Wright. 9 Ae [April 2, 
No. HI, the next series westward, is less perfectly made out: But 
a long kame is described in the State Geological Report in the Seboois 
Lake region, on the head of the East Branch of-the Penobscot. A 
system is reported from Crystal, down the Molunkus river, crossing 
the Mattawamkeag in Kingman, it passes through Webster to Spring- 
field. Farther south they are reported, west of Sisladobsis Lake, 
and in the upper valley of the Machias River, in. townships Nos. 43, 
37 and 31. 120 miles. 
No. IV. About ten miles farther west, kames appear from Stacy- 
ville south, down the Salmon River, at the mouth of the Mattakeunk, 
across from Mattawamkeag, and up the stream to Lee, and still far- 
ther south in township No. 3, and along the whole line of Nickatouas 
Lake, to the headwaters of the Narraguagus, still farther south to 
Beddington and the great Deblois plains. 90 miles. The connection 
between the segments of these last two series is not every where 
demonstrated. 
No. V begins south-east of Mt. Katahdin, crosses Millinoket 
Lake obliquely, near its foot, runs down the west branch of the 
Penobscot, near the foot of Grand Falls; crosses the valley of 
the Nollesemick, thence through a low pass down the Madunkeunk, 
and through Chester to Hockamock Island, where it crosses the 
Penobscot. Thence it goes south and east, through Enfield, Passa- 
dunkeag, Greenbush, Greenfield, No. 32, Aurora (here known as the 
Whale’s Back), and so on through No. 22, to the great Deblois- 
Cherryfield-Columbia plains, 120 miles. Series Nos. IV and V join 
in the Deblois plains. 
No. VI is reported from the Twin Lakes, on the west branch of 
the Penobscot, about ten miles west from the Katahdin series. It 
crosses a low divide into the valley of the Seboois stream, runs east 
of Endless Pond, southward through Maxfield, Howland, Edinburg 
and Argyle, where it crosses the Penobscot at Olaman Island, thence 
south-easterly to Greenfield, where it is said to join the main Katah- 
din series. 
No. VII is reported as beginning near Lake Seboois in the east 
part of Piscataquis Co., and running south through Medford, La 
Grange, Alton, Old Town, Orono and Veazie. It is quite obscured 
for two or three miles above Bangor, but shows plainly below as a 
series of high ridges as far as Hampden Upper Corner. High Head, 
a little below Bangor, is a part of this system. ‘This series is but a 
few miles from the preceding, and very closely parallel. It makes a 
