This page presents the geographical name data for
Martin 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):
Martin Glacier
Feature Class
(see definition):
Glacier
Country Code
(see definition): AQ (Antarctica)
Feature ID
(see definition):
9485
Primary Latitude in degrees, minutes, and seconds
(see definition):
68° 29' 00" S
Primary Longitude in degrees, minutes, and seconds
(see definition):
066° 53' 00" W
Primary Latitude in decimal degrees
(see definition):
-68.4833333
Primary Longitude in decimal degrees
(see definition):
-66.8833333
Elevation
(see definition):
No data
Decision Year
(see definition):
01/01/1955
Description
(see definition):
Glacier, 3 mi wide and 9 mi long, which flows W and then NW from the S side of Mount Lupa to the SE corner of Rymill Bay where it joins the Bertrand Ice Piedmont, on the W coast of Graham Land. First surveyed in 1936 by the British Graham Land Expedition (BGLE) under Rymill. Resurveyed in 1948-49 by the Falklands Islands Dependencies Survey (FIDS) and named for James H. Martin, member of the British Australian and New Zealand Antarctic Research Expedition (BANZARE) under Mawson, 1929-31, and first mate of the Penola during the British Graham Land Expedition (BGLE), 1934-37.
Date Created
(see definition):
No data
Date Edited
(see definition):
No data
NOTE: The information regarding
Martin 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
Martin Glacier information contained here. All suggestions for corrections of any errors about
Martin Glacier should be addressed to the National Geospatial-Intelligence Agency.