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In the Anadarko Hot Ice 1 well, a continuous core was acquired from 107 ft (33 m) subsurface to 2300 ft (701 m). The Hot Ice 1 well cored through the Tertiary-age sediments of the Sagavanirktok Formation, the Tertiary and upper Cretaceous Prince Creek Formation (which includes the informally named Ugnu sandstones), and Schrader Bluff Formation (which includes the informally named West Sak sandstones); the core ended in 42 ft (13 m) of what appears to be a marine section of fine-grained sediment. The recovered core was described as 37% unconsolidated sandstone. The Ugnu sandstones and shallower section cored...

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