Plate Boundaries
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Plate Boundaries
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- PLATE BOUNDARIESPART 1
- Plate Boundaries are at the edges of Plate Tectonics. There are 3 types of Plate Boundaries: Transform, Divergent, and Convergent Boundaries. These boundaries are there for the different type o plate tectonics and crust.
- CONVERGENT BOUNDARY OO:
- There are two plates. The two plates come together. Subduction occurs between them. What I mean by subduction is that the most dense one will go under the less dense one. This forms a trench.
- MOSTDENSEPLATE
- LESS DENSEPLATE
- CONVERGENT BOUNDARY CC:
- The two plates come together. When they converge, neither is subjected and both plates buckle and move upwards. This forms either a mountain or volcanoes. Earthquakes can occur at convergent plate boundaries.
- CONVERGENT BOUNDARY OC:
- The same thing happens as a convergent boundary with oceanic and oceanic. You can find volcanic arcs near the subduction zone. You can also find continental volcanoes.
- MOST DENSE PLATE
- LESS DENSE PLATE
- TRANSFORM BOUNDARY:
- The 2 plates slide past each other. The crust is neither created or destroyed. Earthquakes will occur more when the plates slide past one another.
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