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Published byBrandon Richard Modified over 9 years ago
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Types of Plate Boundaries After completing this section, students will identify that the Earth is made of geologic plates (Standard PI-041) and investigate the types of plate boundaries (Standard PI – 043)
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According to geologists, the Earth’s crust is broken into moving sections called plates. The plates move toward each other, move away from each other, or move past each other
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Scientists classify plate boundaries according to how they move. There are three types of plate boundaries Divergent Boundaries Convergent Boundaries Transform Boundaries
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Divergent Boundaries
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Divergent boundary – boundary between two plates that are moving apart Also known as spreading centers
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Most divergent boundaries lie along the ocean floor and have rift valleys Rift valley – deep valley at the center of a mid-ocean ridge
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Molten rock forces its way upward through cracks along the valley The molten rock cools and forms new sea floor
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Convergent Boundaries
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Convergent boundaries are boundaries between 2 plates that are moving toward each other There are 2 classifications of convergent boundaries: subduction zones and collision boundaries
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Subduction zones occur when an oceanic plate slides beneath another plate Deep-sea trenches form at these boundaries, as well as chains of volcanic islands
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Subduction can also occur between an oceanic and a continental plate Mountain chains and volcanoes form at these boundaries
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Collision boundaries forms when 2 continental plates collide Mountains ridges form at these boundaries, like the Himalayas
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Transform Boundaries
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Transform boundaries occur when 2 plates slide past each other The San Andreas Fault is an example of a transform boundary
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