Earthquake belts
in the world
Circum-Pacific belt:
This follows the region around the Pacific Ocean from Japan, China,
Alaska Aleutians, California (San Andreas fault system),
Mexico, Equador, Peru, Chile and New Zealand. These
are the areas characterized by plate subduction, active volcanoes, strain
build-up and periodic release, causing earthquakes.
•
Mid-Atlantic Ridge: This follows the
lines of Mid-Oceanic Ridges from near the North Pole to the equator, turning around
South Africa and ends up to Rift Valley region of East Africa. Seismicity is
low in this region.
•
The Alpine-Himalayan Trans-Asiatic Belt:
The Alpine mountain areas of Europe, North Africa, Asia Minor, Caucasus,
Turkey, Iraq, Iran, Himalayan region such as Kashmir to Assam, Myanmar and
Philippines. This zone passes through boundaries of continental crustal plate
with high mountain ranges where intense compression takes place.
Elastic rebound
theory
Each type of plate
intersection produces significant straining in crustal rocks. The strain is
accumulated by gradual shifting of tectonic plates. The rocks become disturbed
but maintain their original positions because of continuity, mechanical bond
and friction. When accumulated stress finally exceeds the strength of rocks,
fracture occurs and the Earth shapes back in to an unstrained position. This
phenomenon is generally known as ‘elastic rebound theory’ or Reid’s theory.
The great release of energy associated with the rupture of rocks
produces shock waves that propagate through Earth’s crust and cause an
earthquake. The great (major) earthquakes are usually the transform fault and
subduction types. Sometimes, earthquakes are associated with volcanic eruptions
or subterranean movement of magma.
Related Topics
Privacy Policy, Terms and Conditions, DMCA Policy and Compliant
Copyright © 2018-2024 BrainKart.com; All Rights Reserved. Developed by Therithal info, Chennai.