Ice in a Hole at Dixville Notch, New Hampshire.—Mr. John Ritchie, Jr., of Boston, has examined this place, which he is sure is a refrigerator. It is in a hole north of the cliff and near its top.
Ice on Mount Garfield, New Hampshire.—Mr. John Ritchie, Jr., informs me that ice was discovered among the boulders on the summit of Mount Garfield during the summer of 1897.
Freezing Talus near Rumney, New Hampshire.—Described in Part I., [page 85].
Freezing Talus near North Woodstock, New Hampshire.—Mr. John Ritchie, Jr., has examined this locality. He thinks the ice was gone in July, but judges it to be on the level of an old talus and a couple of meters down.
Freezing Well at Lyman, Grafton County, New Hampshire. (Geology of Vermont, 1861, I., page 197.)—A well in that town is reported as having been frozen solid in June, 1816, at a depth of about 2.60 meters from the surface.
Icy Wells at the Foot of Mount Mansfield, Vermont. (N. M. Lowe, Science Observer, vol. II., page 58.)—These are described as being really “incipient caves.”
Freezing Cave near Manchester, Vermont.—Described in Part I., [page 76].
Ice Bed of Wallingford, Rutland County, Vermont. Described in Part I., [page 99]. (S. Pearl Lathrop, American Journal of Science and Arts, 1844, XLVI., page 331.)—Dr. Lathrop says that ice has been found at the Ice Bed as late as September.
Freezing Wells at Brandon, Vermont. Described in Part I., [page 77]. (Geology of Vermont, 1861, vol. I., page 192.)—Mr. Hager says that the well was dug into a mass of sand and gravel, of the kind known as modified drift. The gravel was frozen at the time of digging. The Boston Natural History Society, in 1859, sank two wells, one 21 meters southeast of the original one, the other 21 meters northwest. The first was 10 meters in depth and did not reach ice; the second was 11 meters in depth, and came to the layer of frozen gravel.