Linked from

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

• LithosphereRelated: Lithospheric fractures and plate boundaries provide routes for magma to rise.

• Planetary differentiationRelated: Differentiation affects where melts form and which materials reach the surface.

• GeologyRelated: Volcanism builds new rock and alters landscapes at plate boundaries and hotspots.

• Planetary geologyRelated: Volcanic landforms show where planetary interiors have melted and resurfaced their crusts.

• Rock cycleRelated: Volcanism returns material from Earth's interior to the surface as lava and ash.

• LystrosaurusRelated: Siberian Traps volcanism is linked to environmental disruption surrounding the extinction.

• Hot springRelated: Volcanic heat powers many, but not all, hot spring systems.

• Albertine RiftRelated: Magma reaches the surface in parts of the Albertine Rift, especially near the Virungas.

• MountainRelated: Repeated eruptions can build volcanic mountains above the surrounding terrain.

• Terrestrial planetRelated: Interior heat drives volcanism, resurfacing rocky planets and releasing gases into their atmospheres.

• OutgassingRelated: Volcanic emissions provide a major route by which planetary interiors release volatile substances.

• Petropavlovsk-KamchatskyRelated: Volcanic terrain defines the peninsula’s landscape and shapes the city’s setting.

• Geochemical cycleRelated: Volcanic gases and lava transfer deep-Earth elements back to surface reservoirs.

• Lake AssalRelated: Volcanic activity has shaped the surrounding Afar landscape and its crater terrain.

• Land (terrain)Related: Volcanic eruptions add new rock and can create islands and plateaus.

• GeodynamicsRelated: Its distribution records melting and material transport within the planet.

• Late Devonian mass extinctionRelated: Volcanic activity is one proposed source of climatic and chemical disruption during the crisis.

• Late Ordovician mass extinctionRelated: Volcanic activity has been proposed as a contributor to late Ordovician environmental change.