What do you think you would see at the plate boundary? Would you see the mantle? Why or why not?
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The Earth’s outer crust (the lithosphere) is composed of a series of tectonic plates that move on a hot flowing mantle layer called the asthenosphere. Heat within the asthenosphere creates convection currents that cause tectonic plates to move several centimeters per year relative to each other. When two tectonic plates meet, we get a “plate boundary.” There are three major types of plate boundaries, each associated with the formation of a variety of geologic features.
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Deep ocean trenches, volcanoes, island arcs, submarine mountain ranges, and fault lines
Explanation: -_-||
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