what are the different types plate boundaries?
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There are three kinds of plate tectonic boundaries: divergent, convergent, and transform plate boundaries. This image shows the three main types of plate boundaries: divergent, convergent, and transform.
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The Earth's crust can be pictured like an egg shell, fractured into many sections, which we call tectonic plates. There are three types of plate boundaries: convergent, divergent and transform. Convergent boundaries are where two plates are moving towards each other, and this is where subduction zones can be created.
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Himalayan Mountains are an example of a Continent-Continent convergent plate boundary where two slabs of continental crust have collided and compressing the crust and the acretionary wedge material and lifting it to form the Himalayan Mountains. Indonesia is another example of an Ocean-Ocean convergent plate boundary.
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The image shows the Convergent plate boundary. Explanation: Convergent boundaries occur wherever the Earth's tectonic plates move or collide toward each other.
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This is a special type of convergent boundary called a collisional boundary. The Himalayas in India are the result of two continental plates (the Indo-Australian and Eurasian plates) colliding head on. The third type of plate boundary is called a conservative or transform boundary.
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Tectonic Plate Boundaries The Pacific Plate (on the west) slides horizontally northwestward relative to the North American Plate (on the east), causing earthquakes along the San Andreas and associated faults. The San Andreas fault is a transform plate boundary, accomodating horizontal relative motions.
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When two plates are moving away from each other, we call this a divergent plate boundary. Along these boundaries, magma rises from deep within the Earth and erupts to form new crust on the lithosphere. Most divergent plate boundaries are underwater and form submarine mountain ranges called oceanic spreading ridges.
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Divergent plate boundaries. One young divergent plate boundary that you'll recognize is actively forming the Red Sea. Although the Arabian penninsula and Africa were once linked to form a single continent, they are now being ripped apart.
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['Convergent boundaries: where two plates are colliding. Subduction zones occur when one or both of the tectonic plates are composed of oceanic crust. ... ', 'Divergent boundaries – where two plates are moving apart. ... ', 'Transform boundaries – where plates slide passed each other.']
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Most of the Earth is covered by seven major plates and another eight or so minor plates. The seven major plates include the African, Antarctic, Eurasian, North American, South American, India-Australian, and the Pacific plates. Some of the minor plates include the Arabian, Caribbean, Nazca, and Scotia plates.
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Convergent boundary types include oceanic/oceanic, oceanic/continental and continental/continental.
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The edges of tectonic plates are called boundaries. There are three types of these boundaries: divergent (where tectonic plates move away from each...
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The three types of convergent plate boundaries include oceanic-continental convergence, oceanic-oceanic convergence, and continental-continental...
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Answer Expert Verified The San Andreas fault is an example of Transform tectonic plate boundary.
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A convergent boundary is an area on Earth where two or more lithospheric plates collide. One plate eventually slides beneath the other causing a process known as subduction. ... Convergent boundaries occur between oceanic-oceanic lithosphere, oceanic-continental lithosphere, and continental-continental lithosphere.
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['Divergent: extensional; the plates move apart. Spreading ridges, basin-range.', 'Convergent: compressional; plates move toward each other. Includes: Subduction zones and mountain building.', 'Transform: shearing; plates slide past each other. Strike-slip motion.']
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Each of these types of plate boundaries is associated with different geological features. Typically, a convergent plate boundary—such as the one between the Indian Plate and the Eurasian Plate—forms towering mountain ranges, like the Himalaya, as Earth's crust is crumpled and pushed upward.