moves up in respect to the footwall.
Finally, we have strike-slip faults! These ones do not move longitudinally, but rather they move parallel to each other in different directions.
Okay, first lesson! Tectonic plates, specifically faults! They come in many different forms!
Normal faults happen due to tension, and the hanging wall moves down in respect to the footwall.
Reverse faults happen when plates are compressed, and the hanging wall
+