Difference between revisions of "Shale" - New World Encyclopedia
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| − | '''Shale''' is a fine-grained [[sedimentary rock]] whose original constituents were [[clay]]s or [[mud]]s. | + | [[Image:ShaleUSGOV.jpg|thumb|right|250px|A piece of '''shale''']] |
| + | '''Shale''' is a fine-grained [[sedimentary rock]] whose original constituents were [[clay]]s or [[mud]]s. It is characterized by thin laminae breaking with an irregular curving fracture, often splintery and usually parallel to the often-indistinguishable bedding plane. This property is called [[Fissility (geology)|fissility]]. Non-fissile [[Rock (geology)|rocks]] of similar composition but made of particles smaller than .0625 millimeters are described as [[mudstone]]s. Rocks with similar particle sizes but with less [[clay]] and therefore grittier are [[silt]]stones. | ||
| − | Shale is the most common sedimentary rock.[http://wps.prenhall.com/esm_lutgens_foundations_3/0,6540,354318-,00.html] | + | Shale is the most common sedimentary rock.<ref>[http://wps.prenhall.com/esm_lutgens_foundations_3/0,6540,354318-,00.html Rocks: Materials of the Lithosphere: Summary,] Pearson Education. Retrieved August 29, 2007.</ref> |
== Formation == | == Formation == | ||
| − | The process in the [[rock cycle]] which forms shale is [[compaction]]. The fine particles that compose shale can remain suspended in air long after the larger and denser particles of sand have deposited out. Shales are typically deposited in very slow moving water and are often found in lake and | + | [[Image:Shale 8040.jpg|thumb|right|200px|[[Weathering]] shale at a [[road]] cut in southeastern [[Kentucky]]]] |
| + | [[Image:Limestoneshale7342.jpg|thumb|200px|Limey shale overlaid by [[limestone]] in [[Tennessee]]]] | ||
| + | The process in the [[rock cycle]] which forms shale is [[compaction]]. The fine particles that compose shale can remain suspended in air long after the larger and denser particles of [[sand]] have deposited out. Shales are typically deposited in very slow moving water and are often found in lake and [[lagoon]]al deposits, in [[river]] [[delta]]s, on floodplains and offshore of [[beach]] sands. They can also be deposited on the [[continental shelf]], in relatively deep, quiet water. | ||
| − | + | Black shales are dark, as a result of being especially rich in [[oxidation|unoxidized]] [[carbon]]. Common in some [[Paleozoic]] and [[Mesozoic]] [[stratum|strata]], black shales were deposited in [[anoxia|anoxic]], reducing environments, such as in stagnant water columns (such as [[oil shale]]). | |
[[Fossil]]s, animal tracks/burrows and even raindrop impact craters are sometimes preserved on shale bedding surfaces. Shales may also contain [[concretion]]s. | [[Fossil]]s, animal tracks/burrows and even raindrop impact craters are sometimes preserved on shale bedding surfaces. Shales may also contain [[concretion]]s. | ||
Shales that are subject to heat and pressure alter into a hard, fissile, and metamorphic material known as [[slate]], which is often used in building construction. | Shales that are subject to heat and pressure alter into a hard, fissile, and metamorphic material known as [[slate]], which is often used in building construction. | ||
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==See also== | ==See also== | ||
| − | * [[ | + | * [[Rock (geology)|Rock]] |
| − | * [[ | + | * [[Sand]] |
| − | * [[ | + | * [[Silt]] |
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* [[Slate]] | * [[Slate]] | ||
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== Notes == | == Notes == | ||
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==References== | ==References== | ||
| − | * Blatt, Harvey, and Robert J. Tracy. 1995. ''Petrology: Igneous, Sedimentary, and Metamorphic'', 2nd ed. New York: W.H. Freeman. ISBN 0716724383 | + | * Blatt, Harvey, and Robert J. Tracy. 1995. ''Petrology: Igneous, Sedimentary, and Metamorphic'', 2nd ed. New York: W.H. Freeman. ISBN 0716724383 |
| − | * Farndon, John. 2006. ''The Practical Encyclopedia of Rocks & Minerals: How to Find, Identify, Collect and Maintain the World's best Specimens, with over 1000 Photographs and Artworks''. London: Lorenz Books. ISBN 0754815412 | + | * Farndon, John. 2006. ''The Practical Encyclopedia of Rocks & Minerals: How to Find, Identify, Collect and Maintain the World's best Specimens, with over 1000 Photographs and Artworks''. London: Lorenz Books. ISBN 0754815412 |
| − | * Pellant, Chris. 2002. ''Rocks and Minerals''. Smithsonian Handbooks. New York: Dorling Kindersley. ISBN 0789491060 | + | * Pellant, Chris. 2002. ''Rocks and Minerals''. Smithsonian Handbooks. New York: Dorling Kindersley. ISBN 0789491060 |
| − | * Shaffer, Paul R., Herbert S. Zim, and Raymond Perlman. 2001. ''Rocks, Gems and Minerals'' | + | * Shaffer, Paul R., Herbert S. Zim, and Raymond Perlman. 2001. ''Rocks, Gems and Minerals'', Rev. ed. New York: St. Martin's Press. ISBN 1582381321 |
| − | * Skinner, Brian J., Stephen C. Porter, and Jeffrey Park. 2004. ''Dynamic Earth: An Introduction to Physical Geology'' | + | * Skinner, Brian J., Stephen C. Porter, and Jeffrey Park. 2004. ''Dynamic Earth: An Introduction to Physical Geology'', 5th ed. Hoboken, N.J.: John Wiley. ISBN 0471152285 |
| − | * Tucker, Maurice E. 2001. ''Sedimentary Petrology''. 3rd ed. Oxford | + | * Tucker, Maurice E. 2001. ''Sedimentary Petrology''. 3rd ed. Oxford: Blackwell Publishing. ISBN 0632057351 |
== External links == | == External links == | ||
| + | All links retrieved August 29, 2007. | ||
| − | * [http://geology.about.com/library/bl/images/blshale.htm Shale | + | * [http://geology.about.com/library/bl/images/blshale.htm Shale] – About.com: Geology, by Andrew Alden |
| − | * [http://csmres.jmu.edu/geollab/Fichter/SedRx/Rocks/shale.html Shale #1: Mudstone. | + | * [http://csmres.jmu.edu/geollab/Fichter/SedRx/Rocks/shale.html Shale #1: Mudstone] – Lynn S. Fichter, Dept. of Geology, James Madison University |
| − | * [http://www.ucmp.berkeley.edu/cambrian/burgess.html The Burgess Shale | + | * [http://www.ucmp.berkeley.edu/cambrian/burgess.html The Burgess Shale] – University of California Museum of Paleontology |
[[Category:Physical sciences]] | [[Category:Physical sciences]] | ||
Revision as of 16:04, 29 August 2007
Shale is a fine-grained sedimentary rock whose original constituents were clays or muds. It is characterized by thin laminae 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 .0625 millimeters are described as mudstones. Rocks with similar particle sizes but with less clay and therefore grittier are siltstones.
Shale is the most common sedimentary rock.[1]
Formation
The process in the rock cycle which forms shale is compaction. The fine particles that compose shale can remain suspended in air long after the larger and denser particles of sand have deposited out. Shales are typically deposited in very slow moving water and are often found in lake and lagoonal deposits, in river deltas, on floodplains and offshore of beach sands. They can also be deposited on the continental shelf, in relatively deep, quiet water.
Black shales are dark, as a result of being especially rich in unoxidized carbon. Common in some Paleozoic and Mesozoic strata, black shales were deposited in anoxic, reducing environments, such as in stagnant water columns (such as oil shale).
Fossils, animal tracks/burrows and even raindrop impact craters are sometimes preserved on shale bedding surfaces. Shales may also contain concretions.
Shales that are subject to heat and pressure alter into a hard, fissile, and metamorphic material known as slate, which is often used in building construction.
See also
Notes
- ↑ Rocks: Materials of the Lithosphere: Summary, Pearson Education. Retrieved August 29, 2007.
ReferencesISBN links support NWE through referral fees
- Blatt, Harvey, and Robert J. Tracy. 1995. Petrology: Igneous, Sedimentary, and Metamorphic, 2nd ed. New York: W.H. Freeman. ISBN 0716724383
- Farndon, John. 2006. The Practical Encyclopedia of Rocks & Minerals: How to Find, Identify, Collect and Maintain the World's best Specimens, with over 1000 Photographs and Artworks. London: Lorenz Books. ISBN 0754815412
- Pellant, Chris. 2002. Rocks and Minerals. Smithsonian Handbooks. New York: Dorling Kindersley. ISBN 0789491060
- Shaffer, Paul R., Herbert S. Zim, and Raymond Perlman. 2001. Rocks, Gems and Minerals, Rev. ed. New York: St. Martin's Press. ISBN 1582381321
- Skinner, Brian J., Stephen C. Porter, and Jeffrey Park. 2004. Dynamic Earth: An Introduction to Physical Geology, 5th ed. Hoboken, N.J.: John Wiley. ISBN 0471152285
- Tucker, Maurice E. 2001. Sedimentary Petrology. 3rd ed. Oxford: Blackwell Publishing. ISBN 0632057351
External links
All links retrieved August 29, 2007.
- Shale – About.com: Geology, by Andrew Alden
- Shale #1: Mudstone – Lynn S. Fichter, Dept. of Geology, James Madison University
- The Burgess Shale – University of California Museum of Paleontology
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