Slickenside
In geology, a slickenside is a smoothly polished surface caused by frictional movement between rocks along the two sides of a fault. This surface is normally striated in the direction of movement. The plane may be coated by mineral fibres that grew during the fault movement, known as slickenfibres, which also show the direction of displacement. Due to irregularities in the fault plane exposed slickenfibres typically have a stepped appearance that can be used to determine the sense of movement across the fault. The surface feels smoother when the hand is moved in the same direction that the eroded side of the fault moved (see diagram for explanation), as the surface steps down in that direction, like the scales on a fish when stroked from the head.
In pedology, the study of soils in their natural environments, a slickenside is a surface of the cracks produced in soils containing a high proportion of swelling clays. Slickensides are a type of cutan. In the Australian Soil Classification, slickensides, along with lenticular structural aggregates, are an indicator of a vertosol.
Gallery
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Dextral slickenside of pyrite
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Slickensides developed on the surface of a small fault in quartzite in the Alpujarras
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Slickensides on a fault plane, south wall of Bear Valley Strip Mine. Lens cap 5.8cm wide.
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Calcite slickenfibres on the surface of a normal fault, east of Kilve, Somerset.
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Slickensides on a fault plane in Corona Heights Park, San Francisco
Slickensides on the Moon
On the Moon, a boulder with slickensides, discovered in a debris-strewn small crater at Station 9 near Rima Hadley, was photographed during a moonwalk by the crew of Apollo 15.
| This article uses material from the Wikipedia article Metasyntactic variable, which is released under the Creative Commons Attribution-ShareAlike 3.0 Unported License. |