Linked from

The 9 pages that link to Andean orogeny, each with the reason it gives.

• AndesRelated: It explains how subduction and crustal deformation raised the range.

• MioceneRelated: Andean uplift altered regional climates and habitats during the Miocene.

• Nazca PlateRelated: Nazca Plate convergence and subduction are central drivers of Andean mountain building.

• AltiplanoRelated: Crustal shortening and uplift raised the region into a high plateau.

• South American PlateBroader topic: It is the principal continental-scale result of convergence at the plate’s western margin.

• Peru–Chile TrenchRelated: The trench and the Andes are linked parts of the same convergent margin.

• Andean Volcanic BeltRelated: Mountain building and crustal thickening alter how magma rises and evolves beneath the belt.

• American CordilleraBroader topic: It illustrates how subduction can raise and deform a major cordillera segment.

• Cordillera BlancaNarrower topic: The Cordillera Blanca is one product of this continent-scale mountain building.