Smackover Formation
{{Short description|Geological formation in southeastern U.S.}}
{{Infobox rockunit
| name = Smackover Formation
| image = Smackover Formation areal extent.png
| caption = Wells reporting Smackover Formation tops are indicated by a black point, and extend from Texas to Florida. Formation top depths measured in 6,764 wells range from 1,394 to 23,554 feet.
| type = Formation
| age = Oxfordian
| period = Oxfordian
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| region = Arkansas, Louisiana, Texas, Alabama, Mississippi, and Florida
| country = United States
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| underlies = Buckner Formation
| overlies = Norphlet Formation
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The Smackover Formation is a geologic formation that extends under parts of Arkansas, Louisiana, Texas, Alabama, Mississippi, and Florida.{{cite web|url=https://www.usgs.gov/news/national-news-release/unlocking-arkansas-hidden-treasure-usgs-uses-machine-learning-show-large|author=U.S. Geological Survey|title=USGS Uses Machine Learning to Show Large Lithium Potential in the Smackover Formation|date=October 21, 2024|accessdate=October 24, 2024}} It preserves fossils dating back to the Jurassic period. The formation is a relic of an ancient sea that left an extensive, porous, and permeable limestone geologic unit.
The Smackover Formation consists of oolitic limestones and silty limestones.{{cite book|last1=Dickinson|first1=Kendell|title=Upper Jurassic Stratigraphy of Some Adjacent Parts of Texas, Louisiana, and Arkansas|date=1968|publisher=USGS|page=E9}}{{cite book|last1=Chimene|first1=Calvin|editor1-last=Braunstein|editor1-first=Jules|title=Upper Smackover Reservoirs, Walker Creek Field Area, Lafayette and Columbia Counties, Arkansas, in North American Oil and Gas Fields|date=1976|publisher=The American Association of Petroleum Geologists|location=Tulsa|isbn=0891813004|pages=177–204}}
Mineral resources
File:Louann Salt stratigraphic column for Texas.png for Texas]]
The Smackover Formation has been a prolific source of petroleum. The 1922 discovery of the Smackover oil field, after which the Smackover Formation is named, resulted in a sizeable oil boom in southern Arkansas.{{cn|date=May 2024}}
In addition to being a petroleum reservoir, as of 2015, the brine from the Smackover Formation is the only source of commercial bromine in the United States.{{cite web|title= Fossilworks: Gateway to the Paleobiology Database|author= ((Various Contributors to the Paleobiology Database))|url= https://www.fossilworks.org|access-date= 17 December 2021|df= }}
A 2022 report estimated that the lithium brine in the formation has "sufficient lithium to produce enough batteries for 50 million electric vehicles."{{Cite web |date=2022-07-13 |title=Resource report concludes Galvanic’s lithium prospect among most prolific in North America |url=https://www.greencarcongress.com/2022/07/20220713-galvanic.html |access-date=2022-08-27 |website=Green Car Congress}} In October 2024, federal and state researchers announced the formation may hold five to 19 million tons of lithium, which is about nine times the annual worldwide demand for electric vehicles projected for 2030.{{cite news |last1=Penn |first1=Ivan |last2=Elliott |first2=Rebecca F. |title=Arkansas May Have Vast Lithium Reserves, Researchers Say |url=https://www.nytimes.com/2024/10/21/business/energy-environment/arkansas-lithium-ev-batteries.html |access-date=23 October 2024 |work=New York Times |date=October 21, 2024}}
File:Smackover and Bossier Formations geologic cross section.png
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See also
{{Portal|Earth sciences|United States|Paleontology}}
References
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