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زمینشناسی و معدن::
تاقدیس
Anticlines and Synclines
The two most common types of folds are anticlines and synclines (Figure 10.8).
Anticlines occur when compres- sional stresses squeeze sedimentary layers into arch-like folds.
Notice in Figure 10.8 that the right limb of the syncline is also the left limb of the adjacent anticline.
Figure 10.9B shows the outcrop pattern produced when erosion removes the upper layers of a plunging anticline and exposes its interiors.
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