Answer:
just tryin' to help you
The tectonic plates are always slowly moving, but they get stuck at their edges due to friction. When the stress on the edge overcomes the friction, there is an earthquake that releases energy in waves that travel through the earth's crust and cause the shaking that we feel.
Gondwana<span> was an ancient supercontinent that broke up about 180 million years ago.</span>
Asia Minor
Hope it helped.
Answer:
idk thats a good question
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