Earthquake is the result of a sudden release of energy in the Earth's crust that creates seismic waves.
Tectonic earthquakes will occur anywhere within the earth where there is sufficient stored elastic strain energy to drive fracture propagation along a fault plane.
There are three main types of fault that may cause an earthquake: normal, reverse (thrust) and strike-slip. Normal and reverse faulting are examples of dip-slip, where the displacement along the fault is in the direction of dip and movement on them involves a vertical component. Normal faults occur mainly in areas where the crust is being extended such as a divergent boundary. Reverse faults occur in areas where the crust is being shortened such as at a convergent boundary. Strike-slip faults are steep structures where the two sides of the fault slip horizontally past each other ; transform boundaries are a particular type of strike-slip fault. Many earthquakes are caused by movement on faults that have components of both dip-slip and strike-slip; this is known as oblique slip.
Earthquakes often occur in volcanic regions and are caused there, both by tectonic faults and the movement of magma in volcanoes. Such earthquakes can serve as an early warning of volcanic eruptions.
seismic unit
earthquakes usually occur at tectonic plate boundaries
Earthquakes
yes earthquakes happen at all types of plate boundaries but most of them occur at destructive, collisional, and conservative plate boundaries
More Earthquakes occur on land.
seismic unit
seismic unit
These are known as aftershocks.
The lithosphere is where earthquakes occur.
Earthquakes occur at all plate boundaries.
Earthquakes and volcanoes both occur in land and ocean. =)
Most earthquakes do occur on fault lines.
Yes that is generally where most earthquakes occur
Most earthquakes occur where the edges of Earth's plates are.
earthquakes usually occur at tectonic plate boundaries
Earthquakes
yes earthquakes happen at all types of plate boundaries but most of them occur at destructive, collisional, and conservative plate boundaries