Normal Fault
A transform fault is least likely to form mountains because it involves horizontal movement along fault lines rather than vertical movement that leads to uplift and mountain formation.
A fault block mountain occurs when rock layers are pulled from opposite directions, large blocks slide downward, creating peaks and valleys. See Link edited by ERIC: To make it easier (SHEARING)
Fault-block mountains form from vertical fault movement. These mountains are created when blocks of the Earth's crust are pushed up and down along fault lines, resulting in steep, jagged peaks and valleys. An example of a fault-block mountain range is the Sierra Nevada in California.
The most common types of mountain formations on Earth are folded mountains, fault-block mountains, and volcanic mountains. Folded mountains are created when tectonic forces compress and deform rock layers. Fault-block mountains form when tectonic forces cause blocks of the Earth's crust to uplift or subside along faults. Volcanic mountains are formed by volcanic activity, where magma rises to the surface and solidifies to create a mountain.
Block mountains form from vertical fault movements when two tectonic plates move against each other, causing one section of rock to be pushed upward while another is pushed downward along a fault line. This results in steep, rugged mountain ranges with distinct uplifted blocks of rock. Examples include the Sierra Nevada in California and the Tetons in Wyoming.
A fault-block mountain forms where the edges of two plates come together to create a fault. When one plate pushes up over the other one, the upper one can continue up until it is high enough to create a fault-block mountain.
The San Andreas fault has caused the basins and mountain ranges to form.
A fault-block mountain forms where the edges of two plates come together to create a fault. When one plate pushes up over the other one, the upper one can continue up until it is high enough to create a fault-block mountain.
A fault-block mountain forms where the edges of two plates come together to create a fault. When one plate pushes up over the other one, the upper one can continue up until it is high enough to create a fault-block mountain.
A transform fault is least likely to form mountains because it involves horizontal movement along fault lines rather than vertical movement that leads to uplift and mountain formation.
A fault block mountain occurs when rock layers are pulled from opposite directions, large blocks slide downward, creating peaks and valleys. See Link edited by ERIC: To make it easier (SHEARING)
they form from the constant moving of techtonic plates which cause magma to spew out and the build up becomes a mountain
normal faults cause mountains to form
to form a mountain the plates under the earth must shift and move
The type of mountain that forms when forces pull from opposite directions is the fault-block mountain.
Folded type mountains form due to the horizontal compression of the Earth's crust, leading to the folding of rock layers. Fault-block mountains, on the other hand, occur when tectonic forces cause the Earth's crust to break and move along faults, resulting in uplifted blocks of rock.
A fault-block mountain can be found in Death Valley, California and also in the Sierra Nevada mountains in California. Movement of large crustal blocks form fault-block mountains.