- Shale
Shale (also called mudstone) is a fine-grained
sedimentary rock whose original constituents wereclay mineral s ormud s. It is characterized by thin laminae [cite encyclopedia
title = shale
encyclopedia = Chambers Dictionary of Science and Technology
publisher = Chambers Harrap Publishers Ltd
date = 1999] breaking with an irregular curving fracture, often splintery and usually parallel to the often-indistinguishable bedding plane. This property is called fissility. Non-fissile rocks of similar composition but made of particles smaller than 1/16 mm are described asmudstone s. Rocks with similar particle sizes but with less clay and therefore grittier aresiltstone s. Shale is the most common sedimentary rock. [cite web
url=http://wps.prenhall.com/esm_lutgens_foundations_3/0,6540,354318-,00.html
title= Rocks: Materials of the Lithosphere - Summary
publisher=
accessdate=2007-07-31]Formation
The process in the
rock cycle which forms shale is compaction. The fine particles that compose shale can remain in water long after the larger and denser particles of sand have deposited. Shales are typically deposited in very slow moving water and are often found in lake andlagoon al deposits, inriver delta s, onfloodplain s and offshore of beach sands. They can also be deposited on thecontinental shelf , in relatively deep, quiet water.'Black shales' are dark, as a result of being especially rich in unoxidized
carbon . Common in somePaleozoic andMesozoic strata, black shales were deposited in anoxic, reducing environments, such as in stagnant water columns.Fossil s, animal tracks/burrows and even raindrop impact craters are sometimes preserved on shale bedding surfaces. Shales may also containconcretion s.Shales that are subject to heat and pressure alter into a hard, fissile,
metamorphic rock known asslate , which is often used in building construction.ee also
*
Bituminous shale
*Oil shale
*Burgess shale
*Barnett Shale
*Bearpaw Shale
*Wianamatta shale Footnotes
References
* Blatt, Harvey and Robert J. Tracy, 1996, "Petrology: Igneous, Sedimentary and Metamorphic", 2nd ed., Freeman, ISBN 0-7167-2438-3
Wikimedia Foundation. 2010.