The hills consist of tilted molasse beds, erosional material transported from the mountains into their foreland . ]]
22.
This species is known from several dozen bones, found in Early Miocene strata of the Patagonian Molasse Formation.
23.
Stephanian age molasse deposits overlie the other Carboniferous rocks and are unrelated to the Hercynian ( Variscan ) orogeny.
24.
The region is divided into several structurally uplifted blocks, where extensively Molasse Basin ) and the Upper Rhine Graben.
25.
The Central Plateau is mainly composed of molasse, a sedimentary rock which formed at the bottom of the Tethys ocean.
26.
Such erosional material of a growing mountain chain is called molasse and has either a shallow marine or a continental facies.
27.
Between them there are hill countries, in the canton of Thurgau also the broad molasse ranges of Seer�cken and Ottenberg.
28.
The fossils of this species are known from several dozen bones, found in Early Miocene rocks of the Patagonian Molasse Formation.
29.
Afterwards, the highway enters the Molasse plateau of Freiburg Plateau, tackling in several stages a height difference of just over.
30.
The molasse can sometimes completely fill a foreland basin, creating a nearly flat depositional surface, that nonetheless remains a structural syncline.
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