Moine Thrust Belt - Formation

Formation

The discovery of the Moine Thrust in 1907 was a milestone in the history of geology as it was one of the first thrust belts discovered. The formation has since been re-interpreted many times. Eventually, the Moine Thrust corroborated tectonic plate theory in that, during the Caledonian orogeny of the Silurian period, Scotland was compressed as a European plate thrust westwards over a thrust fault and above the ancient Lewisian Gneiss on the Laurentian Plate.

The thrust belt defines the boundary between the Hebridean Terrane to its northwest and the Northern Highlands Terrane to its southeast. The thrust carried metamorphic material over 200 km across Scotland entirely masking the geology of the previous terrane. However, small windows, such as the Assynt window and the Glen Achall imbricated thrust system, allow Geologists to estimate what the geology of Scotland was like before the Caledonian orogeny.

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