Want this question answered?
one of the major faults are that there was an open circuit on the windings.
Deep furrows in the ground or ocean floor are faults. San Andreas fault in California is a prime example, having displacement hundreds of kilometers long. Two kinds of faults are dip-slip faults and strike-slip faults.
No. They used to be some of the most active geologic areas. To give an example, that region erupted for 1 million years at full force. If they were to become active, it would be the end of the world as we know it.
No. Your terminology is close but not quite right. The three main types of faults are normal faults, reverse faults, and strike-slip faults. Strike-slip faults may also be called transform faults.
Active faults can generate earthquakes and represent sources of seismic energy. Inactive faults can no longer generate earthquakes but did so in the past. +++ They can, but really the earthquake is the effect of the movement on the fault, so not the defining mechanism. ' An active fault is one still moving (albeit usually in small, irregular steps over millions of years); an inactive fault is stable. If a new phase of tectonic stresses arrive, an inactive fault can be 're-activated', in many cases with the movement in the opposite direction. A fault is a fracture with displacement, and that movement is of the rock on one side of the fault-plane across the other.
OK!over 99 active faults!
because tectonic plates actively move and shift along faults
By locating where faults are active and where past earthquake have occurred.
You will find active faults and, if the margin is convergent, volcanoes.
focus
one of the major faults are that there was an open circuit on the windings.
They can't be predicted and that is the problem. Geologists monitor active faults for signs of movement.
An example of a normal fault is the Great Rift Valley of Africa.
San Andreas Fault
gap hypothesis
gap hypothesis
the san andreas fault