"Frictional sliding " is one aspect for consideration during shear fracturing and faulting.
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In fracturing, frictional sliding typically only has significant effects on the reactivation on existing shear fractures.
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Geologically, Mount Elden is a lava dome composed almost entirely of fractures, longitudinal tension fractures, and conjugate shear fractures.
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Deep, narrow gorges and shear fractures were transformed into caves by large chunks of rock falling from above and wedging into the cracks leaving an open area below.
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Extensive field and core work documents an interconnected network of fractures dominated by closely spaced, bed-normal extension fractures, supplemented by strike-slip conjugate shear fractures and local low-angle thrust planes.
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An additional, important characteristic of shear-mode fractures is the process by which they spawn " wing cracks ", which are tensile cracks that form at the propagation tip of the shear fractures.
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This criterion is based largely off of the work of Charles Coulomb, who suggested that as long as all stresses are compressive, as is the case in shear fracture, the shear stress is related to the normal stress by:
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