Epoch of geologic time approximately 2.6 million to 11 thousand years ago.
This category is also used for ice age.

Results listed by similarity [list alphabetically]
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