FAULT DEFINITION IN GEOLOGY
Answer:
A fault refers to zone or fracture of cracks between two squares of rock. Faults permit the squares to move comparative with one another. Most faults produce rehashed removals throughout geologic time. During an earthquake, the stone on one side of the fault out of nowhere slips concerning the other. The fault surface can be even or vertical or some self-assertive point in the middle.
These are the different types of faults;
- Normal fault refers to a plunge slip issue in which the square over the fault has moved descending comparative with the square beneath.
- Thrust fault refers to a dunk slip fault in which the upper square, over the shortcoming plane, goes over-top the lower block.
- Strike-slip fault refers to a fault on which the two squares slide past each other.
- A left-lateral strike-slip fault is one on which the removal of the far block is to the left when seen from one or the other side.
- A right-lateral strike-slip fault is one on which the removal of the far block is to the right when seen from one or the other side.
What is fault what is different type of fault
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