The Ice Bed of Wallingford is situated about three kilometers to the east of Wallingford, Vermont. A drive of half an hour, over the Mount Holly and Hearburrow roads, takes the visitor to the entrance of a rough wood path, which, at a distance of three or four hundred meters, leads to the Ice Bed. This is a huge talus, at the base of the White Rock Mountain, whose cliffs rise steeply overhead for some three or four hundred meters. The talus, which was doubtless formed by a great slide at some distant date, consists of granite boulders, some of which are big ones. The ice-bearing portion may be some thirty or forty meters high vertically. It lies in a sort of gully or rock basin, and at the top is about thirty meters broad, tapering to a point at the bottom. The talus faces southward, and during a good part of the day the sun shines full upon it. A thin forest fringes the sides and grows round the bottom, but this can afford but little protection from the winds, especially to those from the south. I visited this place on the 5th of October, 1899. There was a distinct drop in temperature as we neared the base of the talus, and a cool air drew gently down over the rocks. I think slight draughts issued from some of the crevices; but of this I am not sure. The temperature was sub-normal, about 8°, but hardly low enough to prove the presence of ice, although we could see our breaths distinctly. We looked carefully under a number of the boulders, but neither ice nor snow was visible. I was assured that ice was abundant there in the past July and August, and I should think it had melted away only shortly before my visit. My impression is, that this is a periodic glacière. CAVES NEAR WILLIAMSTOWN. On the eastern slope of the Petersburgh Mountain of the Taghconic Range in Massachusetts, at a good deal lower altitude than the Williamstown Snow Hole and about southeast of it are some caverns, which are but little known. A five or six kilometer drive from Williamstown takes the visitor to the base of the mountain, whence a rather steep ascent of about a kilometer and a half brings him to the caves, which are in the midst of a dense, scrub forest. The caves were first entered, and possibly discovered, by Mr. W. F. Williams, of Williamstown, when a boy. Since then, he has visited them many times and explored them a good deal. They do not appear to have any name as yet, and it would seem only fitting to christen them after their explorer: the Williams Caves.