A monocline (or, rarely, a monoform) is a step-like fold in rock strata consisting of a zone of steeper dip within an otherwise horizontal or gently dipping sequence.
Formation
Monoclines may be formed in several different ways (see diagram)
By differential compaction over an underlying structure, particularly a large fault at the edge of a basin due to the greater compactibility of the basin fill, the amplitude of the fold will die out gradually upwards. By mild reactivation of an earlier extensional fault during a phase of inversion causing folding in the overlying sequence. As a form of fault propagation fold during upward propagation of an extensional fault in basement into an overlying cover sequence. As a form of fault propagation fold during upward propagation of a reverse fault in basement into an overlying cover sequence.
Examples Waterpocket Fold in Capitol Reef National Park, Utah Comb Ridge in southern Utah Grandview-Phantom Monocline in Grand Canyon, Arizona Grand Hogback in Colorado Lebombo Mountains in Southern Africa Lapstone Monocline in the Blue Mountains (Australia) Beaumaris Monocline in Victoria (Australia) Purbeck Monocline on the Isle of Purbeck, Dorset, England Fore-Sudetic Monocline, Poland Sindh Monocline, Pakistan Torres Flexure, southern Brazil
See also Anticline Homocline Syncline
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