Linked from

The 36 pages that link to Continental collision, each with the reason it gives.

• Continental crustRelated: Collision thickens existing crust and builds major mountain belts.

• OrogenyRelated: Collision thickens and folds crust, as in the formation of the Himalaya.

• Arabian PlateRelated: This process explains the Arabia–Eurasia mountain-building zone.

• Ural MountainsRelated: Collision between ancient landmasses generated the Uralian mountain belt.

• Mohorovičić discontinuityRelated: Collision can thicken, deform, or duplicate crust, producing complex Moho structure.

• Earth's crustRelated: Collision thickens and deforms continental crust, building major mountain belts.

• Anatolian PlateRelated: Collision between Arabia and Eurasia supplies the compression driving Anatolian escape.

• PannotiaRelated: Collision is the proposed mechanism by which Pannotia’s component landmasses joined.

• Mountain rangeRelated: Collision raises broad, high ranges such as the Himalaya.

• Columbia (supercontinent)Related: Collisions welded Columbia's separate crustal blocks into a larger landmass.

• KenorlandRelated: Collision is one process that could have joined the cratons proposed to form Kenorland.

• ContinentsRelated: Collisions join landmasses and build mountain belts along continental margins.

• SupercontinentRelated: Collisions weld separate continental blocks into larger landmasses.

• Continental fragmentRelated: A fragment can collide with a continent and become part of its crust.

• Paleo-Tethys OceanRelated: Collision followed Paleo-Tethyan seafloor consumption and helped join continental blocks.

• Fold mountainsRelated: Collision supplies the compression that folds and uplifts extensive mountain belts.

• Algoman orogenyRelated: Collision is a leading process used to explain the mountain-building and crustal thickening.

• North CascadesRelated: Ancient plate interactions helped assemble and raise the rocks of the range.

• PaleocontinentRelated: Collisions merge paleocontinents and build mountain belts along their margins.

• Terra Australis OrogenRelated: Collision contributed to deformation and mountain building in parts of the belt.