Bailey Ice Stream () is an

ice stream An ice stream is a region of fast-moving ice within an ice sheet. It is a type of glacier, a body of ice that moves under its own weight. They can move upwards of a year, and can be up to in width, and hundreds of kilometers in length. They t ...

on the northern margin of the

Theron Mountains The Theron Mountains () are a group of mountains, extending in a NE-SW direction for and rising , on the eastern side of the Filchner Ice Shelf. They were first seen from the air in 1956 by the Commonwealth Trans-Antarctic Expedition The Co ...

, flowing west-southwest to the

Filchner Ice Shelf Wilhelm Filchner (13 September 1877 – 7 May 1957) was a German army officer, scientist and explorer. He conducted several surveys and scientific investigations in China, Tibet and surrounding regions, and led the Second German Antarctic Expediti ...

. It was named by the

UK Antarctic Place-Names Committee The UK Antarctic Place-Names Committee (or UK-APC) is a United Kingdom government committee, part of the Foreign and Commonwealth Office, responsible for recommending names of geographical locations within the British Antarctic Territory (BAT) an ...

after

Jeremy Thomas Bailey Jeremy may refer to: * Jeremy (given name), an English male given name * Jérémy, a French given name * ''Jeremy'' (film), a 1973 film * "Jeremy" (song), a 1992 song by Pearl Jam * Jeremy (snail), a left-coiled garden snail that died in 2017 * ...

(1941–65), a

British Antarctic Survey The British Antarctic Survey (BAS) is the United Kingdom's national polar research institute. It has a dual purpose, to conduct polar science, enabling better understanding of list of global issues, global issues, and to provide an active prese ...

glaciologist Glaciology (; ) is the scientific study of glaciers, or, more generally, ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science that integrates geophysics, geology, physical geography, geomorphology, clim ...

, who with two companions died in a

crevasse A crevasse is a deep crack that forms in a glacier or ice sheet. Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pieces above a plastic substrate have different rate ...

accident during a radio echo sounding traverse inland from Halley Station on 12 October 1965. On an earlier traverse in April 1965, Bailey sounded the upper portion of this feature.Bailey Ice Stream
/ref>

References

* Ice streams of Antarctica Bodies of ice of Coats Land Filchner-Ronne Ice Shelf {{CoatsLand-geo-stub

See also

References