But it is time to proceed on our down-river trip. So, leaving the outlet of Grand Lake, and passing south about two miles across a "carrying-place," we strike the head of another lake, called _Che-pet-na-cook_, into which the surplus waters of the former lake pass. The name by which this lake is designated is said to signify _hilly pond_ or _lake_. In form it is long and narrow, resembling a deep, massive river. That peculiarity from which its name is derived is strikingly prominent. A range of abrupt and elevated ridges rises suddenly from its western shore, covered with a close, heavy growth of trees, principally Spruce. One peak of the ridge rises several hundred feet from the surface of the lake, which is called "_Spruce Mountain_." After mid-day, a section of this mountain ridge, so dense and frowning as to resemble a thunder-cloud, casts a cavernous shade, like a misty pall, over the surface of its waters, which seem to lay with prostrate fear at its base, imparting an oppressive solemnity over the scenery.
At the foot of this lake, which is between twenty and thirty miles long, the east branch of the St. Croix takes its rise. From this point it passes through a rocky channel for the most part, occasionally flowing through a section of meadow or intervale land until it reaches Baring, a distance of some fifty miles, where for the first time it meets with a formidable barrier to its hitherto wild and unrestrained progress in the character of a "_dam_." Passing this through its various avenues, it flows on to Milltown, which occupies both sides of the river, and includes both the English and American villages. Between this place and the head of ship navigation, some two miles distant, the channel is _dammed_ several times on a succession of falls, where are numerous saw-mills; and, finally, after having leaped a thousand rocky precipices above, and struggled through as many gates and sluice-ways below, it quietly flows on to the Passamaquoddy Bay, where its restless waters find repose in the bosom of the Atlantic Ocean.
In regard to the lumbering resources on this river, I believe it is generally admitted that the supply of Pine is comparatively small, the principal part having already been brought to market; and although the territory belonging to this river is large, still its resources are curtailed by the proximity of the head waters of the St. John, Penobscot, and Machias Rivers.