122 Gr 5 . REPORT OF PROGRESS. I. C. WHITE. 



thing along the valley we should see about 75' of the upper- 

 most Chemung rocks. 



The Drift is largely composed of rounded and angular 

 bowlders of local sedimentary rocks, but occasionally we 

 find a small one of granite or other crystalline rocks all 

 rounded and polished by attrition. 



Near A. F. Shaddock's, in the northwestern portion of the 

 township, a great cliff of sandstone is seen extending along 

 the hill on the west bank of North Wyalusing, at an eleva- 

 tion of 225' above the same and 1145' A. T. The rock is a 

 greenish-gray current-bedded sandstone and has a thickness 

 of 25' ; it is the JVeio Milford Lower sandstone, and is fre- 

 quently seen between this and the mouth of the North 

 Branch. 



Barometric elevations in Hush. 



A. T. 



Forks of road near R. Reynold's, 1050' 



Level of Wyalusing just opposite, 1010' 



Forks in Grangerville, 1025' 



Forks near H. H. Gray's, 1080' 



Cross roads near W. L. Vaughn's, 965' 



Level of Wyalusing just opposite, 950' 



Forks near Mrs. M. Hillis's, 1015' 



Level of Middle Wyalusing near by, 990' 



Forks near L. C. Tupper's, 1015' 



" M. Bradshaw's, 1075' 



" J. C. Shaddock's, 935' 



» H. Carter's, 920' 



« N. Hillis', 885' 



Level of Wyalusing near by, 870' 



Forks near J. T. Hillis's, 900' 



" D. Hillis's, 985' 



" J. M. France's 1470' 



«« East Rush P. O., 1245' 



" B. A. Jones', 1360' 



" A. C. Steadman's, 1245' 



17. Dimock, in Susquehanna county. 



This lies east from Auburn, and the drainage is south- 

 ward by way of White and Meshoppen creeks into the Sus- 

 quehanna river. 



The rocks of the township all belong to the Catskill sc- 



