EXPLANATION OF MAP 105 



1907, 1916), A. P. Brigham (1895), R. S. Tarr (1909), J- M. Clarke 

 (1911), W. J. Miller (1909, 1910, 1914, 1916), H. L. Fairchild (1907). 

 J. B. Woodworth (1901, 1905), J. L. Rich (1906, 1914, 1915). C. E. Gor- 

 don (1911). J- H. Stoller (1911. 1916), H. J. Ailing (1916), R. D. Salisbury 

 and others (1902). 



In New Jersey: R. D. Salisbury and others (1902, PI. 8; and 1908), 

 J. V. Lewis and H. B. Kiimmel (1915). 



In Pennsylvania: H. C. Lewis (1884). 



Because of lack of detailed information it generally has not 

 been possible to discriminate between striae made at different 

 stages of ice recession; hence, in compiling lines of flow, a con- 

 servative attitude has been kept toward the delineation of 

 minor lobes. In the Connecticut, Hudson, and Catskill regions 

 these seem to have been more strongly accentuated than the 

 map indicates, resembling perhaps the more thoroughly studied 

 lobe of the Finger Lakes region. The very wide spread of the 

 Mt. Ascutney boulder train is the best evidence of this. The 

 flow of the ice appears to have been due southward, however, 

 over the entire eastern uplands of Vermont, so that it is a mis- 

 take to regard the southward movement of ice down the Con- 

 necticut Valley as due in any sense to the presence of that 

 valley. 



Terminal moraines 



In Massachusetts: J. B. Woodworth (1897). 



In New York: J. B. Woodworth (1901), M. L. Fuller (1905, 1914). 

 In New Jersey and Pennsylvania: same references as under former 

 heading. 



Recessional moraines 



In Maine: F. J. Katz and A. Keith (191 7). 



In New Hampshire: J. W. Goldthwait (1916, and unpublished data). 



In Massachusetts and Rhode Island: J. B. Woodworth (1896, 1897), 

 F. B. Taylor (1903). W. O. Crosby (1899). 



In New York: T. C. Chamberlin (1883), F. Leverett (1915). R- S. 

 Tarr (1909). H. L. Fairchild (1907), A. P. Brigham (1898), J. L. Rich 

 (1906, 1914, 1915), F. B. Taylor (1913). C. E. Peet (1904), F. Carney 

 (1909). 



