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QUATERNARY

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Originally appearing in Volume V22, Page 718 of the 1911 Encyclopedia Britannica.
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QUATERNARY , in See also:

geology, the See also:time - See also:division which embraces the Pleistocence and See also:Holocene epochs, i.e. the later portion of the See also:Cainozoic era, See also:equivalent to the " See also:Post-See also:Pliocene " or " Post-See also:Tertiary " of certain writers. The See also:term was proposed by J. See also:Desnoyers in 1829 to See also:cover those formations which were formed just anterior to the See also:present. There are other ways of regarding the Quaternary time. See also:Sir A. See also:Geikie (See also:Text See also:Book of Geology, 4th ed., 1903) divides it into an upper, post-glacial or Human See also:period, and a See also:lower, See also:Pleistocene or Glacial period; but he subdivides the former into an Historic and a Prehistoric See also:epoch, a See also:scheme presenting difficulties, for the See also:Palaeolithic or lower See also:stage of prehistoric time cannot really be separated from the Pleistocene (q.v.). E. See also:Kayser (Formationskunde, 3rd. ed., 1906), who is in agreement with the See also:definition accepted above, employs a nomenclature which is rarely adopted by See also:British geologists; he divides the Quartarformation (Quartar) into a younger, See also:modern epoch, the See also:Alluvium, and an older epoch, the Pleistocene or See also:Diluvium (= Glacial). A. de See also:Lapparent, on the other See also:hand (Traite de geologie, 5th ed., 1906), treats the Era moderne or Quaternaire as a See also:great time division equivalent in value to the Tertiary, Secondary, &c., which is so far represented only by a first epoch, the Pleistocene.

End of Article: QUATERNARY

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