“Contortion Spur”的意思、由来-开放百科全书

词条

Contortion Spur

释义

References

Contortion Spur ({{Coord|80|25|S|160|9|E|source:GNIS|display=inline,title}}) is the largest and easternmost of three spurs which descend northwards from Mount Madison near the mouth of Byrd Glacier in Antarctica. The spur exposes a spectacular syncline of white marble and black schist. It was geologically mapped on December 10, 2000, by Edmund Stump of the United States Antarctic Program; he suggested the name because of the skewed form of the spur.

References

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2 : Ridges of the Ross Dependency|Shackleton Coast

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