sufficient to carry with it destruction to any of the labors of man. The spot on the mountain, from which the slip was loosened, is now a naked, white rock; and its pathway downward is indicated by deep channels, or furrows grooved in the side of the mountain, and down one of which pours a stream of water, sufficient to carry a common saw-mill. ‘From this place to the Notch, there is almost a continual ascent, generally gradual, but sometimes steep and sudden. The narrow pathway proceeds along the stream, sometimes crossing it, and shifting from the side of one mountain to the other, as either furnishes a less precarious foothold for the traveller than its fellow. Occasionally it winds up the side of the steep to such a height, as to leave, on one hand or the other, a gulf of unseen depth; for the foliage of the trees and shrubs is impervious to the sight. The Notch itself is formed by a sudden projection of rock from the mountain on the right or northerly side, rising perpendicularly to a great height,――probably seventy or eighty feet,――and by a large mass of rock on the left side, which has tumbled from its ancient location, and taken a position within _twenty feet_ of its opposite neighbor. The length of the Notch is not more than three or four rods. The moment it is passed, the mountains seem to have vanished. A level meadow, overgrown with long grass and wild flowers, and spotted with tufts of shrubbery, spreads itself before the astonished eye, on the left, and a swamp or thicket, on the right, conceals the ridge of mountains which extend to the north: the road separates this thicket from the meadow. Not far from the Notch, on the right hand side of the road, several springs issue from the rocks that compose the base of the mountain, unite in the thicket, and form the Saco river. This little stream runs across the road into the meadow, where it almost loses itself in its meandering among the bogs, but again collects its waters and passes under the rock that makes the southerly wall of the Notch. It is here invisible for several rods, and its presence is indicated only by its noise, as it rolls through its rugged tunnel. In wet seasons and freshets, probably a portion of the water passes over the fragments of rock, which are here wedged together, and form an arch or covering for the natural bed of the stream.