A Block Mountain.
This is called a strike slip fault.
The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
On fault lines and boarders.
parallel normal faults.
A Block Mountain.
This is called a strike slip fault.
Where fault blocks collide into each other. The most prominent example of this are the Himalayan Mountains formed by the collision of the Indian plate and the Eurasian Plate making what is called a folded mountain.
The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
fault block
The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
forwrd against each other
The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
strike-slip
The Sierra Nevada and the Tetons are among the mountain ranges formed by means other than tectonic movement. Many mountain ranges are formed by fault block shifts up and down as well as sculpting by erosion, volcanoes and glaciers. The mountains that we see are most often the result of many complex interactions over long periods of time.
they are formed by fault block
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.