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Geologists can use seismographs to detect hidden faults. When seismic waves encounter a fault, they are reflected off of the fault. Geologists can use this information to chart the location of a depth of a hidden fault.
Vertical and horizontal
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Geologists use a tiltmeter to monitor the upward movement along a fault.
A blind thrust fault is a geological term for a type of thrust fault which does not appear on the surface - where a hanging wall makes an angle with the horizontal of less than 45 degrees, but is hidden from view.
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Horizontal faults can be refered to as lateral faults or strike-slip faults.
The dip of a unit represents the angle at which the bed inclines from the horizontal. In dip-slip faults, the fault blocks move up and down, parallel to the dip of the fault plane.
Geologists can use seismographs to detect hidden faults. When seismic waves encounter a fault, they are reflected off of the fault. Geologists can use this information to chart the location of a depth of a hidden fault.
It the angle between fault current and voltage at the point where the fault occurs.
Vertical and horizontal
normal fault
Strike-slip Fault