The Valais Ocean is a subducted oceanic basin which was situated between the continent Europe and the microcontinentIberia or so called Briançonnais microcontinent. Remnants of the Valais ocean are found in the western Alps and in tectonic windows of the eastern Alps and are mapped as the so-called "north Penninic" nappes.[1]
Tectonic history
After the breakup of Pangaea in the early Mesozoic age, the continents of Africa, South America, Europe, and North America began to move away from each other. The breaking up, or rifting, did not take place along one unbroken line; thus, at the southern edge of the European plate, the microcontinent Iberia also began to break away from Europe. In the western part of the rift that separated the two landmasses, oceanic crust was formed in what is at present the Gulf of Biscay, while in the eastern part, the Valais Ocean was formed.
When, in the Cretaceous period, Africa again began to move towards Europe, the Valais Ocean became sandwiched between the two continents. To the east, the Valais oceanic crust, together with a piece of Iberian continental crust (called the Briançonnais terrane), subducted beneath the Apulian plate, a part of the African tectonic plate that had begun to move independently. This process eventually led to the formation of the Alps. To the west, no subduction took place, but the Iberian plate moved against the European plate along a large transform fault, which led to the formation of the Pyrenees.
