what causes earthquakes to occur?

Read about place tectonics in this article.

http://en.wikipedia.org/wiki/Earthquake

Yes

Earthquakes are caused by the sudden release of energy in the Earth's crust, resulting in seismic waves that shake the ground. This release of energy is usually triggered by the movement of tectonic plates, which are large pieces of the Earth's lithosphere that float on the semi-fluid asthenosphere below.

To understand what causes earthquakes, you first need to know about plate tectonics. The Earth's crust is divided into several large and smaller plates that are continuously moving. Where these plates interact, earthquakes are more likely to occur. There are three main types of plate boundaries:

1. Convergent Boundaries: Here, two plates are moving towards each other. When an oceanic plate collides with a continental plate, the denser oceanic plate subducts beneath the less dense continental plate, creating a subduction zone. The friction and pressure between the plates can build up over time, causing strain and stress to accumulate. Eventually, the pressure becomes too great, and the accumulated energy is released in the form of an earthquake.

2. Divergent Boundaries: At these plate boundaries, two plates are moving away from each other, creating a gap. As the plates separate, magma rises from the mantle to fill the gap, solidifying and forming new crust. However, the process is not always smooth, and the separation can be accompanied by volcanic activity and earthquakes as the crust fractures and adjusts to the stretching forces.

3. Transform Boundaries: Here, two plates slide past each other horizontally. As they move, the plates can become locked due to friction, causing stress to accumulate. When the stress overcomes the friction, the plates suddenly slip, causing an earthquake. The San Andreas Fault in California is a well-known example of a transform boundary.

It's important to note that earthquakes can also occur within plates, away from plate boundaries, but these intraplate earthquakes are relatively less common and generally associated with geological features like faults or hotspots.

To monitor and predict earthquakes, scientists use seismographs to measure seismic waves and collect data on the location, depth, and magnitude of earthquakes. Studying the patterns of earthquakes and the movement of tectonic plates helps in understanding the causes and predicting future seismic activity.