Watson Escarpment (The name as it would appear in a gazetteer)
Watson Escarpment (The name as it would appear on a map)
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Feature type: Escarpment (2f)
This name originates from United States of America. It is part of the United States Gazetteer and the SCAR Composite Gazetteer of Antarctica.
Names that other countries have for this feature:
A major escarpment in the Queen Maud Mountains, trending northward along the east margin of Scott Glacier, then eastward to Reedy Glacier where it turns southward along the glacier's west side. Somewhat arcuate, the escarpment is nearly 100 mi long, rises 3,550 m above sea level, and 1,000 to 1,500 m above the adjacent terrain. The north-central part of the escarpment was observed from a vantage point on Supporting Party Mountain and was partially mapped in December 1929 by the ByrdAE geological party under Laurence Gould. The escarpment was more closely observed in December 1934 by the ByrdAE geological party under Quin Blackburn, and was named by Byrd for Thomas J. Watson, American business executive, a patron of this expedition. The escarpment was mapped in detail by USGS from surveys and USN air photos, 1960-64.
No images of this place could be found.
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