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The Riss glaciation ((ドイツ語:Riß-Kaltzeit), ''Riß-Glazial'', ''Riß-Komplex'' or (obs.) ''Riß-Eiszeit'') is the second youngest glaciation of the Pleistocene epoch in the traditional, quadripartite glacial classification of the Alps. The literature variously dates it to between about 300,000 to 130,000 years ago and 347,000 to 128,000 years ago. It coincides with the Saale glaciation of North Germany. The name goes back to Albrecht Penck and Eduard Brückner who named this cold period after the river Riß in Upper Swabia in their 3 volume work ''Die Alpen im Eiszeitalter'' ("The Alps in the Ice Age") published between 1901 and 1909. == Boundaries and division == The Riss glaciation was defined by Penck and Brückner as the Lower (''Niedere'') or Younger Old Moraines and Old Terminal Moraines High Terraces (''Jüngere Altmoränen und Alt-Endmoränen-Hochterrassen''). The type locality lies near Biberach an der Riß in the area of the outer northeastern Rhine Glacier. Results gained from over a century of research show that in almost all glacial periods, several ice advances took place. Today it is reckoned that there were, ''in toto'', at least eight to fifteen ice advances. In the Riss stage, too, there were several advances of the ice sheet, so that it can be divided into interstadials (ice retreats) and stadials (ice advances) and at least one hitherto unnamed warm period. The present-day division differs from the original Penck classification. The beginning of the Riss ice age, according to the 2002 Stratigraphic Table of Germany, was the end of the Holstein interglacial (known as the Mindel-Riss interglacial in the Alpine Foreland and corresponding to the ''Samerbe'', ''Thalgut'', ''Praclaux'' and ''La Côte''). Its end is the start of the Eem interglacial (Riss-Würm interglacial). It is thus roughly contemporaneous with the Saale glaciation of the North German glacial sequence. The Riss is paralleled by MIS 6, 8 and 10, which would therefore place it about 350,000 and 120,000 years ago. Excluded from the Riss glaciation is the so-called Old Riss (''Ältere Riß''), the time of the greatest ice advance in the Alpine region: today it is referred to as the Haslach-Mindel complex (in Bavaria and Austria), Hoßkirch complex (in Baden-Württemberg) or Great Glaciation in Switzerland. The classification of ice ages in Switzerland varies from that used in the Bavarian and Austrian Alpine Foreland. The glaciation complex between the end of the Holstein and the beginning of the Eem interglacials is referred to as the Penultimate Ice Age and the Great Glaciation.〔 It is divided into two additional interstadials, the so-called Double Holstein Event of Meikirch (''doppelte Holstein-Vorkommen von Meikirch''), which is not identical, however, with the Holstein interglacial.〔Habbe 2007, p. 80〕 During the period of maximum glaciation, ancient man (Homo heidelbergensis – later the Neanderthals) retreated behind the permafrost boundary and, in the warmer periods, spread beyond it to the north and northeast. Not until the Weichsel-Würm ice age did modern Cro-Magnon man settle these regions about 40,000 B. C. 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「Riss glaciation」の詳細全文を読む スポンサード リンク
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