



Stations on or near the shore of Lake Erie 



50 The shore of Lake Erie from the mouth of Eighteen Mile 



creek to the mouth of Pike creek. Exposed : upper Ham- 

 ilton shales, the Genesee shales, the Middlesex shales 

 of the Portage group and the Cashaqua shales. 



51 The ravine of Eighteen Mile creek, from North Evans to 



Ederi Valley. The Cashaqua shales and the Khinestreet 

 shales. 



52 Along Big Sister creek from Evans to Angola and Pontiac. 



The Khinestreet shales and the Bristol shales (or Angola 

 shales). 



53 Along the lake shore from Fox's point to the mouth of Mud 



creek. Bristol shales. 



54 Along the lake shore from Irving to Dunkirk. Silver 



Creek shales. 



55 Walnut creek ravine from Silver Creek to Keech's Cor- 



ners. Silver Creek shales and Point Gratiot shales. 



56 The lake shore from the mouth of the Little Canadaway 



creek to the mouth of Slipperyrock creek, opposite 

 Brocton. Portland shales. 



57 Lake Shore at Correll's point. Portland shales. 



59 Along Silver creek at the High bridge and Smith's Mills, 



and ravine 1 mile west of Smith's Mills. Portland shales. 



60 Along Walnut creek at Forestville. Portland shales. 



61 Terry's ravine, 1 mile north of Forestville. Portland shales 



and the Laona sandstones. 



62 Lake shore in western part of the town of Westfield. The 



Laona sandstones. 

 64 Along Canadaway creek at Laona. The Laona sandstones. 

 Along Twelve Mile creek 14 niile from the lake shore at 

 Northeast Pa. Thin sandstones containing brachiopods. 



