The two types of faults that can result in mountains are reverse faults and normal faults.
Faults are created when tectonic plates are stretching or compressing. There are two types of faults which are normal and reverse faults.
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.
Normal reverse and strike-slip faults are types of geological faults that occur due to tectonic forces. Normal faults occur when the Earth's crust is extended, causing one block of rock to move downward relative to another, typically forming steep angles. Conversely, reverse faults result from compressional forces, where one block of rock is pushed up over another, creating a steep incline. Strike-slip faults involve lateral movement, where two blocks slide past each other horizontally, often associated with transform plate boundaries.
When two tectonic plates collide, it can result in the formation of mountain ranges due to the intense pressure and folding of the Earth's crust. This process is known as continental collision and can lead to the creation of complex geological features, such as fold mountains and faults, as the plates push against each other.
they over lap and cause mountains and hills Folded mountains are produced
The two types of faults that create mountains are thrust faults, where rocks are pushed up and over each other, and normal faults, where rocks are pulled apart and one block slides down. These fault movements result in the crust being folded and uplifted, leading to the formation of mountains.
Thrust faults and reverse faults can result in mountain formation. Thrust faults occur when rocks are pushed up and over each other, while reverse faults involve compressional forces causing rocks to move vertically. Both of these fault types contribute to the uplift and formation of mountain ranges.
The two types of faults that can result in mountains are thrust faults and normal faults. Thrust faults occur when older rock is pushed on top of younger rock, causing uplift and mountain formation. Normal faults occur when tensional forces cause one block of rock to drop down relative to another block, creating valleys and mountain ranges.
Faults are fractures in the Earth's crust where two blocks of rock move past each other. When these blocks of rock shift along a fault line, they can create vertical movement, leading to uplift and the formation of mountains. Over time, repeated movement along faults can result in the gradual building of mountain ranges.
Faults are created when tectonic plates are stretching or compressing. There are two types of faults which are normal and reverse faults.
bearing faults and circuit connection faults
rverse and normal
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.
it means that boy over there
Surface features produced by crustal movements at a transform plate boundary include strike-slip faults and earthquakes. These are caused by the horizontal movement of two tectonic plates sliding past each other. This movement does not typically result in significant volcanic activity or the formation of mountains.
Where two plates move away from each other tension forces create many normal faults.
Anticlines, Reverse faults. and Folded mountains -apex (: