Along the San Andreas Fault line.
At divergent and transform boundaries.
On tectonic plate boundaries. The transform boundaries. :P
Earthquakes can, and do, occur at divergent, convergent, and transform plate boundaries.
An earthquake can occur at divergent, convergent, or transform plate boundaries. However, transform boundaries are most commonly associated with earthquakes due to the intense stress caused by the plates sliding past each other.
Most present-day faults occur along boundaries. The three types of geologic boundaries are transform boundaries, divergent boundaries and convergent boundaries.
transform and divergent
They occur near ocean ridges. (Information is from BCScience10)
Earthquakes can occur at tectonic plate boundaries, such as convergent boundaries where plates collide, divergent boundaries where plates move apart, and transform boundaries where plates slide past each other. The stress from the movement of these plates can cause the crust to fracture and release energy in the form of an earthquake.
The mid-ocean ridge does not occur along transform boundaries. It is a divergent boundary where two tectonic plates move apart, allowing magma to rise up and create new oceanic crust. Transform boundaries are where plates slide past each other horizontally.
Earthquakes commonly occur at transform boundaries. These boundaries are where two tectonic plates slide past each other horizontally, creating friction that eventually releases as seismic energy, causing earthquakes.
At transform plate boundaries, processes like subduction and seafloor spreading do not occur. Instead, these boundaries are characterized by the sliding past of two tectonic plates horizontally. There is no creation or destruction of crust at transform boundaries, only sideways movement.
The three types of convergence are convergent boundary, divergent boundary, and transform boundary. Convergent boundaries occur when tectonic plates collide, divergent boundaries occur when tectonic plates move away from each other, and transform boundaries occur when tectonic plates slide past each other horizontally.