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The Holstein Interglacial followed the Elsterian Glacial Stage and preceded the Saale Glacial Stage.
The Riss Glacial Stage is roughly contemporaneous with the Illinoian Glacial Stage of North America.
The Eemian Interglacial followed the Saale Glacial Stage and preceded the Weichsel Glacial Stage.
The Würm glacial stage followed the Riss-Würm interglacial and is correlated with the Weichsel glacial stage of northern Europe and the Wisconsin glacial stage of North America.
The Riss is correlated with the Gipping Glacial Stage of Great Britain and the Saale Glacial Stage of northern Europe.
The Waal Interglacial follows the Eburon Glacial Stage and precedes the Menapian Glacial Stage, both times of relatively severe climatic conditions.
The Riss-Würm Interglacial Stage, a period of relatively moderate climatic conditions, followed the Riss Glacial Stage and preceded the Würm Glacial Stage, both periods of deteriorating conditions.
The Günz-Mindel Interglacial preceded the Mindel Glacial Stage and followed the Günz Glacial Stage, a period of relatively moderate climatic conditions between two periods of glacial advance.
The extensive and complex Saale deposits are correlated with the Gipping Glacial Stage of Britain and the Riss Glacial Stage of the European Alpine region.
The Elsterian is equated with the Mindel Glacial Stage of classical European usage in the Alpine region, and the Kansan Glacial Stage of North America.
The Weichsel is correlated with the Würm Glacial Stage of Alpine Europe and is broadly equivalent to the Wisconsin Glacial Stage of North America.
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