The three types of plate boundaries are:
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Divergent Boundaries:
- At divergent boundaries, tectonic plates move away from each other. This movement creates space for magma to rise from the mantle, leading to the formation of new crust. Divergent boundaries are often associated with mid-ocean ridges, where oceanic plates pull apart, and can also occur on land, creating rift valleys.
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Convergent Boundaries:
- Convergent boundaries occur when two tectonic plates move toward each other. This movement can result in one plate being forced beneath another in a process called subduction. Depending on the type of plates involved (continental or oceanic), convergent boundaries can lead to the formation of mountain ranges, deep ocean trenches, or volcanic arcs.
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Transform Boundaries:
- At transform boundaries, tectonic plates slide past one another horizontally. The movement is typically characterized by friction, causing earthquakes along fault lines. Transform boundaries do not create or destroy crust but can significantly impact the geography of the regions they traverse, often resulting in the formation of linear valleys or offsets in landforms.
Each of these boundary types plays a crucial role in the dynamics of Earth's geology and the formation of its surface features.