Earthquakes are primarily caused by the movement of tectonic plates along faults, which are fractures in the Earth's crust. When the stress on these faults exceeds the strength of the rocks, they slip, releasing energy in the form of seismic waves. This sudden release of energy is what we perceive as an earthquake. The most common types of faults associated with earthquakes are strike-slip, normal, and reverse faults.
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The Hayward Fault is a Strike-slip Fault.
The fault that caused the 1995 Kobe earthquake was the Nojima fault.
A reverse fault is formed here
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.
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Earthquakes are measured in machine called 'Seismograph', the range of which is calculated in Richter scale. Further, the epicenter of the earthquake can also be confirmed by the above machine.
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Movement and proximity of the moon
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