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The entire wiki reimagined as a visual magazine with video discovery · Watch your interests come alive
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Molasse basin
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The Molasse basin is a foreland basin north of the Alps which formed during the Oligocene and Miocene epochs. The basin formed as a result of the flexure of the European plate under the weight of the
The Bavarian Alps rise from the green hills of the Molasse basin. The hills consist of tilted molasse beds, erosional material transported from the mo
The Bavarian Alps rise from the green hills of the Molasse basin. The hills consist of tilted molasse beds, erosional material transported from the mountains into their foreland.
Alternating grey fluviatile sands and red silty marls of the Lower Freshwater Molasse at Wallenried, Switzerland.
Alternating grey fluviatile sands and red silty marls of the Lower Freshwater Molasse at Wallenried, Switzerland.
Fold and thrust belt
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A fold and thrust belt is a series of mountainous foothills adjacent to an orogenic belt, which forms due to contractional tectonics. Fold and thrust belts commonly form in the forelands adjacent to m
An example of thin-skinned thrusting in Montana. The white Madison Limestone is repeated, with one example in the foreground (that pinches out with di
An example of thin-skinned thrusting in Montana. The white Madison Limestone is repeated, with one example in the foreground (that pinches out with distance) and another to the upper right corner and top of the picture.