Answer:
The answer is Thrust fault.
Explanation:
Blame, in geography, a planar or precisely bent break in the stones of the Earth's outside layer, where compressional or tensional powers cause relative dislodging of the stones in spite of what may be normal sides of the split. Flaws go long from a couple of centimeters to innumerable, and development other than may continue running from not as much as a centimeter to two or three hundred kilometers along the break surface (the blame plane). In a few cases, the change is scattered over a blame zone made out for different individual charges that have a belt a couple of meters wide. The geographic distribution of blemishes fluctuates; some expansive zones have none, others are cut by endless needs.
A reverse fault occurs when convergent motion forces rocks to move upward along the fault.
Faults simply mean fractures in the earth’s crust in which the rock from any sides of the cracks are no longer beside each other. In other words, it means the rock from both sides of crack has moved past each other.
In some cases, the cracks can be tiny and show no movement within the rock layers.
However, there are three different types of faults and these include
Strike-slip fault is a fault in which the two block slides horizontally move pass each other. That is, the rocks are moving past each other horizontally.
Normal fault create space between the rocks, it is also the opposite of reverse faults. A popular place where normal faults spread earth crusts apart is the range province within North America.
Thrust (reverse) fault is a faults that take place when the upper block which is directly above the fault plane move pass the lower block. Reverse faults are very common, especially in the area of compression.
Strike-slip faults are mostly vertical while the two other types of faults are usually at an angle towards the earth's surface.
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