|Длина||53 км (33 миль) км|
Barnard Glacier is a 53 км (33 миль) long glacier in the U.S. state of Alaska. It trends southwest to the Chitina River east of Hawkins Glacier, 64 км (40 миль) southeast of McCarthy in the Saint Elias Mountains. The glacier is named for Barnard College, a member of the Seven Sisters that is associated with Columbia University in New York, New York.
Barnard Glacier is a clean, crevassed ice tongue, with no medial or lateral moraines. It heads in a large cirque and connects with an irregular ice mass on a shelf to the nor glacier which has small terminal lobes and terminates on the lip of its hanging valley. Two streams descend from the terminus. Mature spruce forest extending from the fiord well up toward the glacier terminus indicates that Barnard Glacier has not descended much farther toward the fiord for a century or more; but a barren zone between the ice and forest, present in 1899 as well as in 1910, proves that it was retreating. Between 1899 and 1910 there was an advance of the south lobe down the lip of the hanging valley, and a slight advance of the north lobe, while between the two lobes an ice block talus was formed.
- Geoobject (№ 1398617) // U.S. Geological Survey Geographic Names Information System // geonames.usgs.gov. — Advisory Committee on Antarctic Names. U.S. Board on Geographic Names.
- Tarr, Ralph Stockman. Alaskan glacier studies of the National Geographic Society in the Yakutat Bay, Prince William Sound and lower Copper River regions / Ralph Stockman Tarr, Lawrence Martin, National Geographic Society (U.S.). — The National Geographic Society, 1914. — P. 306–.