Linked from

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

• StratovolcanoRelated: Magma accumulates and evolves below many stratovolcanoes before rising toward the surface.

• Mid-ocean ridgeRelated: Melt rising beneath the ridge axis crystallizes to form the lower crust and gabbro layer.

• Caldera basinRelated: Withdrawal from this reservoir removes support beneath the summit.

• Mount FujiRelated: Stored magma can contribute to renewed activity beneath Fuji.

• Flood basaltRelated: How magma is stored and transferred during exceptionally large eruptions remains difficult to reconstruct.

• KīlaueaRelated: Changes in magma storage beneath the summit accompany inflation and deflation.

• LavaRelated: It stores magma before some of it rises and emerges as lava.

• East Pacific RiseRelated: Magma beneath the ridge supplies much of its erupting lava and new crust.

• Volcanic ventRelated: It can supply magma that rises toward a vent.

• Porphyritic textureRelated: Crystal growth and later changes may occur during storage in a chamber.

• Bushveld ComplexRelated: Repeated magma replenishment is central to explaining the complex’s layered structure.

• Igneous petrologyRelated: Processes within these reservoirs shape many intrusive and volcanic rocks.

• Yellowstone CalderaRelated: Withdrawal from Yellowstone’s magma storage contributed to caldera collapse.

• Intrusive rockRelated: Many intrusive rocks crystallize within magma bodies before later exposure.

• Juan de Fuca RidgeRelated: Magma stored beneath ridge segments supplies eruptions and new crust.

• Skaergaard intrusionRelated: Its layered rocks preserve evidence of crystallization within a large magma body.

• Volcano seismologyRelated: Seismic methods infer its structure indirectly, and its geometry can remain uncertain.

• Igneous intrusionRelated: A chamber can feed intrusions that extend into surrounding crust.

• BatholithRelated: Magma supplied to crustal intrusions can collect in chambers before cooling.

• Mount AsoRelated: Changes in Aso’s underground magma and fluids help drive eruptions and unrest.

• PopocatépetlRelated: Magma storage and movement beneath the volcano help drive its activity.

• Santorini calderaRelated: Withdrawal of magma from a reservoir can cause the ground above it to subside.

• Emi KoussiRelated: Magma storage beneath the volcano supplied eruptive material.

• Igneous differentiationRelated: The physical structure and lifetime of chambers constrain how differentiation proceeds.

• TeideRelated: Magma storage beneath Teide helps drive its eruptive activity.

• Complex volcanoRelated: Changing magma storage can redirect eruptions among different vents.

• Île Saint-PaulRelated: Magma accumulation and withdrawal can contribute to volcanic collapse that forms calderas.

• MenengaiRelated: Withdrawal of magma from beneath a volcano can trigger caldera collapse.