GLACIAL DRIFT. 201 
due to other causes than the mere influence of the two mountains, so that 
we cannot strongly insist that the easterly movement of the stria from 
Hill to Warner is entirely due to the presence of the two mountains. 
The only feature where this case is unlike Monadnock, is the easting at 
the base of the mountain, which we see may have been produced by an 
independent movement. 
Other Mountains similarly Striated. Of other mountains similarly 
situated, some exhibit the same kind of ice-action. Mt. Gunstock has 
S. 62° E. strize on top, and the S. 32°-35° E. course on the east side, bor- 
dering Lake Winnipiseogee. Mt. Lovell in Washington shows the direc- 
tion S. 36° E. on the summit, while it is commonly S., 21° E. in the north 
part of the town, though crossed by a set running S. 41° E. Lempster 
mountain summit shows the direction S. 41° E., and it is S. 21° E. on the 
west side. On Mt. Cuba we find S. 28° E. and S. 37” E,, while it is com- 
monly west of south in Orford on the west, and S, 22° E. in Wentworth. 
Moose mountain in Hanover shows S. 38° E. on its summit, while the 
course is south on the western side, and S. 19° E. on the Enfield side. 
There is a south-east course in the middle and south-east part of Hano- 
ver, which may have some connection with these movements on the ele- 
vated summits. Sunapee mountain would be expected to agree with its 
neighbors, but no observations of striz have been made there. Mt. As- 
cutney, just out of the state, exhibits phenomena worthy of mention here. 
This has the same altitude with Mt. Monadnock, while the land about it 
is more uneven, averaging less than around the Cheshire peak. Owing 
to the rapid disintegration of the rock, strize are scarce, and perhaps the 
few examples discovered should not be taken as truthfully representing 
the general courses. The very summit showed a due south course. About 
300 feet lower down, on the north-east side of the mountain, following 
the Windsor path, are striz running due east, or N. 80° E. They rest 
upon a wall inclined 70° N., and point down the mountain towards the 
south part of Cornish. Others in the neighborhood run S. 20° W. About 
two thirds of the way down are other distinct strie running S. 10° E,; 
and no others were seen on the mountain proper. On reaching the dam 
over Mill brook, west of Windsor village, the course S. 30° E. is seen, 
and a few N. 70° E., a very unusual direction, supposed to have been 
the result of some local disturbance. In Weathersfield and Claremont, 
