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Quaternary geology : ウィキペディア英語版 | Quaternary geology
Quaternary geology is the branch of geology that study developments from 2.6 millions years ago onwards. In particular quaternary geology study the process and deposits that developed during the quaternary, a period characterized by glacial-interglacial cycles.〔〔 Quaternary geology has developed over time from being originally a branch of historical geology to becoming a science on its own.〔 ==See also==
*Geoarchaeology *Geomorphology *Hydrology *Neotectonics *Palynology *Sedimentology *Soil science *Tephrochronology
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Quaternary geology」の詳細全文を読む
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