What is a common result of tectonic plate movement?

The movement of tectonic plates is a fundamental process that shapes the Earth's surface. When tectonic plates interact, they can create a variety of geological features and events. One of the most notable results of this movement is the formation of mountains. For instance, when two continental plates collide, they can force the crust upwards, leading to mountain ranges like the Himalayas.

Additionally, tectonic plate movements are a primary cause of earthquakes. These seismic events occur when there is a sudden release of energy in the Earth's crust due to the plates slipping past each other, colliding, or moving apart. This release of energy generates seismic waves, resulting in earthquakes that can be felt across large distances.

In contrast, static land formations refer to geological structures that do not change, which is not true of areas affected by tectonic activity. Flat plains and deserts or lakes may develop in certain geological conditions, but they are not direct results of tectonic plate movements. Thus, the association of mountains and earthquakes with tectonic plate movement embodies the dynamic nature of our planet's geology.