Consider the following statements regarding Oblique-Reverse Fault. An ...
Oblique-Reverse Fault is a type of geological fault characterized by both horizontal and vertical movement along the fault plane. Let's evaluate each statement given in the question:
Statement 1: An oblique-reverse fault is a geological fault characterized by only horizontal movement along the fault plane.
This statement is incorrect. Unlike normal faults where there is only vertical movement, and strike-slip faults where there is only horizontal movement, oblique-reverse faults involve both vertical and horizontal movement along the fault plane. Therefore, this statement is incorrect.
Statement 2: This type of faulting is common in areas of compression along the convergent plate boundaries.
This statement is correct. Oblique-reverse faults are indeed common in areas of compression along convergent plate boundaries. When two tectonic plates collide, the compressional forces can cause the rocks to be pushed together and uplifted, resulting in the formation of oblique-reverse faults.
Statement 3: The stress along these fault lines does not induce any earthquakes.
This statement is incorrect. The stress along oblique-reverse faults can induce earthquakes. Earthquakes occur when the accumulated stress along a fault exceeds the strength of the rocks, causing them to rupture and release energy. Since oblique-reverse faults involve significant movement along the fault plane, they can generate earthquakes of varying magnitudes.
In conclusion, only statement 2 is correct, while statements 1 and 3 are incorrect. Oblique-reverse faults are characterized by both horizontal and vertical movement, they are common in areas of compression along convergent plate boundaries, and they can induce earthquakes due to the accumulated stress along the fault lines.
Consider the following statements regarding Oblique-Reverse Fault. An ...
Only statement 2 is correct.
- An oblique-reverse fault is a geological fault characterized by both horizontal and vertical movements along the fault plane. This type of faulting is common in areas of compression along the convergent plate boundaries. The stress along these fault lines can induce earthquakes as rocks abruptly shift to release accumulated stress.
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