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Crustal deformation. That is, when pieces of the Earth's crust change shape due to tectonic forces.
hoe many types of granite rocks are there
there are all three types of rocks: igneous, metamorphic and sedimentary.
There are three (3) different types of rocks, igneous, sedimentary and metamorphic rocks
There are thousands of different types of rocks.
cracks == In addition to cracks: faulting, metamorphism to new rock types, earthquakes, tilting, and folding.
Tensional forces and compressional forces.
Crustal deformation. That is, when pieces of the Earth's crust change shape due to tectonic forces.
sedimentary rocks
Through erosional forces and differences in rock types.
balance
There are four different types of earthquakes - tectonic, volcanic, collapse and explosion. A tectonic earthquake is one that occurs when the earth's crust breaks due to geological forces on rocks and adjoining plates that cause physical and chemical changes.
Three types of weathing
Its due to temperature and pressure. when 2 continental plates converge the form a mountain belt, because there is no subduction zone they create a high range of mountains like the Himalayas. The common rock types are the metamorphic rocks and the pressure cause folds in the rock as they stretch depends on the direction. It can be anticline or syncline. Temperature also causes the folding of rocks as magma passes through rocks it makes the rock nearby ductile cause deformation on it.These are usually regional metamorphic rocks.
Sudden forces break the crust of the earth to make openings through which various types of material including molten magma, solid rocks, gases etc. are ejected to the surface from the interior of the earth.
deformation
There are three main forces that drive deformation within the Earth. These forces create stress, and they act to change the shape and/or volume of a material. The following diagrams show the three main types of stress: compressional, tensional, and shear. Stress causes the build up of strain, which causes the deformation of rocks and the Earth's crust. Compressional stresses cause a rock to shorten. Tensional stresses cause a rock to elongate, or pull apart. Shearstresses causes rocks to slip past each other.