Normal faults
Hi, uh, ok, the Sierra Nevada Mountain Range wuz formed by 2 colliding plate boundaries tat collided and formed the Sierra Nevadas. thanks 4 reading!!!! - created by Lauren Eisele from Masuda Middle School
Hi, uh, ok, the Sierra Nevada Mountain Range wuz formed by 2 colliding plate boundaries tat collided and formed the Sierra Nevadas. thanks 4 reading!!!! - created by Lauren Eisele from Masuda Middle School
Fault Block mountains or Horst- formed when colliding plates build up pressure along parallel cracks (faults) in the Earth's surface. The extreme pressure causes large blocks of land to slip and be uplifted. Elevations are normally greater than 3000 meters above sea level. Example: The Sierra Nevadas of California.
Folding and lifting with some volcanic activity, as they were formed just inland of a previous subduction zone that was part of the ancient "pacific ring of fire". The rest of California formed later.
When plates within the Earth's crust bend and crack, faults are formed. Faults are fractures in the Earth's crust where movement has occurred along the break. These movements can be either vertical or horizontal, causing earthquakes.
Fault Block mountains or Horst- formed when colliding plates build up pressure along parallel cracks (faults) in the Earth's surface. The extreme pressure causes large blocks of land to slip and be uplifted. Elevations are normally greater than 3000 meters above sea level. Example: The Sierra Nevadas of California.
Fault Block mountains or Horst- formed when colliding plates build up pressure along parallel cracks (faults) in the Earth's surface. The extreme pressure causes large blocks of land to slip and be uplifted. Elevations are normally greater than 3000 meters above sea level. Example: The Sierra Nevadas of California.
swagg
reverse fault
Fault Block mountains or Horst- formed when colliding plates build up pressure along parallel cracks (faults) in the Earth's surface. The extreme pressure causes large blocks of land to slip and be uplifted. Elevations are normally greater than 3000 meters above sea level. Example: The Sierra Nevadas of California.
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Mountains formed between two large faults are known as "fault-block mountains." These mountains typically arise due to tectonic forces that cause blocks of the Earth's crust to be uplifted or tilted along fault lines. The movement of these faults can create steep, rugged terrain as sections of the crust are displaced relative to one another. Examples of fault-block mountains include the Sierra Nevada in California.