a quake.
At convergent boundaries, plates do not slide past each other. Instead, they move towards each other and collide or subduct under one another. This collision or subduction process is what characterizes convergent plate boundaries.
they are less likely to happen at the center of Earth's plates because the plates collide in the front or in the back and unless a plate is the middl3e and another is moving to its center it well most likey not hit its center.
Earthquakes can occur along tectonic plate boundaries, where the plates are in motion and often collide or slide past one another. The most active areas for earthquakes are along the Pacific Ring of Fire and along mountain ranges like the Himalayas. However, earthquakes can also occur in areas where there are underground faults or volcanic activity.
Tectonic plates slide past each other at transform plate boundaries. This movement can result in earthquakes as the plates grind against each other. Examples of transform plate boundaries include the San Andreas Fault in California and the Alpine Fault in New Zealand.
An earthquake will most likely occur because the techtonic plates below the earth's surface are grinding past one another causing severe shaking.
an earthquake
an earthquake
earthquakes happen because plates connect and slip past each other
An Earthquake occurs.
San Andreas
Transform Boundary.
earthquakes happen
When shearing causes areas between plates that are sliding past one another to form faults.
Most earthquakes happen at the edge of tectonic plates, where the plates are colliding or sliding past each other. These areas are known as plate boundaries, and the stress and friction from the movement of the plates can lead to earthquakes.
Transform
plates sliding past each another
A transform fault is created.