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NEW YORK STATE MUSEUM 



At Danskammer the stream is about 3500 feet wide. The resuhs 

 of wash borings gave a range in depths from 133.2 feet to 268.5 

 feet to supposed rock bottom, but the evident irregularity and 

 variabiHty would seem to indfcate a bed of loose material at these 

 depths at this crossing. 



At the Storm King crossing the drill brought up from a depth of 

 617.4 feet a core of granite just like that on the east bank of the 

 river, which it had penetrated to a distance of 8.8 feet. The drill 

 was thought to have reached rock bottom at this point at a depth 

 of 608.6 feet not far from 750 feet from the east bank. 



Casper creek was tested near its mouth by wash borings. The 

 lowest point thus reached was dj feet below tide. 



The Casper creek crossing. (After Kemp) 



In Wappinger creek one wash boring below the falls reached a 

 depth of 50 feet below tide. Of three core borings, the maximum 

 was 39 feet. 



Fig. 29 The Wappinger creek crossing. (After Kemp) 



A proposed line of the aqueduct crossed Fishkill creek near the 

 village of Fishkill. Everything is beneath the drift at this point. 

 Of two core holes, the deeper reached the limestone at 40 feet below 

 tide. After penetrating 8 feet of limestone, the drill encountered 

 fine yellow sand in which it continued for 60 feet, when the hole 

 was abandoned. This crossing is about five miles back from the 

 Hudson. 



FISHKILL CRECK 



Fig. 30 The Fishkill creek crossing. (After Kemp) 



