HYDROLOGY OF NEW YORK 



259 



1901, the remaining canal, with the exception of that from High 

 Falls feeder to Rondiout. was abandoned. 



Above its junction with Sandberg creek, at Xapanoch, Kondout 

 creek is a mountain stream. At Honk falls a natural declivity 

 affords a fall of 125 feet over tilted strata of Hudson river shale. 

 There is a dam at the head of this fall of 22% feet, making the 

 total head 14 7 % feet. 



Water power of Rondoui creek. The following is a list of the 

 principal developed water powers on Rondout creek in 1901 : 



(1) 



o 

 6 

 7 

 8 

 9 

 10 

 It 

 12 

 13 

 14 



15 

 16 

 17 

 18 

 19 



Locution 



(3 



Name of mill and of owner and 

 operator 



(3) 



Eddyville 



Lavrrenoeville . . 

 Below High Falls 



High Falls 



High Falls 



Port Hickson 



Napanoch 



Napanoch 



Napanoch, R. H. 

 Xapanoch. L. H. 



Napanoch 



Napanoch, L. H. 

 Napanoch, L. H. 

 Napanoch. R. H. 



Napanoch, L. H. 



Napanoch 



Lackawack 



Grahaniville 

 Bull River 



D. & H. Canal Co 



Lawrenceville Cement Co. . . . 

 W. I. Vandermark. J. H. Van- 



dermark estate 



Hasbrook & Hopper, Ulster 



County Savings Banks 



D. & H. Canal 



E. C. Shook & Son 



M. M. Pillsbury 



Humphrey & Young 



J. C. & S. E. D. Hornbeck . 



Pittsburg Ax Factory 



Napanoch Knife Co 



Young & Humphrey, John 



Russell estate 



M. M. Pillsbury Paper Mill . . . 



Honk Falls Power Co 



C. N. Morse 



^ si 



(4) 



10 



12 

 31 

 10 

 6 



30 

 30 



SS 



C d 

 o a> 



ae O c3 



(5) 



None 

 80 



""60 

 ' '481 



15| 



12 



•56 

 147* 

 10 



593 

 1,500 

 140 



50-100 



Wallkilt river. Wallkill river is the chief tributary of Rondiout 

 creek. It has its source on Sparta mountain, New Jersey, about 

 twenty-one miles from the point where it enters New York State. 

 From its source to the head of the Drowned Lands it is essen- 

 tially a highland stream. 



