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The Glacier Ice Impact Hypothesis

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The Glacier Ice Impact Hypothesis proposes four mechanisms for the creation of the Carolina Bays and the Nebraska Rainwater Basins. First, one or more extraterrestrial impacts on the Laurentide Ice Sheet by the Great Lakes ejected pieces of glacier ice in ballistic trajectories. The secondary impacts produced seismic vibrations that liquefied unconsolidated soil. The oblique impacts of glacier ice on viscous ground created inclined conical cavities. And finally, the inclined conical cavities, also called penetration funnels, became shallow elliptical basins by viscous relaxation.
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