That's a good start, but not quite complete! While it's true that plate boundaries are where tectonic plates meet, it's more accurate to say that they are zones rather than just points.

Here's why:

* Tectonic plates aren't rigid: They are massive, but they can bend, flex, and break. This means the boundary isn't a single, sharp line.

* The boundary is a region of activity: At plate boundaries, you'll find earthquakes, volcanoes, mountain ranges, and other geological features that develop over a relatively broad area.

So, think of a plate boundary as a zone of interaction between two or more tectonic plates, rather than a single, fixed point.