Glen Glacier (80°44′S 25°16′W / 80.733°S 25.267°W / -80.733; -25.267) is a glacier at least 7 nautical miles (13 km) long, flowing south in the Shackleton...

Schimper Glacier, Gordon Glacier, Stratton Glacier and Blaiklock Glacier flow northwest from the range into the Slessor Glacier. The Glen Glacier and Cornwall...

Alexander R. Glen, member of the Committee of Management of the CTAE, 1955-58. 80°47′S 26°16′W / 80.783°S 26.267°W / -80.783; -26.267. A glacier 9 nautical...

highest being Holmes Summit at 1,875 metres (6,152 ft), lying east of Glen Glacier in the south-central part of the Shackleton Range. The Read Mountains...

Dawson-Lambton Glacier Glen Glacier Goldsmith Glacier Gordon Glacier Hayes Glacier Jeffries Glacier Lerchenfeld Glacier Penck Glacier Recovery Glacier Schimper...

833°W / -80.717; -25.833) are a group of nunataks between Cornwall Glacier and Glen Glacier, marking the western end of the Read Mountains in the Shackleton...

A glacier (US: /ˈɡleɪʃər/; UK: /ˈɡlæsiər, ˈɡleɪsiər/) is a persistent body of dense ice that is constantly moving downhill under its own weight. A glacier...

400-foot-deep (120 m) narrow gorge cut through rock by Glen Creek, a stream that was left hanging when glaciers of the Ice age deepened the Seneca valley, increasing...

theoretical glaciology and continuum mechanics, the Glen–Nye flow law, also referred to as Glen's flow law, is an empirically derived constitutive relation...

(genitive Comhain). The glen is U-shaped, formed by an ice age glacier, about 12.5 kilometres (7+3⁄4 mi) long with the floor of the glen being less than 700...