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Murray Glacier: Antarctica
SOURCE: National Geospatial-Intelligence Agency, Bethesda, MD, USA
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This page presents the geographical name data for Murray Glacier in Antarctica, as supplied by the US military intelligence in electronic format, including the geographic coordinates and place name in various forms, latin, roman and native characters, and its location in its respective country's administrative division.

Feature Name (see definition): Murray Glacier

Feature Class (see definition): Glacier

Country Code (see definition): AQ (Antarctica)

Feature ID (see definition): 10421

Primary Latitude in degrees, minutes, and seconds (see definition):
71° 39' 00" S

Primary Longitude in degrees, minutes, and seconds (see definition):
170° 00' 00" E

Primary Latitude in decimal degrees (see definition): -71.65

Primary Longitude in decimal degrees (see definition): 170

Elevation (see definition): No data

Decision Year (see definition): No data

Description (see definition): Valley glacier, 20 mi long, draining seaward along the E side of Geikie Ridge in the Admiralty Mountains. Its terminus coalesces with that of Dugdale Glacier where both glaciers discharge into Robertson Bay along the N coast of Victoria Land. First charted by the British Antarctic Expedition (BrAE), 1898-1900, under C.E. Borchgrevink, who named this feature for Sir John Murray of the Challenger expedition, 1872-76.

Date Created (see definition): No data

Date Edited (see definition): No data



NOTE: The information regarding Murray Glacier in Antarctica on this page is published from the data supplied by the National Geospatial-Intelligence Agency, a member of the Intelligence community of the Antarctica, and a Department of Defense (DoD) Combat Support Agency. No claims are made regarding the accuracy of information contained here. All suggestions for corrections of any errors about Murray Glacier should be addressed to the National Geospatial-Intelligence Agency.


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https://geographic.org/geographic_names/antname.php?uni=10421&fid=antgeo_116

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