Stone.] 440 [March 3, 
IV. Musquash Stream System. 
This extends about seventeen miles, from near Musquash Lake in 
Topsfield, to Big Lake, and perhaps beyond. If it ends at Big 
Lake, it is one of the very few kames of its length, which do not 
end at the south in “ plains.” 
V. Grand Lake— Old Stream System. 
Grand Lake is a beautiful body of water bordered by high ranges 
and peaks, being situated in the heart of the Mt. Desert Highlands. 
It is often called Western or Schoodic Grand Lake, to distinguish it 
from the Eastern Grand Lake, situate on the upper St. Croix. A 
kame comes down the eastern arm of the lake to the outlet, thence 
southerly to the valley of Little River, thence down the valley of 
Old Stream, for much of the way as. kame-plains. Length, about 
25 miles. 
Va. Farm Cove Kame. 
Length about eight miles from Farm Cove on Grand Lake, south- 
ward through a low pass to join the main kame in the valley of 
Little River. 
Vb. Length about sixteen miles along Chain Lake Stream, and 
Clifford Stream, and perhaps northward to Big Lake. 
Notsz. Probably systems IV and V are one system, but thus far I 
cannot prove the connection. Much of this wilderness is swampy 
and very difficult to explore. 
VI. Baskahegan Lake — Machias River System. 
Length about forty-seven miles, from near the north-west angle of 
Baskahegan Lake, through a low pass in Kossuth, thence through 
Pleasant, Scragely and Junior Lakes, and then along the west sides of 
Grand and Pocumpus Lakes. It then expands into plains reaching 
toward Waubausoos Lake, also to Machias 3d Lake, and thence 
along the Machias River to near the Calais-Bangor air-line road. 
An extensive system, measured by the amount of sand and gravel 
it contains, and of very gentle slope. 
VIxandy. Bancroft and Hot Brook Kames. 
A kame crosses the E. and N. A. Railway, about one mile west of 
Bancroft Station, northern connections unknown. Southward prob- 
ably connects via Hawkins Brook with a kame found for about five 
miles along Hot Brook, and which may connect with VI. A large 
sand and gravel plain found near upper Hot Brook Lake, may have 
been formed by either a stream running south from Bancroft, or 
northward along Hot Brook. The only point of special interest is 
that here a kame-stream may possibly have flowed northward. 
