Folding and Faulting usually work together to form mountains. Faulting works by one plate shifting up and one plate submerging. Folding however works by both plates pushing against each other slowly folding over and over.
Faulting and Folding and work together to make mountains by as one plate moves down the other up causes the plate going up to roll over or move on top of the other plate then as the bottom plate gets heat from the earths core it rises folding the plate on top again to bring it even higher.
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The large anticlines form the fold mountain and the dome mountains. This is usually as a result of jointing, folding and faulting.
its the differences between tilting an folding
deformation
The effects of diastrophism are so many on the surface of the earth and include formation of mountains, plateaus and may cause tremors and earthquakes.
changes in rocks associated with faulting and folding
Mountains
The large anticlines form the fold mountain and the dome mountains. This is usually as a result of jointing, folding and faulting.
Folding and faulting in mountains occurs because of the movement of lithospheric plates as described in the theory of plate tectonics. Continent to continent collision compresses the crust and its sedimentary cover rocks, displacing and distorting them upwards (folding) and fracturing them (faulting). Folding and faulting can also occur in oceanic crust-continental crust collisions, in areas above subduction zones.
mountains
Fault block mountains are often created through rifting, which is an indication of tensional tectonic forces. Fault block mountains are primarily the result of faulting and folding.
The Rocky Mountain Front in Montana which were formed by faulting, folding and overthrusting.
Collisions Of Continental Plates
its the differences between tilting an folding
The three major mountains are formed through faulting.
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deformation
The effects of diastrophism are so many on the surface of the earth and include formation of mountains, plateaus and may cause tremors and earthquakes.