Danube-Günz Interglacial
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The Danube-Gunz interglacial (german: Donau-Günz-Interglazial), Danube-Gunz warm period (''Donau-Günz-Warmzeit''), often just Danube-Gunz, or also Uhlenberg interglacial (''Uhlenberg-Warmzeit'') are historical terms for a hypothetical
warm period Warm, WARM, or Warmth may refer to: * A somewhat high temperature * Kindness Music * ''Warm'' (The Lettermen album), 1967, and the title song * ''Warm'' (Johnny Mathis album), 1958, and the title song * ''Warm'' (Herb Alpert album), 1969 * ' ...
of the
Pleistocene The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was fina ...
in the
Alps The Alps () ; german: Alpen ; it, Alpi ; rm, Alps ; sl, Alpe . are the highest and most extensive mountain range system that lies entirely in Europe, stretching approximately across seven Alpine countries (from west to east): France, Sw ...
, between the
Danube The Danube ( ; ) is a river that was once a long-standing frontier of the Roman Empire and today connects 10 European countries, running through their territories or being a border. Originating in Germany, the Danube flows southeast for , pa ...
and
Gunz glacial Gunz may refer to: Games * '' GunZ: The Duel'', a 2005 South Korean online third-person shooting game * '' GunZ 2'', a 2011 South Korean fighting video game, sequel to ''GunZ: The Duel'' Places * Günz, a river in Bavaria, Germany ** Östli ...
s. The interglacial was defined as the erosion phase that followed the Danube glacial and preceded the Gunz stage. It is therefore represented by the gap between the two depositions that are attributed to the two cold periods; in the type regions of the two glacial there are various depositions. In the area of the
Iller-Lech Plateau The Iller-Lech Plateau (german: Donau-Iller-Lech-Platte), also known as the Upper Swabian Plateau (''Oberschwäbische Hochebene''), is one of the natural regions of Germany. Boundaries In the northwest the Iller-Lech Plateau borders on the Sw ...
they lie between the Lower Deckschotter (''Untere Deckschottern'') of the
Zusam The Zusam is a river in Bavaria, Germany and a right tributary of the Danube. Its source is just north of the village of Könghausen, in the Unterallgäu district of Bavaria. It flows north for approximately 97 km, before converging into the ...
Plateau and the Intermediate Deckschotter (''Zwischenschottern''); in the region of the Salzach Glacier between the ''Eichwald Schotter'' and the Older Deckenschotter (''Ältere Deckenschottern''); and the area of
Traun Traun () is an Austrian city located on the north bank of the river Traun and borders Linz, the capital of Upper Austria, to the east. The name ''Traun'' is derived from the Celtic word for river (''dru''). Traun is the fifth largest city in U ...
and Enns between the ''Prägünz Schotter'' and the Older Deckenschotter. The erosion phase linked with this interglacial is very distinct and the composition of the gravels (''Schotter'') in the area east of the
Rhine Glacier The Rhine Glacier was a glacier during the last glacial period and was responsible for the formation of the Lake Constance. References Glaciers of Switzerland Rhine {{switzerland-glacier-stub ...
changes markedly. Modern research has found that both Danube and Gunz correspond to many glacial cycles, as identified by
marine isotope stage Marine isotope stages (MIS), marine oxygen-isotope stages, or oxygen isotope stages (OIS), are alternating warm and cool periods in the Earth's paleoclimate, deduced from oxygen isotope data reflecting changes in temperature derived from data ...
s, making the term Danube-Gunz superfluous. The term is not used in the 2016 version of the detailed stratigraphic table by the German Stratigraphic Commission.German Stratigraphic Commission: Stratigraphische Tabelle von Deutschland 2016
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See also

*
Timeline of glaciation There have been five or six major ice ages in the history of Earth over the past 3 billion years. The Late Cenozoic Ice Age began 34 million years ago, its latest phase being the Quaternary glaciation, in progress since 2.58 million years ago. ...


References

{{Alpine glaciations Pleistocene events Ice ages