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olaszul en el Diccionario Oxford Paravia de italiano

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Molasse can be very thick near the mountain front, but usually thins out towards the interior of a craton; such massive, convex accumulations of sediment are known as "clastic wedges".
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Coarse sediments from the continual uplift and erosion were later deposited in foreland areas as molasse.
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In the western section of the municipality, which is larger by far, there is a glacial landscape of molasse hills with extensive woods and moor-like depressions.
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The inhabitants of the village paid taxes on wheat, barley, olive trees, vineyards, fruit trees, grape syrup, molasse, and goats and/or beehives.
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It is considered a classic orogenic molasse.
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The region where the molasse crops out is divided into two.
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The tower was originally built in wood, then in molasse and pebbles like the place.
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When the orogen evolves the foreland basin becomes shallower and molasse is deposited on top of the flysch.
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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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Such erosional material of a growing mountain chain is called molasse and has either a shallow marine or a continental facies.
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