Lord Glacier
Encyclopedia
Lord Glacier is a glacier
Glacier
A glacier is a large persistent body of ice that forms where the accumulation of snow exceeds its ablation over many years, often centuries. At least 0.1 km² in area and 50 m thick, but often much larger, a glacier slowly deforms and flows due to stresses induced by its weight...

 about 6 nautical miles (11 km) long draining from Coulter Heights
Coulter Heights
Coulter Heights are snow-covered heights that rise between Strauss Glacier and Frostman Glacier near the coast of Marie Byrd Land. The rock outcrops of Kuberry Rocks, Matikonis Peak and Lambert Nunatak protrude above the snow surface of the heights. The feature was mapped by the United States...

 to Hull Bay
Hull Bay
Hull Bay is an ice-filled bay, about 25 nautical miles wide, fed by Hull Glacier, which descends into it between Lynch Point and Cape Burks, on the coast of Marie Byrd Land. Discovered by the United States Antarctic Service , 1939-41. The bay derives its name from Hull Glacier, which is named for...

. Named by Advisory Committee on Antarctic Names
Advisory Committee on Antarctic Names
The Advisory Committee on Antarctic Names is an advisory committee of the United States Board on Geographic Names responsible for recommending names for features in Antarctica...

 (US-ACAN) after Neal E. Lord, geophysicist, University of Wisconsin, whose research focused on theoretical and field analysis of Ice Stream
Ice stream
An ice stream is a region of an ice sheet that moves significantly faster than the surrounding ice. Ice streams are a type of glacier. They are significant features of the Antarctic where they account for 10% of the volume of the ice...

 area of West Antarctica
West Antarctica
West Antarctica, or Lesser Antarctica, one of the two major regions of Antarctica, is the part of the continent that lies within the Western Hemisphere including the Antarctic Peninsula.-Location and description:...

from the late 1980s to the present.
The source of this article is wikipedia, the free encyclopedia.  The text of this article is licensed under the GFDL.
 
x
OK