245:("Hattem Layers"). These erratics are supposed to be transported by fluvial drift ice and are the first indicators in this part of the North Sea Basin of a major glaciation in the Scandinavian mountains. Most probably the reshaping of the Eridanos source areas in the Scandinavian mountains had already started during this glacial stage. During the succeeding Bavel Interglacial the fluvial system reached its largest size, but sedimentation rates already dropped at that time. The repeated buildup of the Scandinavian ice cap during successive ice ages after this interglacial resulted in a complete destruction of the source area, decapitating the fluvial system, and in the birth of a glacially excavated area surrounding the Scandinavian mountainous areas, in which region the Baltic Sea would later come into existence. During the first glacial stage of the
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in the sand, as well as in the gravel fractions. The color of the mainly coarse sands is grey-white, and in the
Netherlands these deposits are, therefore, known as the White Sands ("Witte Zanden"). During the Early Pleistocene in the Netherlands fluvial deposits of eastern provenance mix with fluvial
317:, 1988. The history of the great northwest European rivers during the past three million years. Philosophical Transactions of the Royal Society, B.318: 559–602.
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Eridanos sediments in the
Netherlands and the neighbouring North Sea can be recognized by a high content of transparent blue-grey, lightgrey, and colorless
332:"The South Swedish Dome: a key structure for identification of peneplains and conclusions on Phanerozoic tectonics of an ancient shield"
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deflected the
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Fluvial sedimentation from the
Fennoscandian area into the North-West European Basin during the Late Cenozoic
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The Late
Cenozoic Eridanos delta system in the southern North Sea Basin: a climate signal in sediment supply?
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Remnants of the
Eridanos are found all through northern Europe, from the current North Sea and the
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Geologisch onderzoek in de stuwwal van de
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Eridanos deposits in the
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Overeem, I., Weltje, G. J., Bishop-Kay, C., Kroonenberg, S. B., 2002.
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is now. Its river system is also known as the "Baltic River System".
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The
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area, where sediments carried by the river built an immense
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The geological
Eridanos was most important during the
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The Eridanos began about 40 million years ago in the
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330:; Olvmo, Mats; Bonow, Johan M. (2017).
156:. By about 12 million years ago in the
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36:verification
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409:Pleistocene
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195:Description
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