The earth's mantle will not change in the future because this region is safe from the intervention of human beings.
<h3>What happens in the Earth's mantle?</h3>
The transfer of heat and material in the mantle helps us to determine the landscape of Earth. Activity in the mantle moves the plate tectonics, that contributes to volcanoes, seafloor spreading, earthquakes, and building of mountains.
So we can conclude that The earth's mantle will not change in the future because this region is safe from the intervention of human beings.
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The
answer is c. shear
When earthquakes occurs, rocks are constantly exposed to forces
known as stress which cause deformation of rocks that tend to bend, twist, or
fracture them. The respond to stress that result to changes in shape, size, or
volume are referred to as strain.
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If stress act
equally from all directions, the applied force is a uniform stress. However,
if stress is not equivalent from all directions then it is a
differential stress. Moreover, there are various kinds of differential stress namely,
tensional stress that causes the rock to stretch, the compressional stress
that squeezes the rock and the shear stress which is a consequence of
slippage, twisting or transformation of rocks.
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Answer:
Option D.
Explanation:
Scientific method is the method of experimentation that is used in science to explore observations and answers to questions on natural world. It involves making observations, formulating hypothesis and conducting scientific experiments.
Scientific processes is the end result of scientific method. It involve step by step approaches use to carry out scientific experiments about natural world.
The answer is; fossil
Fossil is defined as any dead organism ( or its trace or impression) of a past geological time that is naturally preserved in the earth in geological features such as rocks, bogs, and etcetera. Coral reef is no exception because it is considered a living organism. It is composed of colonies of coral polyps and algae that secrete a carbon carbonate skeleton.