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Suzanne L. Bevan, Adrian
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53:) is an ice-filled inlet that recedes inland for 7 nautical miles (13 km) and is 12 nautical miles (22 km) wide at its entrance between
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discovered the inlet on his flight of
December 20, 1928. Wilkins reported four large glaciers flowing into the inlet, which he named
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because their relative position was suggestive of the radial cylinders of his
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Sailing
Directions (planning Guide) and (enroute) for Antarctica
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Defense
Mapping Agency Hydrographic/Topographic Center,
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Centuries of intense surface melt on Larsen C Ice Shelf
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engine. The inlet was photographed from the air by the
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16:Inlet on the coast of Graham Land, Antarctica
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127:https://doi.org/10.5194/tc-11-2743-2017
125:, The Cryosphere, 11, 2743–2753, 2017
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81:(USAS) in 1940 and charted by the
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178: This article incorporates
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292:Bowman Coast geography stubs
230:. You can help Knowledge by
111:Andy Elvidge, Ian Renfrew,
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114:What causes foehn warming?
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277:Inlets of Graham Land
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