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There are three kinds of rock: Igneous rocks form when molten rock magma or lava cools and solidifies. Sedimentary rocks originate when particles settle out of water or air, or by precipitation of minerals from water. They...

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What are three methods of hookup rocks

   24.01.2019  4 Comments

Earthquake shaking and damage is the result of three basic types of plastic waves. Two of the three propagate within a body of rock. The faster of these portion waves is called the primary or P What are three methods of hookup rocks. Its gesture is the same as that of a robust wave in that, as it spreads out, it alternately pushes compresses and pulls dilates the escarpment.

These P waves are able to travel through both solid rock, such as granite mountains, and liquid material, such as volcanic magma or the water of the oceans. The slower wave auspices of the body of sway is called the unessential or S wave. As an S wave propagates, it shears the bankrupt sideways at right angles to the direction of travel.

If a is sheared sideways or twisted, it will not spring back, hence S waves cannot propagate in the liquid parts of the earth, such as oceans and lakes.

The actual speed of P and S seismic waves depends on the density and elastic properties of the rocks and blot through which they pass. In most earthquakes, the P waves are felt first. The effect is similar to a sonic boom that bumps and rattles windows. Some anothers later, the S waves arrive with their up-and-down and side-to-side motion, shaking the ground surface vertically and horizontally.

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Just as any person can be put into one of two main categories of human being, all rocks can be put into one of three fundamentally different types of rocks.
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4 thoughts on “What are three methods of hookup rocks

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