There are 3 main types of faults
1. Normal
2. Strike slip
3. Reverse(Thrust)
In a normal fault the foot wall stays in place while the hanging wall moves DOWNWARDS
In a strike slip the tectonic plate(s) slide past each other horizontally
In a reverse fault, the hanging wall gets pushed UPWARDS over the foot wall
(The pictures are in the reverse order)
An example of a dip-slip or transform fault is the San Andreas fault in California. In this type of fault, there is horizontal displacement. Another type of fault is a normal fault. In this type of fault, the hanging wall falls below the foot wall. This occurs from tensional stress.
By studying how the earth's crust reacts to earthquakes, volcanoes, or underground explosions and the like.
cupping, twisting, splitting and knots.
normal reverse strike-slip
Predicting when earthquakes will happen and when volcanoes will erupt
In the extreme tension forces can cause local vulcanism. At a local level it may create fault block mountains. Over larger landscapes, it creates Rift Valleys such as the giant one in East Africa today.
No. Your terminology is close but not quite right. The three main types of faults are normal faults, reverse faults, and strike-slip faults. Strike-slip faults may also be called transform faults.
There are 6 types of fault lines. Strike-slip faults, dip-slip faults, oblique- slip faults, listric faults, ring faults, and synthetic and antithetic faults.
Faults are created when tectonic plates are stretching or compressing. There are two types of faults which are normal and reverse faults.
Your faults are flaws in your personality. Earth's faults are cracks in the ground along which blocks of rock move.
Your faults are flaws in your personality. Earth's faults are cracks in the ground along which blocks of rock move.
Your faults are flaws in your personality. Earth's faults are cracks in the ground along which blocks of rock move.
The three major types of faults are normal faults, reverse faults, and strike-slip faults. Synclines are not faults but rather geological structures that describe the folding of rock layers.
The main direction of the stress on blocks of rock at normal faults, reverse faults and the strike slip faults usually happens at the weak areas.
Cable faults are normally categorised as (a) conductor-to-earth (ground) faults, (b) conductor-to-conductor faults, and (c) conductor-to-conductor-to earth (ground) faults. In addition to that, we can categorise them by whether they are 'high-resistance' or 'low-resistance' faults.
The two types of faults that can result in mountains are thrust faults and normal faults. Thrust faults occur when one tectonic plate is forced up over another, while normal faults occur when the Earth's crust is being pulled apart, causing one block to drop down relative to the other.
Normal faults are when you have hanging walls that slide down relative to and below the footwall. Dip-slip faults are normal faults.
Folds are the when the rock layers bend. Faults are breaks in the rock layers. Folds are called anticlines and synclines. Faults are called reverse faults, normal faults, or strike-slip faults.