Compressional stresses (reverse or thrust fault) cause a rock to shorten. Tensional stresses (normal fault) cause a rock to elongate, or pull apart. Shear stresses (strike-slip or horizontal fault) causes rocks to slip past each other.
The three types of faults are Normal faults, Reverse faults, and Strike and Slip fault
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.
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.
There are three main types of faults: normal, reverse, and strike-slip. These faults represent the different ways that rocks can move along fractures in the Earth's crust.
the three types of faults are normal (colliding), reverse (moving apart), strike-slip (sliding past each other)
The three main types of stress in a rock are shearing, tension, and compression.
The three types of static stresses are tension (stretching force), compression (squeezing force), and shear (sliding force). Static stresses can cause materials to deform or fail if they exceed the material's strength.
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.
Describe the three types of plate motion and the faults that are characteristic of each type of motion.
The three main types of fault lines are normal faults, reverse faults, and strike-slip faults. Normal faults occur when rocks are pulled apart, reverse faults form when rocks are pushed together, and strike-slip faults happen when rocks slide past each other horizontally.
ShearingCompressionTension
the three types of faults are normal (colliding), reverse (moving apart), strike-slip (sliding past each other)