The nature of folding that occurs on the
earth's surface depends on many factors. These
include the nature of rocks, intensity and duration
Axis of the fold
Sy
Axial, plane
of force.
Fig. 1.4:P
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Figure 10.6: Rocks that were originally deposited in horizontal layers can subsequently deform by tectonic forces into folds and faults. Folds constitute the twists and bends in rocks. Faults are planes of detachment resulting when rocks on either side of the displacement slip past one another.
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