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Guided Notes on the Theory of Plate Tectonics

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Continent/Continent Convergent Plate Boundary: When two continental plates collide, neither plate is as dense as the mantle below. Therefore, neither plate dives below the other. They smash together, pushing crust up and down, and creating a tall mountain range. The Himalayas were formed in this way. Tall, non-volcanic mountains Earthquakes caused by crumpling and cracking of plates due to collision

Continent/Continent Convergent Plate Boundary: an example

https://sites. google. com/a/abschools https://sites.google.com/a/abschools.org/ms-broadwater-s-web-page/geology/mid-ocean-ridges-and-subduction