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	<title>Alluvium - Revision history</title>
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		<id>https://indianpedia.org/index.php?title=Alluvium&amp;diff=466833&amp;oldid=prev</id>
		<title>Aurelia2406 at 14:40, 3 November 2025</title>
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&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;{{short description|Loose soil or sediment that is eroded and redeposited in a non-marine setting}}&lt;br /&gt;
{{redirect-distinguish|Alluvial|Alluvial (horse)|Alluvial diagram}}&lt;br /&gt;
[[File:Riogranderift sanluisbasin.png|thumb|Alluvium and adjacent constituents]]&lt;br /&gt;
[[File:South Africa-Eastern Cape-Gamtoos Valley-Alluvial Gravel01.jpg|thumb|Alluvium deposits in the [[Gamtoos River|Gamtoos Valley]] in [[South Africa]]]]&lt;br /&gt;
[[File:AlluvialPlain.JPG|thumb|An [[alluvial plain]] in [[Red Rock Canyon State Park (California)]]]]&lt;br /&gt;
[[File:Amazon alluvium deposit - autazes.jpg|thumb|Alluvial river deposits in the [[Amazon basin]], near Autazes, AM, [[Brazil]]. The seasonal deposits are extremely fertile and crucial to [[subsistence farming]] in the Amazon Basin along the river banks.]]&lt;br /&gt;
&amp;#039;&amp;#039;&amp;#039;Alluvium&amp;#039;&amp;#039;&amp;#039; ({{etymology|la|{{wikt-lang|la|alluvius}}|}}, {{etymology||{{wikt-lang|la|alluere}}|to wash against}}) is loose [[clay]], [[silt]], [[sand]], or [[gravel]] that has been deposited by running water in a stream bed, on a [[floodplain]], in an [[alluvial fan]] or [[beach]], or in similar settings.&amp;lt;ref name=dictalluvium&amp;gt;{{cite book |editor1-last=Jackson |editor1-first=Julia A. |title=Glossary of geology. |date=1997 |publisher=American Geological Institute |location=Alexandria, Virginia |isbn=0922152349 |edition=Fourth |chapter=alluvium}}&amp;lt;/ref&amp;gt;&amp;lt;ref&amp;gt;[https://web.archive.org/web/20110501155938/http://www.geotech.org/survey/geotech/dictiona.html Glossary of Geological Terms]. Geotech.org. Retrieved on 2012-02-12.&amp;lt;/ref&amp;gt;&amp;lt;ref&amp;gt;[http://geology.com/dictionary/glossary-a.shtml Geology Dictionary – Alluvial, Aquiclude, Arkose]. Geology.Com. Retrieved on 2012-02-12.&amp;lt;/ref&amp;gt; Alluvium is also sometimes called &amp;#039;&amp;#039;&amp;#039;alluvial deposit&amp;#039;&amp;#039;&amp;#039;.&amp;lt;ref&amp;gt;{{cite book |editor1-last=Jackson |editor1-first=Julia A. |title=Glossary of geology. |date=1997 |publisher=American Geological Institute |location=Alexandria, Virginia |isbn=0922152349 |edition=Fourth |chapter=alluvial deposit}}&amp;lt;/ref&amp;gt;&amp;lt;ref&amp;gt;{{cite book |last1=Allaby |first1=Michael |title=A dictionary of geology and earth sciences |date=2013 |publisher=Oxford University Press |location=Oxford |isbn=9780199653065 |edition=Fourth |chapter=alluvium}}&amp;lt;/ref&amp;gt; Alluvium is typically geologically young and is not [[Consolidation (geology)|consolidated]] into solid rock. [[Sediments]] deposited underwater, in seas, [[estuaries]], lakes, or ponds, are not described as alluvium.&amp;lt;ref name=dictalluvium/&amp;gt;&lt;br /&gt;
Floodplain alluvium can be highly fertile, and supported some of the earliest human civilizations.&amp;lt;ref&amp;gt;{{cite journal |last1=Kidder |first1=Tristram |last2=Liu |first2=Haiwang |last3=Xu |first3=Qinghai |last4=Li |first4=Minglin |title=The Alluvial Geoarchaeology of the Sanyangzhuang Site on the Yellow River Floodplain, Henan Province, China: THE YELLOW RIVER FLOODPLAIN, HENAN PROVINCE |journal=Geoarchaeology |date=July 2012 |volume=27 |issue=4 |pages=324–343 |doi=10.1002/gea.21411|s2cid=140587757 }}&amp;lt;/ref&amp;gt;&lt;br /&gt;
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==Definitions==&lt;br /&gt;
The present [[Scientific consensus|consensus]] is that &amp;quot;alluvium&amp;quot; refers to loose [[sediments]] of all types deposited by running water in [[floodplains]] or in [[alluvial fans]] or related [[landforms]].&amp;lt;ref name=dictalluvium/&amp;gt;{{sfn|Allaby|2013|loc=&amp;quot;alluvial&amp;quot;}}&amp;lt;ref name=Miller2020&amp;gt;{{cite journal |last1=Miller |first1=Bradley A. |last2=Juilleret |first2=Jérôme |title=The colluvium and alluvium problem: Historical review and current state of definitions |journal=Earth-Science Reviews |date=October 2020 |volume=209 |article-number=103316 |doi=10.1016/j.earscirev.2020.103316|bibcode=2020ESRv..20903316M |doi-access=free }}&amp;lt;/ref&amp;gt; However, the meaning of the term has varied considerably since it was first defined in the French dictionary of [[Antoine Furetière]], posthumously published in 1690. Drawing upon concepts from [[Roman law]], Furetière defined &amp;#039;&amp;#039;[[alluvion]]&amp;#039;&amp;#039; (the French term for alluvium) as new land formed by deposition of sediments along rivers and seas.&amp;lt;ref name=Miller2020/&amp;gt;&lt;br /&gt;
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By the 19th century, the term had come to mean recent sediments deposited by rivers on top of older &amp;#039;&amp;#039;[[diluvium]]&amp;#039;&amp;#039;, which was similar in character but interpreted as sediments deposited by [[Noah&amp;#039;s flood]]. With the rejection by geologists of the concept of a primordial universal flood, the term &amp;quot;diluvium&amp;quot; fell into disfavor and was replaced with &amp;quot;older alluvium&amp;quot;. At the same time, the term &amp;quot;alluvium&amp;quot; came to mean all sediment deposits due to running water on plains. The definition gradually expanded to include deposits in estuaries, coasts, and young rock of marine and [[fluvial]] origin.&amp;lt;ref name=Miller2020/&amp;gt;&lt;br /&gt;
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Alluvium and diluvium were grouped as &amp;#039;&amp;#039;[[colluvium]]&amp;#039;&amp;#039; in the late 19th century. &amp;quot;Colluvium&amp;quot; is now generally understood as sediments produced by [[gravity]]-driven transport on steep slopes. At the same time, the definition of &amp;quot;alluvium&amp;quot; has switched back to an emphasis on sediments deposited by river action. There continues to be disagreement over what other sediment deposits should be included under the term &amp;quot;alluvium&amp;quot;.&amp;lt;ref name=Miller2020/&amp;gt;&lt;br /&gt;
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==Age==&lt;br /&gt;
Most alluvium is [[Quaternary]] in age and is often referred to as &amp;quot;cover&amp;quot; because these sediments obscure the underlying [[bedrock]]. Most sedimentary material that fills a [[Sedimentary basin|basin]] (&amp;quot;basin fill&amp;quot;) that is not [[Lithification|lithified]] is typically lumped together as &amp;quot;alluvial&amp;quot;.&amp;lt;ref name=EB&amp;gt;{{Cite EB1911|wstitle=Alluvium}}&amp;lt;/ref&amp;gt; Alluvium of [[Pliocene]] age occurs, for example, in parts of [[Idaho]].&amp;lt;ref&amp;gt;{{Citation | last = Ames | first = Dan | contribution = Formation of the Soils | year = 1998 | title = Soil Survey of Jerome County and Part of Twin Falls County, Idaho | url = https://archive.org/details/usda-contents/page/238/mode/1up | pages = 238 | publisher = Natural Resources Conservation Service, [[United States Department of Agriculture]] | contribution-url = https://web.archive.org/web/20220223221606/https://www.nrcs.usda.gov/Internet/FSE_MANUSCRIPTS/idaho/ID704/0/id704_text.pdf}}&amp;lt;/ref&amp;gt; Alluvium of late [[Miocene]] age occurs, for example, in the valley of the [[San Joaquin River]], [[California]].&amp;lt;ref&amp;gt;{{cite book | url=https://pubs.usgs.gov/pp/1197/report.pdf | title=Amount and Timing of Late Cenozoic Uplift and Tilt of the Central Sierra Nevada, California—Evidence from the Upper San Joaquin River Basin (USGS Professional Paper 1197) | publisher=[[USGS]] | author=Huber, N. King | year=1981 | location=Washington D.C. | pages=13}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
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== See also ==&lt;br /&gt;
{{Div col|colwidth=12em}}&lt;br /&gt;
* [[Alluvial plain]]&lt;br /&gt;
* [[Bay mud]]&lt;br /&gt;
* [[Braided stream]]&lt;br /&gt;
* [[Desert pavement]]&lt;br /&gt;
* [[Eluvium]]&lt;br /&gt;
* [[Hydraulic action]]&lt;br /&gt;
* [[Illuvium]]&lt;br /&gt;
{{Div col end}}&lt;br /&gt;
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==References==&lt;br /&gt;
{{reflist}}&lt;br /&gt;
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== External links ==&lt;br /&gt;
* {{Commons category-inline}}&lt;br /&gt;
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{{authority control}}&lt;br /&gt;
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[[Category:Sedimentology]]&lt;/div&gt;</summary>
		<author><name>Aurelia2406</name></author>
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