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. Until now, reliable chronological classifications based on numericalages for many Pleistocene fluvial deposits in the Alpine Foreland were rare.In this study, new numeric data (ESR, OSL, 14C ) fromMiddle and Upper (Late) Pleistocene Hochterrassen(high terraces) andUbergangsterrassen (transitional terraces) inthe Bavarian Alpine Foreland are presented. The dating results imply thatthe Hochterrassen gravel sensustricto were deposited during the penultimate glacial (MIS 6,Rissian), and that underlying older gravel accumulation are predominantly ofpenultimate interglacial (MIS 7, Riss–Riss interglacial) age. In some areasof the Hochterrassen in the Danube valley southof Regensburg (interglacial Hartinger Schichten,Harting layers), and in some areas of the Rainer Hochterrasse (basal gravel unit I),Hochterrassen gravels are underlain by much olderinterglacial gravel deposits. These interglacial basal gravel depositsillustrate that the downcutting of these valleys far away from areas ofPleistocene foreland glaciations happened predominantly duringwarm-temperate interglacial or late-glacial periods. One last interglacial(MIS 5e, Riss–Wurm interglacial)Hochterrasse is morphologically preserved in theIsar valley. This Jungere Moosburger Hochterrasse is composed of theFagotienschotter (Fagotia gravel, named after thegastropod Fagotia acicularis). The next youngerterraces are the Early to Middle Wurmian (MIS 5d to MIS 3?)Ubergangsterrassen (transitional terraces),whereas the younger one of the two Ubergangsterrassenwas formed most probably during the Middle Wurmian (MIS 3).

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The formation of Middle and Upper Pleistocene terraces (&amp;lt;i&amp;gt;Übergangsterrassen&amp;lt;/i&amp;gt; and &amp;lt;i&amp;gt;Hochterrassen&amp;lt;/i&amp;gt;) in the Bavarian Alpine Foreland – new numeric dating results (ESR, OSL, &amp;lt;sup&amp;gt;14&amp;lt;/sup&amp;gt;C) and gastropod fauna analysis