Shorten the Earth's crust.
shorten, compress
Normal faults have a hanging wall and footwall Normal Faults are common at mid-ocean ridges Normal Faults occur where the crust is being pulled apart at the divergent plate boudary. Sorry i only have 3 facts, but I anyone with the question
tacitos
Faults are formed when a large crack in the Earth's crust move. One part of the crust moves against another part. Normal faults occur when strong forces deep underground pulls the sides apart, and the upper side, or the hanging wall will drop down.
Normal faults are caused by tension in the movement of rocks
because the hulk and iron man are gettin bis-ay, if you know what i mean, and this makes earthquakes
Normal faults thin and extend the earth's crust. Reverse faults cause crustal shortening and thickening.
Tensile stress within the crust.
It is called Graben
Faults are surfaces along the earths crust in which rocks have been fractured and displaced. There are three types of faults: strike-slip, normal and reverse.
Normal faults have a hanging wall and footwall Normal Faults are common at mid-ocean ridges Normal Faults occur where the crust is being pulled apart at the divergent plate boudary. Sorry i only have 3 facts, but I anyone with the question
Plate motions produce stress in Earths crust that leads to faults, mountain building, and earthquakes.
tacitos
Faults are formed when a large crack in the Earth's crust move. One part of the crust moves against another part. Normal faults occur when strong forces deep underground pulls the sides apart, and the upper side, or the hanging wall will drop down.
tacitos
Not necessarily. Earthquakes occur when there is movement along cracks in the Earth's crust called faults. There are three main types of fault, all of which can produce earthquakes. Normal faults usually occur where the crust is being pulled apart. Reverse faults, also called thrust faults, are usually found where sections of the crust are pushed together. Transform faults occur where sections of the crust slide past each other horizontally, neither pushing together nor pulling apart.
There are three types of fault lines in the crust. There are divergent boundaries, convergent boundaries, and transform boundaries.
normal and rivesre fault, thrust fault, dip-strike fault.