Linked from

The 33 pages that link to Orogeny, each with the reason it gives.

• Continental collisionNarrower topic: Continental collision is one major route to mountain-belt formation.

• Tectonic upliftNarrower topic: Mountain-building episodes commonly combine uplift with folding, faulting, and crustal thickening.

• DolomitesNarrower topic: The range’s uplift belongs to the larger tectonic history that built the Alps.

• Alpine orogenyNarrower topic: The Alpine episode is one regional example of this broader process.

• Thrust faultNarrower topic: Thrusting is a principal way orogenic belts shorten and thicken the crust.

• Caledonian orogenyNarrower topic: The Caledonian event is one named example of this broader process.

• Foreland basinNarrower topic: An orogeny creates the mountain load beside which a foreland basin develops.

• Dinaric AlpsNarrower topic: The range’s uplift belongs to the mountain-building history of the Mediterranean region.

• PyreneesNarrower topic: The Pyrenees are one product of this broader process.

• Andean orogenyNarrower topic: The Andes are a major example of this broader geological process.

• Kunlun MountainsNarrower topic: The Kunlun Mountains are a major product of mountain-building processes.

• Alleghanian orogenyNarrower topic: The Alleghanian event is one named episode of mountain building.

• Taurus MountainsNarrower topic: The Taurus Mountains belong to the broader mountain-building belt formed by continental convergence.

• FlyschNarrower topic: Flysch deposition is tied to the growth and advance of an orogenic belt.

• Grenville orogenyNarrower topic: The Grenville event is a major example of this broader tectonic process.

• Mountain formationNarrower topic: This broader process groups the tectonic changes that build many mountain ranges.

• Pontic MountainsNarrower topic: The Pontic Mountains are a product of mountain-building along northern Anatolia.

• Binalud MountainsNarrower topic: The range’s uplift and deformation are local expressions of mountain-building across Iran.

• Fold mountainsNarrower topic: Fold mountains develop during orogenies that deform and raise continental crust.

• Gamburtsev Mountain RangeNarrower topic: Its origin requires explaining how high relief developed within an ancient continental interior.

• Algoman orogenyNarrower topic: The Algoman event is a regional example of this broader geological process.

• Terra Australis OrogenNarrower topic: The Terra Australis Orogen is an exceptionally extensive example of orogenic development.