182 G 5 . REPORT OF PROGRESS. I. C. WHITE. 



About 2 miles west from the former locality, and near 

 Wefferling's Tannery, a massive grayish-white stratum of 

 sandstone is seen at 1475', and below it comes a layer of cal- 

 careous breccia which very probably represents the Cherry 

 Ridge limestone. 



As we pass eastward from the Upper Wilcox Pond, the 

 base of a gray sandstone is seen at 1450' A. T. and 60' higher 

 up is seen the base of a grayish-white rock with a layer of 

 calcareous breccia at its base. 



Barometric elevations in Oregon. 



A. T. 



Forks near M. E. church at south line of township, . . . 1400' 



" A. Fox's, . . 1520' 



Cross roads at School House No. 4, 1490' 



Forks near D. Agin's, 1480' 



Cross roads near S. Knapp's, 1485' 



Forks near E. Corbin's, 1290' 



Level of Carly brook near J. Riefler's, 1200' 



Forks south of T. Galvin's, 1235' 



Forks next south, one half mile, 1270' 



38. Berlin, in Wayne county. 



This township lies southeast from Oregon, having it and 

 Damascus for its northern boundary, Pike county on its 

 southeast line, while its extreme eastern point rests on the 

 Delaware river opposite the village of Narrowsburg, N. Y. 



The drainage of the district is quite complicated, the water 

 form the western portion going into the Lackawaxen ; that 

 from the central and southeastern portions passing off 

 through Pike county into the Delaware ; while that from 

 the northeastern corner goes eastward to the river through 

 Corkin's creek. 



The rocks of the township belong exclusively to the Cats- 

 Tcill system, the top of the Chemung being buried under 

 several hundred feet of overlying red and gray rocks even 

 at the deepest water-way on the Delaware river. 



The massive Catskill cliff sandstones crop out in bold 

 bluffs at many localities within the township. 



