Explore: Alpine Foreland

The Alpine Foreland, less commonly called the Bavarian Foreland, Bavarian Plateau or Bavarian Alpine Foreland (German: Bayerisches Alpenvorland), refers

Harz, Thuringian Basin, Upper Main-Upper Palatine Hills, Southern Alpine Foreland), others group well-known major regions together (Rhenish Massif, South

periods. The average annual temperatures during the Würm ice age in the Alpine Foreland were below −3 °C (today +7 °C). That has been determined from changes

zone between the High Alps and the Swiss Plateau and the Bavarian Alpine Foreland in the north, as well as to the Pannonian Basin (Alpokalja) in the

used as early as 1882 by Albrecht Penck initially for the northern Alpine Foreland. Later the term was expanded and used to refer to the Scandinavian

The Molasse basin (or North Alpine foreland basin) is a foreland basin north of the Alps which formed during the Oligocene and Miocene epochs. The basin

North Alpine foreland basin and onto the Swabian Jura with thickness of up to 250 m (820 ft); these were deposited in the Paratethys when the Alpine front

waterbodies lie within the Lake Constance Basin (Bodenseebecken) in the Alpine Foreland through which the Rhine flows. The nearby Mindelsee is not considered

England Alpine Foreland, a region in Southern Germany North and South Foreland, two headlands on the coast of Kent, England Nils Tore Føreland (born 1957)

confused with the Bavarian Alps or the Bavarian Alpine Foreland. These terms include the whole of the alpine region (together with parts of the Wetterstein