Tectonic Plates are made of two types of crust - Continental and Oceanic.
- Continental crust is thicker and less dense.
- Oceanic crust is thinner and more dense.
The plates are moving due to convection currents taking place in the the rock in the mantle underneath them.
The places where plates meet are called boundaries or plate margins.
- North American Plate
- Eurasian Plate
- Pacific Plate
- Indo-Australian Plate
- South American Plate
- African Plate
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