Linked from

The 48 pages that link to Subduction zone, each with the reason it gives.

• StratovolcanoRelated: Many stratovolcanoes form above descending oceanic plates that release water into the mantle.

• TsunamiRelated: Large earthquakes at subduction zones commonly produce the strongest ocean-wide tsunamis.

• SerpentinizationRelated: Hydrated ultramafic rocks can carry water into subduction systems.

• Decompression meltingRelated: Water released from descending slabs commonly promotes flux melting rather than decompression melting.

• Gravity anomalyRelated: Trenches and dense descending slabs create characteristic gravity signals.

• VolcanoRelated: Water released by sinking plates helps generate magma beneath volcanic arcs.

• Sierra Nevada batholithRelated: Subduction supplied water and helped generate the arc magmas that formed its plutons.

• AmphiboliteRelated: Subducted mafic rocks can undergo pressure-temperature histories that produce amphibolite.

• DioriteRelated: Water released from a descending slab can generate magmas that crystallize into diorite.

• TonaliteRelated: Many tonalites form in magmatic arcs above subducting plates.

• ActinoliteRelated: Water released from descending oceanic crust helps drive metamorphic reactions that can produce actinolite.

• Mount DamavandRelated: Regional plate convergence contributes to the tectonic conditions associated with Iranian volcanism.

• SerpentiniteRelated: Water released around subduction zones can alter mantle rocks into serpentinite.

• BatholithRelated: Many batholiths form above subduction zones as water-rich magmas rise through continental crust.

• GreenschistRelated: Subduction can bury and metamorphose basaltic crust into greenschist.

• HeklaRelated: Subduction beneath Iceland contributes to the magma feeding Hekla.

• Serpentine subgroupRelated: Water released in subduction settings can hydrate mantle rocks and form serpentinites.