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seismic waves
seismic waves
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Strike-slip faults cause shearing
Earthquakes are typically caused by movement along a fault line, which is a fracture in the Earth's crust where rocks have shifted position relative to each other. The three main types of faults that can cause earthquakes are normal faults, reverse faults, and strike-slip faults.
There are 6 types of fault lines. Strike-slip faults, dip-slip faults, oblique- slip faults, listric faults, ring faults, and synthetic and antithetic faults.
The Eltanin and Romanche fracture zones are oceanic transform faults. These types of faults occur at the boundary between two tectonic plates where they slide past each other horizontally. The movement along these faults can cause earthquakes and contribute to the overall plate tectonics process
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Mainly transverse faults. This is caused by the way in which the sea-floor spreads, and the perpendicular faults slide past each other as the plates separate. The plates are moving away from each other, but as the divergence is not uniform and in a single line, faults are formed between the respective sides as a result of their movement. These faults are transverse as they move side by side. This is comparable to a Conservative plate boundary, but is not to be confused with it as this is not a tectonic boundary, but a fault.
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the answer is that compression is the kind of stress.
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