Linked from

The 140 pages that link to Subduction, each with the reason it gives.

• Volcanic arcNarrower topic: The descending plate supplies the setting and materials that generate arc magma.

• Continental collisionNarrower topic: Oceanic lithosphere commonly subducts before the continents on either side collide.

• Lesser AntillesNarrower topic: Atlantic oceanic crust descends beneath the Caribbean plate along the arc.

• Mariana TrenchNarrower topic: The trench is the surface scar of the subduction zone that consumes the Pacific seafloor.

• Mount FujiNarrower topic: Subduction helps generate magma beneath the region where Fuji stands.

• Nazca PlateNarrower topic: The Nazca Plate’s eastward descent is a major example of this process.

• Philippine Sea PlateNarrower topic: Subduction defines much of the Philippine Sea Plate’s perimeter.

• Alpine orogenyNarrower topic: Subduction consumed oceanic crust during the approach of Africa and Eurasia.

• Island arcNarrower topic: The sinking oceanic plate supplies the water and tectonic setting that produce an island arc.

• Japan TrenchNarrower topic: The trench marks the surface expression of Pacific Plate subduction.

• South American PlateNarrower topic: This process accounts for much of the plate’s active western margin.

• Sunda TrenchNarrower topic: The trench is the surface expression of the plate descent occurring along this boundary.

• Farallon PlateNarrower topic: The Farallon Plate disappeared as it descended beneath the North American Plate.

• Juan de Fuca PlateNarrower topic: The plate's northeastward motion ends in descent beneath North America.

• Oceanic trenchNarrower topic: A descending plate bends the seafloor into a trench at a convergent boundary.

• Cocos PlateNarrower topic: The Cocos Plate’s descent beneath neighboring plates is a major example of this process.

• Izu–Bonin–Mariana arcNarrower topic: The arc is a direct product of Pacific Plate subduction.

• Accretionary wedgeNarrower topic: The descending plate supplies sediment and rock that the wedge incorporates.

• Andean orogenyNarrower topic: Subduction establishes the forces and melting processes behind the Andean margin.

• Wadati–Benioff zoneNarrower topic: Subduction produces the dipping slab whose earthquakes define the zone.

• Okhotsk PlateNarrower topic: Subduction at the plate’s eastern and southern edges generates earthquakes and volcanism.

• Peru–Chile TrenchNarrower topic: This plate-boundary process forms the trench and drives regional volcanism.

• Philippine SeaNarrower topic: Subduction at the sea’s margins creates trenches, earthquakes, and volcanic arcs.

• Slab rollbackNarrower topic: Rollback occurs within subduction but describes horizontal hinge motion, not descent itself.

• Trans-Mexican Volcanic BeltNarrower topic: This process drives melting beneath the belt and produces its magmas.

• Aleutian TrenchNarrower topic: Subduction bends the incoming plate and deepens the seafloor at the boundary.

• Apennine MountainsNarrower topic: Subduction in the western Mediterranean is part of the chain’s tectonic history.

• Central American Volcanic ArcNarrower topic: The arc is a classic landward volcanic chain produced above a subducting plate.

• Fuji-Hakone-Izu National ParkNarrower topic: Subduction beneath Japan supplies magma to the region’s volcanoes.

• Kuril–Kamchatka TrenchNarrower topic: The Pacific Plate sinks beneath the Okhotsk Plate, creating the trench.

• Mexican PlateauNarrower topic: Subduction beneath western Mexico contributes to regional volcanism and mountain building.

• Sagami BayNarrower topic: Plate convergence beneath the bay drives earthquakes and long-term seabed deformation.

• Variscan orogenyNarrower topic: Subduction consumed oceanic crust before continental blocks collided.

• Mount PeléeNarrower topic: Subduction beneath the Caribbean region supplies magma to Pelée and neighboring volcanoes.

• Rheic OceanNarrower topic: Subduction consumed oceanic crust along margins of the closing Rheic basin.

• Tonga TrenchNarrower topic: The sinking Pacific Plate is the process that forms and maintains the trench.

• Deep-focus earthquakeNarrower topic: Descending plates carry the cold, stressed rock in which most deep-focus earthquakes occur.

• Japanese island arcNarrower topic: Oceanic plates descend beneath Japan, generating earthquakes and the magma that feeds its volcanoes.

• Puerto Rico TrenchNarrower topic: Underthrusting at the trench is a shallow, complex form of plate convergence.

• Whole-mantle convectionNarrower topic: Subduction sends surface material downward and supplies the clearest candidate flow across the transition zone.

• Alaska PeninsulaNarrower topic: Pacific Plate subduction generates the magma feeding the peninsula’s volcanoes.

• Coast MountainsNarrower topic: Ancient subduction generated magma that contributed to the Coast Mountains’ bedrock.

• Italian PeninsulaNarrower topic: Subduction around Italy helps explain its active volcanic and earthquake zones.

• Izu IslandsNarrower topic: Pacific Plate subduction supplies the geological setting for Izu volcanism.

• Klyuchevskaya SopkaNarrower topic: The subduction of the Pacific Plate beneath the Okhotsk region helps supply Kamchatka’s magma.

• Kermadec IslandsNarrower topic: Pacific Plate subduction beneath the Australian Plate feeds the Kermadec volcanic arc.

• Median Tectonic LineNarrower topic: Subduction generated the contrasting metamorphic and magmatic belts flanking the fault.

• South Sandwich IslandsNarrower topic: Subduction beneath the island chain fuels its active volcanoes.

• Kronotsky Nature ReserveNarrower topic: Subduction beneath Kamchatka drives the volcanism that shapes the reserve.

• Paleo-Tethys OceanNarrower topic: Subduction consumed Paleo-Tethyan seafloor as the ocean narrowed.