1880.] 439 [Stone. 
the stream ran southward through Dennysville and Edmunds, and 
crossed Trescott to the sea. 
Length of system about 150 miles. 
I1a. New Limerick—Amity Kame. 
Length about twenty miles from near the centre of the town of 
New Limerick, in nearly a straight general course to join the main 
kame near the south line of Amity. In Linneus is a prominent 
ridge, very meandering by short zigzags. 
IIb. Weston Kame. 
A local kame running for two or three miles to join the main 
kame in Grand Lake. 
IIc. Island Falls—Danforth Kame. 
Extends from near the north-east corner of Hersey through 
Tsland Falls to Haynesville. It here leaves the valley of the Matta- 
wamkeag and crosses a low col, keeping for part of the way along 
the side of a hill, and about half way up the slope. It continues 
nearly south till within three miles of Danforth, when it turns south- 
eastward by a beautiful curve whose chord is about one mile in 
length, and thence points straight toward the Danforth pass. South 
of Danforth there were two passes, the more favorable one leading 
directly south to Baskahegan Lake; but the kame took a higher and 
narrower pass south-eastward along the line of the E. and N. A. R., 
and joins the main kame a short distance south of Tomah Station. 
At Danforth and northward the kame consists of fine gravel, while 
at Forest Station near the col it is almost wholly of pebbles. East of 
Forest it disappears for about three miles on a down slope of thirty 
feet per mile. Length 55 miles. 
Id. Little Tomah Stream Gravels. 
Length about six miles from Little Tomah Lake to Tomah Stream. 
Partly of kame origin. 
Ill. East Machias System. 
Not personally explored. A series of gravel ridges running for 
near four miles northward from East Machias and nearly parallel to 
the road to Cooper. 
IiIm. Crawford Kame. 
A kame about one mile long is found near where the Air Line 
road from Calais to Bangor crosses the East Machias River. Prob- 
ably a kame-stream ran down this valley, but if so its gravels have 
been disguised by the sea in the Champlain period. 
