350 J. D. Dona—Glacial Phenomena 
According to my observations in Connecticut, the direction 
in = set ee is 8. 14°-25° E., and near Lane’s Mine 
in onroe, 8. 12°-13° E., places within 12 miles of the New 
Hay i destin 7 in ihe towns of Norfolk, eae and Kent, 
farther west, S. 18°-20° E.; of Warren, S, 30° E.; of Newtown, 
32° K., and 2 is farther west, 8. 41° E: of Sharon, S. 33°~ 
36° E.; of Cornwall, S. 33°-36° E.; and on Mt. Washington and 
its highest summit, Mt. eg . en On Massachusetts 
(the latter, 2,634 feet high), S. °. The direction in 
ence accordin ng to Mr. H. Nae is S. 23° E. and S. 38° E.; 
n No rfolk, according to Mather, S. 20°-25° E.; and on Mt, Ton, 
in southwestern Lite hfield, according to E. Hitchcock, 8. 17°- 
22° EK, Other facts of similar import from eastern New York, 
Massachusetts, Vermont and New Hampshire, are given in Ach 
iii, pp. 177-195), are of tater publication. 
Mt. Adams, W. side, height 5,500 Seb gs Bo ag §. 58° E. 
Between Adams and Jefferson, near gap (4,939 ft.) §, 33° E. 
Top of Mt. Washington (6,293 ft.), smoothing and faint markings 
sai 5,800-6,000 feet, transported stones, p. 204), but striz ob- 
§. 43° E. 
“200 bar ncn Lake of the Clouds 8. i E. 
Lake of the Clouds (5,000 ft.), the intersecting directions { : oi > 
Between Mt. Pleasant and Mt. Franklin (4,400 ft.) 8. 30° E. 
Between Mt. Pleasant and Mt. Clinton (4,050 ft.) §. 30° E. 
Near top of Mt. TB (4,320 ft.), N. side §. 47°-52° E. 
Mt. Clinton, S. pe uuege. §. 50° EB. 
South end of me “pe ter 7 ae 
Top of Mt. Webster (4,000 ft.) 8. 30° E. 
Top of Mt. Moosilauke (4,811 ft.) §. 22° E. 
The abrasion observations thus far made appear to show 
that bee mean direction of glacier flow in western Connecticut 
and Massachusetts was somewhere between S. rei BE. and 5. 
38° E., and probably between §S. 12° E. and S. 25° E. 
b. The evidence from bowlders outside of the athens valley 
is of the same import. 
Percival states that transportation over Litchfield was 
.S.E., as indicated by the distribution of limestone blocks 
from Canaan—which means about S. 20°-25° BE. A few of 
these Canaan limestone bowlders I have found lying now in 
Orange, within four miles of the New Haven region, indicating 
transportation for 48 to 50 miles in the direction S. 16° E. 
They are easily recognized by the tremolite and canaanite 
Nomegibi white pyre see) they contain. Bowlders of quartzyte, 
same region, or from Berkshire, just north, are widely 
Sasibcek Bowlders of porphyritic gneiss from the north- 
