* Faults: These are breaks in the Earth's crust where movement occurs.
* Tension: The Earth's tectonic plates pull apart, causing the crust to stretch and crack along fault lines.
* Block Movement: One block of crust slides down relative to the other, creating a steep, uplifted block (the mountain) and a lower block (the valley).
Key Characteristics of Fault-Block Mountains:
* Steep, vertical slopes: The uplifted block creates a sharp, almost cliff-like face.
* Flat tops: The mountaintop often retains its original, relatively flat surface.
* Linear arrangement: Fault-block mountains tend to line up along the fault line, creating a series of parallel peaks and valleys.
Examples:
* Sierra Nevada Mountains (California): A classic example of a fault-block range.
* Wasatch Range (Utah): Another prominent example in the western United States.
* Vosges Mountains (France): An example in Europe.
So, yes, mountains formed by huge rocks separated by faults are definitely mountains, specifically fault-block mountains.
