Tectonic uplift refers to the geologic process of raising the Earth's crust, leading to the elevation of landforms. This process is typically associated with tectonic plate movements, including both the collision and separation of plates. When tectonic plates converge, the intense pressure and force can lead to the uplift of mountain ranges and the formation of fold mountains. Conversely, when plates diverge, the stretching and thinning of the crust can result in the uplift of volcanic mountain ranges and the creation of rift valleys.
The primary causes of tectonic uplift include:
Tectonic uplift has a range of significant effects on the Earth's surface and environment, including:
To better understand tectonic uplift, consider the following study guide: