the head of Spider River; thence it bends to the northwest until it
approaches within about 4 miles of Lake Megantic; thence it turns again
south, having the valley of Arnolds River on the right and of Dead River
on the left. It leaves Gasford Mountain in Canada, threads its way over
very high ground between the head of Arnolds River and the tributaries
of the Magalloway; inclines then to the north, so to the west, over very
rocky, mountainous, and difficult country, leaving Gipps Peak in the
United States, and turns by a sharp angle at Saddle Back to the south.
After that it again inclines to the west, and then to the south, and
again to the west, and passes the head of the Connecticut. About 3 miles
and a half east of the head of the Connecticut there is a division of
waters similar to that described near Leech Lake. The boundary runs down
a stream from near its source to the fork where it divides, and then
again follows the dividing ridge. The spot is noted on the map.

After the boundary has passed the head of the Connecticut it runs to the
northwest, descending into very low, swampy ground between the heads of
Indian Stream and the tributaries of the St. Francis. Thus it passes on,
bending again to the south of west, over a high hill, to the source of
Halls Stream.

Iron monuments have been erected at intervals along the highlands from
the source of the Southwest Branch of the St. John to the source of
Halls Stream, the position of each of which is shown upon the maps.

From the source of Halls Stream the boundary descends that river,
dividing the islands, which are, however, merely unimportant alluvial
deposits, in the manner indicated by the maps until it reaches the
intersection of that stream by the line formerly run by Valentine and
Collins as the forty-fifth degree of north latitude.