Linked from
The 195 pages that link to Plate tectonics, each with the reason it gives.
SubductionNarrower topic: Subduction zones are the consuming boundaries that complete the plate-tectonic cycle.
Radiometric datingRelated: Radiometric ages constrain the timing of crust formation, magmatism, and tectonic activity.
Atlantic OceanNarrower topic: The movement of plates beneath the Atlantic determines its changing boundaries and ridge.
GondwanaNarrower topic: Plate tectonics explains how Gondwana assembled and later broke apart.
BiogeographyRelated: The acceptance of drifting continents transformed biogeography from descriptive to historical.
CretaceousRelated: Plate motion broke apart continents and opened oceans during the Cretaceous.
Seafloor spreadingNarrower topic: Spreading is the engine that made the full theory of plate tectonics cohere by 1968.
Tibetan PlateauNarrower topic: Plate motion explains the collision that raised the Tibetan region.
East African RiftNarrower topic: The parent theory that classifies the rift as a divergent boundary.
LithosphereRelated: Lithospheric plates move and interact through the processes described by this theory.
EndemismRelated: Plate movement can split ranges, join landmasses, and create isolated habitats over geological time.
Mid-ocean ridgeNarrower topic: Identifying ridges as divergent boundaries gave plate tectonics the geometry it needed to close.
Pacific PlateNarrower topic: The Pacific Plate is one of the largest moving pieces in this global system.
Subduction zoneNarrower topic: Subduction is one of the central processes by which tectonic plates interact.
Appalachian MountainsNarrower topic: Plate convergence explains the collisions that raised the Appalachians.
Mantle convectionRelated: The surface expression that convection was invoked to explain.
Continental driftCompared with: The successor that kept drift's continental motion but replaced its picture of plates versus ocean floors.
Volcanic islandNarrower topic: Plate motion determines where many island-building volcanoes form and how their chains develop.
MesozoicNarrower topic: It explains the Mesozoic breakup of Pangaea and the opening of ocean basins.
Eurasian PlateNarrower topic: It explains the motions and boundary interactions involving the Eurasian Plate.
VolcanismNarrower topic: Plate boundaries organize many of Earth's volcanic settings.
PaleozoicNarrower topic: Plate movement explains the era’s changing continents and eventual assembly of Pangaea.
Continental collisionNarrower topic: Continental collision is a consequence of plate convergence.
Late CretaceousNarrower topic: Continental rearrangement changed coastlines, ocean circulation, and migration routes.
Tethys OceanNarrower topic: Plate motions account for Tethys's opening, migration, and eventual disappearance.
CenozoicNarrower topic: Plate motion provides the physical framework for Cenozoic continental change.
OrogenyNarrower topic: Plate motions supply the forces behind most major mountain-building episodes.
PaleobiogeographyRelated: Plate motion changes the positions and connections of habitats through geological time.
EarthRelated: Plate motion builds continents, recycles crust, and drives earthquakes and volcanism.
ArcheanRelated: When and how modern-style plate tectonics operated during the Archean remain debated.
North American PlateNarrower topic: The plate’s boundaries and motion are explained by this global framework.
PaleogeographyNarrower topic: Its motions explain how continents and ocean basins change position through geological time.
Arabian PlateNarrower topic: The Arabian Plate is one moving unit within this global system.
UniformitarianismRelated: Present plate motions help reconstruct ancient continents and ocean basins.
JurassicNarrower topic: Plate motion drove the continental rifting that defined Jurassic geography.
Transform faultNarrower topic: Transforms supplied the missing third boundary type that completed the theory.
Hotspot volcanismNarrower topic: Hotspot tracks became a way to measure plate motion away from plate boundaries.
Continental riftingNarrower topic: Continental rifting is one way plate boundaries develop and reorganize.
African PlateNarrower topic: It provides the framework for explaining the African Plate’s boundaries and motion.
Mariana TrenchNarrower topic: The framework explaining why the trench exists where it does and how deep it can grow.
Wilson cycleNarrower topic: The cycle is the large-scale temporal pattern that plate tectonics explains.
Earth's mantleRelated: Mantle flow and sinking lithosphere help drive and accommodate plate motion.
Philippine Sea PlateNarrower topic: It provides the framework for describing the Philippine Sea Plate and its boundaries.
GeographyRelated: Plate motion creates landforms and hazards that structure physical environments.
Indian subcontinentNarrower topic: It explains the landmass’s movement and collision with Eurasia.
Megathrust earthquakeNarrower topic: Converging plates supply the long-term motion that loads megathrust faults.
OphioliteRelated: It supplied a tectonic framework for oceanic rocks found within mountain belts.
Wallace LineNarrower topic: It explains the deep channels and continental histories underlying the faunal divide.
Pacific IslandsNarrower topic: Plate motion explains the volcanic, seismic, and tectonic settings of many islands.
SeamountRelated: Plate motion transports seamounts away from volcanic sources and can later subduct them.