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Explore the structure of tectonic plates, comprising Earth's lithosphere with oceanic and continental crusts. Learn about their categorization into major, minor, and microplates, and the interactions at plate boundaries that lead to geological phenomena such as earthquakes and volcanic eruptions. Understand the role of different plate sizes in shaping the Earth's surface and their contribution to the planet's dynamic history.
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Tectonic plates are large, rigid slabs of Earth's lithosphere composed of the crust and uppermost part of the mantle
Oceanic Crust
Oceanic crust is thinner and more malleable than continental crust, composed of dense basaltic rocks rich in silicon and magnesium
Continental Crust
Continental crust is thicker and less dense than oceanic crust, composed of lighter granitic rocks rich in silicon and aluminum
Tectonic plates are classified as major, minor, or microplates based on their size and influence on global tectonics
Plate boundaries can be divergent, convergent, or transform, depending on the direction of plate movement
Divergent boundaries occur where plates move apart, creating new crust as magma rises from below the lithosphere
Convergent boundaries occur where plates move towards each other, resulting in subduction or mountain formation
Transform boundaries involve horizontal movement of plates alongside each other, often causing earthquakes
The Earth's major tectonic plates, such as the Pacific and Eurasian plates, have unique features and dynamics that shape the planet's surface
Major tectonic plates can be predominantly oceanic or continental and are responsible for shaping continents, influencing seismic and volcanic activity, and affecting biodiversity
The movement and interactions of major tectonic plates play a crucial role in shaping the Earth's surface and geological processes
Smaller tectonic plates, such as the Arabian and Juan de Fuca plates, have a significant impact on regional tectonics and seismic activity
Minor and microplates often interact with major plates, leading to complex tectonic processes and geological events
Over time, smaller plates can be accreted onto larger plates, contributing to the changing arrangement of tectonic plates throughout Earth's history