Dip-Slip fault is a bedding fault and its pattern is En-Echelon, while Strike Slip fault is strike fault and its pattern is Parallel.
Rocks can move along a fault in three main ways: 1) They can slide past each other horizontally in a strike-slip motion, 2) They can move vertically in a dip-slip motion, either upwards (reverse fault) or downwards (normal fault), or 3) A combination of strike-slip and dip-slip motion can occur in oblique faults.
When movement occurs along a strike-slip fault, the blocks of crust move horizontally past each other in a lateral direction, parallel to the fault plane. There are two main types of strike-slip faults: right-lateral and left-lateral, depending on the relative motion of the blocks. Earthquakes can occur along strike-slip faults as stress builds up and is released due to the movement of the blocks.
The normal fault, the thrust fault, the transcurrent fault , and the reverse fault.
The San Andreas Fault is a strike-slip fault, where two tectonic plates move horizontally past each other. The main force causing movement along the fault is the tectonic forces generated by the motion of the Pacific Plate relative to the North American Plate.
An upwarped mountain is formed by the uplifting of large blocks of Earth's crust without significant faulting. In contrast, a fault-block mountain is created by the displacement of blocks along faults, causing some blocks to be uplifted while others are dropped down. Ultimately, the main difference lies in the processes that lead to the formation of these mountain types.
Strike-slip Faults
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When rocks on opposite sides of a fault move in the same direction at different rates, it results in a strike-slip fault. This type of fault occurs when there is horizontal motion along the fault line. The two main types of strike-slip faults are left-lateral and right-lateral, depending on the direction of movement when facing the fault.
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There are 3 main types of faults 1. Normal 2. Strike slip 3. Reverse(Thrust) In a normal fault the foot wall stays in place while the hanging wall moves DOWNWARDS In a strike slip the tectonic plate(s) slide past each other horizontally In a reverse fault, the hanging wall gets pushed UPWARDS over the foot wall (The pictures are in the reverse order)
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Rocks can move along a fault in three main ways: 1) They can slide past each other horizontally in a strike-slip motion, 2) They can move vertically in a dip-slip motion, either upwards (reverse fault) or downwards (normal fault), or 3) A combination of strike-slip and dip-slip motion can occur in oblique faults.
When movement occurs along a strike-slip fault, the blocks of crust move horizontally past each other in a lateral direction, parallel to the fault plane. There are two main types of strike-slip faults: right-lateral and left-lateral, depending on the relative motion of the blocks. Earthquakes can occur along strike-slip faults as stress builds up and is released due to the movement of the blocks.
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