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alpine foreland वाक्य

"alpine foreland" हिंदी मेंalpine foreland in a sentence
उदाहरण वाक्यमोबाइल
  • This outcrop of these marine sedimentary rocks is situated in the northern part of the North Alpine Foreland Basin ( NAFB ) and it is famous for a superabundance of family Turritellidae.
  • These terms include the whole of the alpine region ( together with parts of the Wetterstein, the Karwendel, etc . ) and the whole Alpine Foreland on Bavarian state territory.
  • The Alpine Foreland is crossed by the rivers Iller, Wertach, Swabia with the State of Baden-W�rttemberg, and its eastern boundary being the Salzach river on the border with Austria.
  • The Alpine glaciers, that formed a network of ice streams during the high points of the ice ages, repeatedly flowed beyond the boundary of the Alps and advanced into the Alpine Foreland.
  • In this Alpine Foreland glaciation, Penck identified a number of landforms : the ground moraines, the " Zungenbecken ", the terminal moraines and the gravel plains in front of them.
  • The economy and environment of the 4th and 3rd millennia BC in the northern Alpine foreland based on studies of animal bones . " Environmental Archaeology " 11 ( 1 ) : 49-64
  • When the glacier has more fully retreated this produces a finger lake or glacial piedmont lake ( German : " Zungenbeckensee ", known as a " Gletscherendsee " of the glacial series in the Alpine Foreland ).
  • Mediterranean high-pressure systems from the south are characterized by few clouds and warm air, and they influence the weather of the southern slopes of the Alps and that of the Southeastern Alpine Foreland, making them the most temperate part of Austria.
  • Due to its location in the " front row " of the Alps, the Rote Fl�h has outstanding views both of the flat Alpine Foreland as well as the lake of Haldensee, just under 1, 000 metres below in the valley of Tannheimer Tal.
  • In southern Germany, with the exception of the Alpine foreland and the Upper Rhine Graben, there are rather thin Quaternary deposits and formations, geographically confined mostly to lower slopes and valleys where they occur as scree and stone runs or as fluvial gravels and sands.
  • Just over 28 % of Austria is moderately hilly or flat : the Northern Alpine Foreland, which includes the Danube Valley; the lowlands and hilly regions in northeastern and eastern Austria, which include the Danube Basin; and the rolling hills and lowlands of the Southeastern Alpine Foreland.
  • Just over 28 % of Austria is moderately hilly or flat : the Northern Alpine Foreland, which includes the Danube Valley; the lowlands and hilly regions in northeastern and eastern Austria, which include the Danube Basin; and the rolling hills and lowlands of the Southeastern Alpine Foreland.
  • Many secondary landscape regions only have one major unit group ( Mecklenburg Coastal Lowland, Harz, Thuringian Basin, Upper Main-Upper Palatine Hills, Southern Alpine Foreland ), others group well-known major regions together ( Rhenish Massif, South German Scarplands ); others are entirely new groupings.
  • These valleys, created by glacial meltwaters, do not appear in the Alpine Foreland as they do, for example, in North Germany because their function was assumed by the great rivers that already existed in the region-the Danube, Rhine, Rh�ne and Po-or their tributaries, which transported away the meltwaters of the glaciers.
  • In contrast to the Helvetic Domain and the Flysch Zone that still mostly have a low mountain character ( " German : " ) although they are morphologically clearly set apart from the Alpine foreland, the Northern Limestone Alps form high mountains ( " German : " ) of well over 2, 000 metres above sea level.
  • The beginning of the Riss ice age, according to the 2002 Stratigraphic Table of Germany, was the end of the Holstein interglacial ( known as the Mindel-Riss interglacial in the Alpine Foreland and corresponding to the " Samerbe ", " Thalgut ", " Praclaux " and " La C�te " ).
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