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The Labyrinth is an approximately 50 km-long network of bedrock channels and scoured terrain believed to have been formed by erosion associated with release of subglacial meltwater (buried lakes) beneath the East Antarctica ice sheet. The Labyrinth, Antarctica.

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Photo by Jacquelyn Hams (PolarTREC 2012), Courtesy of ARCUS
Photographer: Jacquelyn Hams
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