the elastic rebound theory
stress builds up on a fault line over time and then releases all of the stress in an earthquake.
an earthquake
Yes, this is a very good description of the cause of an earthquake.
A build up of stress. As the plates move past each other or one moves under another, the edges of the plates get locked up. This is because the edges of the plates are not smooth but jagged. Eventually so much stress builds up that the plates "pop" past each other releasing a huge amount of energy in the form of an earthquake
Aftershocks are smaller earthquakes that occur after a larger event (the mainshock) in the same area. If an even larger earthquake occurs, then the original mainshock becomes a foreshock and the bigger event becomes the mainshock.
stress builds up on a fault line over time and then releases all of the stress in an earthquake.
The fault locks, and stress builds up until an earthquake occurs.
When that happens a earthquake is produced.
It is when two plates in the earth because of the release of stress or tension in the earth's lithosphere.
The place in the Earth's crust where stress is released during an earthquake is called the focus or hypocenter. It is the point underground where the rupture of the fault occurs and energy is released in the form of seismic waves. This is the actual source of an earthquake.
earthquake
The great San Francisco earthquake happened in 1906 and not in 1902. The type of stress was a strike-slip stress.
Most earthquakes occur as a result of "stick-slip" behavior. As two plates move past each other they stick to each other along the fault and build up stress. Eventually the plates slip along part of the fault, releasing that stress as an earthquake. The longer part of a plate goes without an earthquake, the more stress builds up, and the more energy is available for a large earthquake. Scientists think these seismic gaps are areas where the plates have been stuck for a long time and so have built up stress for a very large earthquake.
Suddenly builds up
an earthquake
We determine the scaling relationships between earthquake stress drop and recurrence.
It is called tectonic stress.