Earth's tectonic plates meet at boundaries called plate boundaries. These boundaries are not smooth lines, but rather complex zones where the plates interact.

Here are the three main types of plate boundaries:

* Divergent Boundaries: Plates move apart from each other. This is where new crust is formed, usually in the form of mid-ocean ridges or rift valleys.

* Convergent Boundaries: Plates move towards each other. This is where one plate is forced beneath the other (subduction) or where the plates collide and crumple (continental collision). These boundaries are responsible for mountain ranges, volcanoes, and earthquakes.

* Transform Boundaries: Plates slide past each other horizontally. This creates friction and can cause earthquakes.

Here's a simple breakdown:

* Divergent: Think of two cars pulling away from each other.

* Convergent: Think of two cars driving towards each other.

* Transform: Think of two cars passing each other on a highway.

You can find more information about the specific locations of different plate boundaries by searching online for "tectonic plate map".