Linked from

The 12 pages that link to Himalayan orogeny, each with the reason it gives.

• CenozoicRelated: Its uplift altered atmospheric circulation and influenced Cenozoic climate.

• Indian subcontinentRelated: It transformed the subcontinent’s northern margin into a high mountain system.

• NeogeneRelated: Its uplift influenced Asian landscapes and regional climate during the Neogene.

• Asian monsoonRelated: The resulting mountain barrier altered regional atmospheric circulation and rainfall.

• Nanga ParbatRelated: This process formed the range containing Nanga Parbat.

• MakaluRelated: The tectonic collision that raised the Himalaya also produced Makalu's elevation.