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This is what divides the mantle and the crust into these three sphere layers. At the lower part of the mantle (depth 2883km-350km) there exists a region of high temperature and high strength, this is known as the mesosphere or middle sphere, then at a depth of 350-100km there is a sphere with balance of temperature and pressure (leaving rocks with little strength) called the asthenosphere or weak sphere which has a plastic nature, and finally there is the region from 100km to the Earth's surface called the lithosphere...
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The rocks in the lithosphere are more rigid, cooler and stronger than the plastic asthenosphere.
Fig 1 ? The sliced view of the Earth identifying the layers and spheres.?
Now that the Earth's interior has been identified and separating into regions the question to be ask is ? how was it determined?'
GEOLOGICAL OBSERVATIONS
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