2. CARROLL TOWNSHIP. F 2 . 167 



Greenish white shale with plant-rags, . . 3 



Yellowish white sandstone with sandy shale and plant-rags, G 



Green sandstone with sandy shales, 4 



Red shales, . 8 



Green sandstone, 4 beds, with thin sandstone partings, . . 4 



Green sandstone with plant-rags, 2 



Green and yellow shale with plants almost forming a thin 



coal bed, 1 



Red shale, 3 



Green shale with plant-rags, 1 



Red shale. 



The beds shown in this section lie above those to the 

 east of this road on the land of Mr. Borroll and Mr. Grier. 

 Judging by eye and taking into account the small dip, they 

 must lie about 300 feet above them. The whitish Kingsmill 

 sandstone with its fossils should cross the road in the 

 ground north of the mill ; but so many stones have been 

 hauled here for the purpose of protecting the land from 

 the ice that it is impossible to distinguish them from the 

 rocks in place. The ice, too, has brought down quantities 

 of large bowlders and scattered them along the bank. 



Above the mill and for some distance below it the creek 

 is working to the westward and cutting away its right bank. 

 Below that point to the bridge the other bank is being 

 washed down. 



On the opposite side of the creek and above the mill are 

 some fossiliferous beds in the green shale and red sandstone 

 which have yielded a Lingula and some other fossils not 

 yet identified, but indicating transition beds between the 

 Chemung and the Catskill. 



