GLACIAL DRIFT IN NEW ENGLAND. 447 



little broken, is not surprising ; I have, how- 

 ever, seen very distinct ones in some valleys 

 of the White Mountains and in Vermont. 

 Up to this time there had been nothing very 

 new in the aspect of the phenomena as a 

 whole ; but on examining attentively the in- 

 ternal arrangement of all these materials, es- 



O ' 



pecially in the neighborhood of the sea, one 

 soon becomes convinced that the ocean has 

 partially covered and more or less remodeled 

 them. In certain places there are patches of 

 stratified sand interposed between masses of 

 glacial drift-deposit ; elsewhere, banks of sand 

 and pebbles crown the irregularities of the 

 glacial deposit, or fill in its depressions; in 

 other localities the glacial pebbles may be 

 washed and completely cleared of mud, re- 

 taining, however, their markings ; or again, 

 these markings may have disappeared, and 

 the material is arranged in lines or ramparts, 

 as it were, of diverse conformation, in which 

 Mr. Desor recognized all the modifications of 



o 



the " oesars ' of Scandinavia. The disposi- 

 tion of the cesars, as seen here, is evidently 

 due entirely to the action of the waves, and 

 their frequency along the coast is a proof of 

 this. In a late excursion with Captain Davis 

 on board a government vessel I learned to 



