Butson Ridge
Encyclopedia
Butson Ridge is a rocky ridge with a number of ice-covered summits, the highest at 1305 metre, forming the north wall of Northeast Glacier
Northeast Glacier
Northeast Glacier is a steep, heavily crevassed glacier, 13 miles long and 5 miles wide at its mouth, which flows from McLeod Hill westward and then southwestwards into Marguerite Bay between the Debenham Islands and Roman Four Promontory, on the west coast of Graham Land...

 on the west coast of Graham Land
Graham Land
Graham Land is that portion of the Antarctic Peninsula which lies north of a line joining Cape Jeremy and Cape Agassiz. This description of Graham Land is consistent with the 1964 agreement between the British Antarctic Place-names Committee and the US Advisory Committee on Antarctic Names, in...

. It was first surveyed in 1936 by the British Graham Land Expedition
British Graham Land Expedition
A British expedition to Graham Land led by John Lachlan Cope took place between 1920 and 1922. The British Graham Land Expedition was a geophysical and exploration expedition to Graham Land in Antarctica between 1934 to 1937. Under the leadership of John Riddoch Rymill, the expedition spent two...

 under Rymill. It was resurveyed in 1946–48 by the Falkland Islands Dependencies Survey (FIDS) and named for Dr. Arthur R.C. Butson, FIDS medical officer at Stonington Island
Stonington Island
Stonington Island is a rocky island lying 1 mile northeast of Neny Island in the eastern part of Marguerite Bay, off the west coast of Graham Land. Stonington Island is located at . Stonington Island, 0.4 miles long from northwest to southeast and 0.2 miles wide formerly connected by a drifted snow...

, who in July 1947 rescued a member of the Ronne Antarctic Research Expedition
Ronne Antarctic Research Expedition
The Ronne Antarctic Research Expedition was an expedition from 1947-1948 which researched the area surrounding the head of the Weddell Sea in Antarctica.-Background:...

 from a crevasse
Crevasse
A crevasse is a deep crack in an ice sheet rhys glacier . Crevasses form as a result of the movement and resulting stress associated with the sheer stress generated when two semi-rigid pieces above a plastic substrate have different rates of movement...

in Northeast Glacier.
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