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Plate tectonics is the theory explaining the movement of Earth’s lithospheric plates, which are rigid slabs of rock that float on the semi-fluid asthenosphere. Alfred Wegener's continental drift theory provides evidence for this concept, showcasing how continents like Pangaea gradually separated. Various plate boundaries include divergent, convergent, and strike-slip, each with unique movement patterns. For instance, divergent boundaries, found along mid-ocean ridges, cause plates to move apart, while convergent boundaries, near trenches, bring plates together. Fossils and geological formations offer further insight into this dynamic system.
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Plate Tectonics Mr. Skirbst Earth Science Topic 26
Plate Tectonics (lithospheric) plates
Plate Tectonics (lithospheric) plates (rock) slabs
Plate Tectonics (lithospheric) plates (rock) slabs tectonics
Plate Tectonics (lithospheric) plates (rock) slabs tectonics movement
Plate Tectonics movement of rocky slabs across the Earth
Plate Tectonics theory of continental drift Alfred Wegener
Plate Tectonics Earth’s continents are “floating” from one place to another
Plate Tectonics Evidence from fossils Glossopteris (found in S. Hemisphere)
Plate Tectonics Evidence from rocks mountains, shapes, deposits
Plate Tectonics Evidence from sea-floor sea-floor spreading mid-ocean ridge
Plate Boundaries Divergent boundary
Plate Boundaries Divergent boundary plates move apart
Plate Boundaries Divergent boundary plates move apart found along mid-ocean ridges
Plate Boundaries Divergent boundary plates move apart found along mid-ocean ridges called constructive boundary
Plate Boundaries Divergent boundary
Plate Boundaries Convergent boundary
Plate Boundaries Convergent boundary plates come together
Plate Boundaries Convergent boundary plates come together found near trenches
Plate Boundaries Convergent boundary plates come together found near trenches called destructive boundaries
Plate Boundaries Strike-slip boundary
Plate Boundaries Strike-slip boundary grind horizontally
Plate Boundaries Strike-slip boundary grind horizontally forms lateral faults
Plate Boundaries Strike-slip boundary grind horizontally forms lateral faults called a conservative boundary
Pangaea Large, single landmass that existed in the past before slowly breaking apart and moving into the current position