WHAT IS AN EARTHQUAKE BELT
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Seismic Belts are the narrow geographic zone on the Earth's surface along which most earthquake activity occurs. As the lithosphere is made up of several large tetonic plates.
The two major seismic belts are the Circum-Pacific Belt, which surrounds the Pacific Ocean, and the Alpide Belt, which stretches from the Azores through the Mediterranean and Middle East to the Himalayas and Indonesia, where it joins the Circum-Pacific Belt.
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