Molasse basin

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Geology of the Alps
The Alps
Tectonic subdivision

Helvetic Zone

Penninic nappes
Austroalpine nappes
Southern Alps
Formations & rocks

Bündner schist | flysch | molasse

Geological structures

Aarmassif | Dent Blanche klippe | Engadine window | Flysch zone | Giudicárie line | Greywacke zone | Hohe Tauern window | Molasse basin | Penninic thrustfront | Periadriatic Seam | Ivrea zone | Lepontin dome | Rechnitz window | Rhône-Simplon line | Sesia unit

Paleogeografic terminology

Valais Ocean

Briançonnais microcontinent
Piemont-Liguria Ocean
Apulian or Adriatic plate

In geology, a molasse basin is the stage of a developing foreland basin, in which molasse is deposited. The term is used for all localities, but this type of basin was first studied in the Swiss and Bavarian foreland of the Alps, where the term molasse had its origins[1], therefore that particular basin is called the Molasse basin.

The Bavarian Alps rise from the green hills of the Molasse basin. The hills consist of detritus from the mountains in their hinterland.
The Bavarian Alps rise from the green hills of the Molasse basin. The hills consist of detritus from the mountains in their hinterland.

"The" Molasse basin was formed during the early Tertiary period as a result of crustal thickening with the rising of the Alps. The basin filled with the products of erosion and weathering in the new mountain range, sand, gravel and boulders deposited as fans of sandstones and conglomerates. The base of the basin is formed by pre-orogenic (Mesozoic) sedimentary rocks. When the Alps rose further, a decollement horizon developed at the base of the Mesozoic rocks in Triassic evaporites, along which thrusting to the north took place, forming the Jura mountains to the northwest. The Swiss part of the Molasse basin is now located in between the Alps and the Jura mountains, as a large piggy-back basin. In the Eastern Alps an external mountain range never developed, the Molasse basin of the Eastern Alps is therefore simpler in its structure. Due to the continued thrusting, foreland basin extension was soon compensated by uplift. The molasse in the Swiss Plateau, the South Bavarian plain and Eastern Austria is now at 350 to 400 meters above sea level at its northern rim, slowly rises southwards and can attain more than 1,000 m at its contact with the Alps.

[edit] References

  1. ^ Molasse, Lexique de géologie sédimentaire, Université de Liège (in French)
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