34 ICE RECESSION IN NEW ENGLAND 



81. — 3% miles N of Woodsville, }i mile S of East Ryegate 

 station and locality 82, ravine E of the Connecticut 

 River, between the river and the road. 



7 feet sand. 



6 feet clay, partly disturbed. 



High section of good varve clay; only a part measured. 



Series measured: 7147-7198. 



82. — 4 miles N of Woodsville, bluff on the eastern side of the 

 Connecticut River, directly opposite East Ryegate 

 station. 



Plain of sedimentation. 



2 feet gravel. 



Somewhat silty clay with good lamination, varves 7200-7328. 



Fat blue clay with very distinct lamination, varves 6999-7199. 



50 feet talus down to river level. 



Depth to substratum unknown. 



Series measured: 6999-7328. 



83. — 600 yards N of locality 82, bluff on the western side of the 

 river. 



The clay is covered by 20 feet of sand. It contains many 

 deformed zones. It continues to unknown depth below the 

 river. 



Series measured: (7213-7277, 7260-7321, 7307-7321, 

 7323-7354). 



84. — The junction of the Connecticut and Passumpsic Rivers, 

 on the easternmost channel of the Connecticut, 300 yards 

 upstream from its junction with the main river. 



10 feet sand, gravel, and cobbles. 

 25 feet varve clay, not measured. 

 Exceedingly fat clay, varves 7247-7338. Varve limits often 



difficult to distinguish. 

 The clay continues below river level. 



Series measured: (7247-7338). 



