Alpine orogeny

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The Alpine orogeny is a major mountain-building event that created the Alps and other ranges across southern Europe and parts of Asia through the collision of tectonic plates during the Cenozoic Era.

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Referenced by (16)

Full triples — surface form annotated when it differs from this entity's canonical label.

Pennine Alps geologicalAge Alpine orogeny
Altai Mountains geologicalFormation Alpine orogeny
Lesser Caucasus geologicalOrigin Alpine orogeny
Pamir Mountains geologicalOrigin Alpine orogeny
Balkan Mountains geologicalPeriod Alpine orogeny
Sierra Nevada (Spain) geologicalPeriod Alpine orogeny
Cenozoic includesEvent Alpine orogeny
Iranian plateau orogeny Alpine orogeny
Jura Mountains orogeny Alpine orogeny
Lesser Caucasus orogeny Alpine orogeny
Pennine Alps orogeny Alpine orogeny
Alps partOf Alpine orogeny
Himalayan orogeny partOf Alpine orogeny
Ligurian Alps partOf Alpine orogeny