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Elster glaciation
The Elster glaciation ((ドイツ語:Elster-Kaltzeit), ''Elster-Glazial'' or ''Elster-Zeit'') or, less commonly, the Elsterian glaciation - in the older and popular scientific literature also called the Elster Ice Age (''Elster-Eiszeit'') - is the oldest known ice age that resulted in the large-scale glaciation of North Germany. It is temporally identified with the south German Mindel glaciation. The Elster glaciation is currently dated to about 400,000 to 320,000 years ago.〔Litt et al. (2007: pp.27ff)〕 It succeeded a long period of rather warner average temperatures, the Cromerian Complex. Two ice advances were very extensive. The Elster was followed by the Holstein interglacial. The glacial period is named after the White Elster, a right tributary of the Saale.
== Literature ==
* Thomas Litt, Karl-Ernst Behre, Klaus-Dieter Meyer, Hans-Jürgen Stephan und Stefan Wansa: (''Stratigraphische Begriffe für das Quartär des norddeutschen Vereisungsgebietes.'' ) Eiszeitalter und Gegenwart (Quaternary Science Journal), 56(1/2): 7-65, Hannover 2007 ,
* Leopold Benda (ed.): ''Das Quartär Deutschlands.'' 408 pp., Borntraeger, Berlin, Stuttgart, 1995 ISBN 3-443-01031-8
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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