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Beardmore Glacier

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Beard·more Glacier  (bîrdmôr, -mr)
A valley glacier, about 418 km (260 mi) long, in the Queen Maud Mountains of Antarctica. It was discovered by the British explorer Sir Ernest Shackleton in 1908.


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Dick Richards was appointed physicist but had a breakdown after returning from the Beardmore Glacier and was unable to work for much of 1916.
They will pick their way across the Beardmore glacier, collecting ice samples for scientific analysis in the UK.
Ashworth excavated the relic from a 2-meter-thick outcrop of siltstone along Antarctica's Beardmore Glacier.
 
 
 
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