orogeny and epeirogeny
Crustal deformation. That is, when pieces of the Earth's crust change shape due to tectonic forces.
Anelastic deformation. Deformation processes where a material assumes its original shape after the load is removed, but with a time delay.
Deformation is calculated by using deflecto meter.
Deformation is a change in the shape and volume of a rock, deformation is produced when a rock experiences a stress that is greater than the strength of the rock.
orogeny and epeirogeny
orogeny and epeirogeny
elastic deformation, ductile deformation and fracture
deformation
Faults are formed by brittle deformations and folds are formed by ductile deformation.
Crustal deformation. That is, when pieces of the Earth's crust change shape due to tectonic forces.
fracturing, basal slip and plastic deformation or plastic flow :)
elastic deformation
The general term is deformation, but it has several different types depending on the material.
Elastic deformation is recoverable deformation. As such, when the load that caused the deformation is removed the material will return to it's original shape.
Cleavage is the degree of deformation that occurs with types of rocks. The cleavage of geodes is indiscernible due to the irregularity of the stone.
ductile deformation