Linked from

The 195 pages that link to Plate tectonics, each with the reason it gives.

• Radiometric datingRelated: Radiometric ages constrain the timing of crust formation, magmatism, and tectonic activity.

• BiogeographyRelated: The acceptance of drifting continents transformed biogeography from descriptive to historical.

• CretaceousRelated: Plate motion broke apart continents and opened oceans during the Cretaceous.

• 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.

• Mantle convectionRelated: The surface expression that convection was invoked to explain.

• 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.

• UniformitarianismRelated: Present plate motions help reconstruct ancient continents and ocean basins.

• Earth's mantleRelated: Mantle flow and sinking lithosphere help drive and accommodate plate motion.

• GeographyRelated: Plate motion creates landforms and hazards that structure physical environments.

• OphioliteRelated: It supplied a tectonic framework for oceanic rocks found within mountain belts.

• SeamountRelated: Plate motion transports seamounts away from volcanic sources and can later subduct them.

• GeologyRelated: Plate motion links many large-scale changes in Earth’s crust and surface.

• GeophysicsRelated: It provides the large-scale framework for interpreting tectonic deformation and seismicity.

• PrecambrianRelated: Its early history shaped continents, oceans, and the recycling of surface materials.

• Deep timeRelated: Plate motions rearrange continents and ocean basins over millions of years.

• GeomorphologyRelated: Plate motion creates uplift, subsidence, and structural relief that surface processes modify.

• Physical geographyRelated: Plate motion builds mountains, opens ocean basins, and drives earthquakes and volcanism.

• Elastic-rebound theoryRelated: Plate motion drives the tectonic loading that strains faults.

• Pilbara CratonRelated: Whether modern-style plate tectonics operated during Pilbara crust formation remains debated.

• Isua Greenstone BeltRelated: Isua’s structures and rock associations inform debates over when modern-style plate tectonics began.

• GlossopterisRelated: It explains the ancient continental movements that continental drift proposed.

• Rare Earth hypothesisRelated: Carbon cycling through tectonics is proposed as one stabilizer of Earth’s long-term climate.

• Foreland basinRelated: Converging plates commonly build the mountain belts associated with foreland basins.

• Carbonate–silicate cycleRelated: Tectonics controls much of the burial, uplift, and volcanic return of carbon.

• MountainRelated: Colliding and separating plates create many mountain belts.

• Paradigm shiftRelated: Its adoption unified previously separate geological observations into a new explanatory framework.

• Prince Edward IslandsRelated: The islands’ volcanic setting reflects processes at the boundary between major oceanic plates.

• ProterozoicRelated: Continental rearrangements influenced Proterozoic climate, ocean circulation, and nutrient supply.

• Satellite geodesyRelated: Long GNSS time series measure plate velocities and test models of tectonic motion.

• Vine–Matthews–Morley hypothesisRelated: The hypothesis made seafloor spreading measurable, giving plate tectonics its quantitative foundation.

• Wadati–Benioff zoneRelated: Provided the explanation, decades later: the dipping zones are sinking slabs.

• Nature (natural world)Related: It accounts for the slow formation and reshaping of continents and ocean basins.

• Earth scienceRelated: Plate motion links earthquakes, mountain building, and ocean-basin change.

• Intrusive rockRelated: Intrusive rocks record magma generation in settings such as subduction zones and continental collisions.

• Mantle viscosityRelated: Mantle viscosity influences how forces from mantle flow and subduction are transmitted to plates.

• Nuvvuagittuq Greenstone BeltRelated: Claims of very ancient rocks raise questions about when recognizable tectonic processes began.

• ArchipelagoRelated: Plate motion creates many volcanic and uplifted island chains.

• FlyschRelated: Plate tectonics explains flysch basins through convergence, crustal loading, and sediment routing.

• New Zealand biogeographyRelated: Plate movements formed New Zealand’s landforms and altered connections with neighboring regions.

• PaleoarcheanRelated: Whether modern-style plate motion operated during the Paleoarchean remains central to reconstructing its crust.

• PeninsulaRelated: Plate motion can uplift or deform land that forms a peninsula.

• Biogeographic realmRelated: Continental movement altered connections and separations among the ancestors of realm biotas.

• Internal structure of EarthRelated: Mantle heat and deformation sustain the motion of the lithospheric plates.

• NothofagusRelated: Continental movement provides one framework for interpreting southern plant distributions.

• EoarcheanRelated: Whether modern-style plate tectonics operated in the Eoarchean remains debated.

• Historical geologyRelated: Plate motions explain the changing positions of continents and the formation of ancient rocks.

• History of EarthRelated: Plate movement builds continents, opens oceans, and drives much of Earth’s geological history.