46 ICE RECESSION IN NEW ENGLAND 



Localities in the Hudson Valley 



On account of a gap, comprising varves 5601 to 5712, in the 

 normal curve in southernmost Vermont and New Hampshire. 

 the corresponding zone has been taken from measurements made 

 by the writer, in 1921, in the Hudson Valley. Since the ice 

 recession in the Hudson Valley is to be treated by Baron De 

 Geer, only the necessary series has been made use of; and only 

 the position of the localities will be given (ci. PL VI). 



a. — Catskill, N. Y., brickyard K mile SE of the railroad station. 

 b. — Catskill, brickyard a few hundred yards E of the railroad 



station. 

 c. — Hudson, N. Y.. brickyard a mile NE of the railroad station, 

 d. — 5>2 miles N of Hudson, brickyard on the railroad i}4 mile 



N of Stockport. 

 e. — Coxsackie, N. Y.. old brickyard on the Hudson % mile NNW 



of the ferry, 

 f. — 11} 2 miles S of Albany, N. Y., the southernmost brickyard 



on the Hudson, y 2 mile N of Coeymans. 

 g. — Albany, brickyard on Van Woert Street, 

 h. — Cohoes, N. Y.. brickyard on the Mohawk River at the 



northwestern edge of the city. 

 i. — 3 miles NNW of Cohoes (railroad station), old brickyard 



on the Mohawk River $i mile N of Crescent station. 

 ].- — 4 miles NW of Cohoes, brickyard W of the Mohawk River 



i>4 miles NW of Crescent station. 



