Holocene

Epoch of geologic time approximately 11 thousand years ago extending to the present. https://doi.org/10.3133/fs20103059
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Mineralogic causes of variations in magnetic susceptibility of late Pleistocene and Holocene sediment from Great Salt Lake, Utah

Results of magnetic susceptibility (MS) measurements and magnetic mineralogy of sediments sampled in three cores from the south basin of Great Salt Lake

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