Greenbrier Group (original) (raw)

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The Greenbrier Limestone, also known locally as the "Big Lime", is an extensive limestone unit deposited during the Middle Mississippian Epoch (345.3 ± 2.1 – 326.4 ± 1.6 Ma), part of the Carboniferous Period. This rock stratum is present below ground in much of West Virginia and neighboring Kentucky, and extends somewhat into adjacent western Maryland and southwestern Virginia. The name derives from the Greenbrier River in West Virginia. Numerous solution caves are developed within the Greenbrier Formation.

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dbo:abstract The Greenbrier Limestone, also known locally as the "Big Lime", is an extensive limestone unit deposited during the Middle Mississippian Epoch (345.3 ± 2.1 – 326.4 ± 1.6 Ma), part of the Carboniferous Period. This rock stratum is present below ground in much of West Virginia and neighboring Kentucky, and extends somewhat into adjacent western Maryland and southwestern Virginia. The name derives from the Greenbrier River in West Virginia. Greenbrier Limestone is in some places more than 400 feet (120 metres) thick, allowing it to trap large quantities of oil and gas. Since this carbonate rock erodes quickly in the region's wet climate, outcrops are not prominent and are often quarried. The Greenbrier Limestone is subdivided into six stratigraphic units. In ascending order, they are , , , , , and . The limestones in this interval are predominantly skeletal grainstones or packstones. The Pickaway and especially the Union contain oolitic grainstones. Numerous solution caves are developed within the Greenbrier Formation. (en) Le calcaire de Greenbrier (en anglais Greenbrier Limestone, connu localement sous le nom de Big Lime) est une formation calcaire, qui s'est déposée pendant le Viséen (ou Mississippien moyen, 345.3 ± 2.1 – 326.4 ± 1.6 Ma) et qui s'étend sur toute la Virginie-Occidentale, le Kentucky, l'ouest du Maryland et le sud-ouest de la Virginie. Il est ainsi nommé en référence à la rivière . La couche a par endroits plus de 120 mètres d'épaisseur et contient des gisements de pétrole et de gaz. Le calcaire de Greenbrier est divisé en six unités stratigraphiques, qui sont, dans un ordre ascendant : le calcaire de Denmar ; le schiste de Taggard ; le calcaire de Pickaway ; le calcaire de l'Union ; le schiste de Greenville et le calcaire d'Alderson. En Virginie-Occidentale, le calcaire comporte de nombreuses grottes. * Portail de la géologie * Portail des États-Unis (fr)
dbo:thumbnail wiki-commons:Special:FilePath/SinksofGandyCreek1.jpg?width=300
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dbo:wikiPageLength 2938 (xsd:nonNegativeInteger)
dbo:wikiPageRevisionID 1117419346 (xsd:integer)
dbo:wikiPageWikiLink dbr:Carboniferous dbr:Price_Formation dbr:Oolite dbc:Carboniferous_West_Virginia dbc:Geologic_formations_of_West_Virginia dbc:Mississippian_United_States dbr:United_States dbr:Virginia dbr:Limestone dbr:Maryland dbr:Geology_of_West_Virginia dbr:Mississippian_age dbr:Sinks_of_Gandy dbr:Maccrady_Formation dbr:Stratum dbc:Limestone_formations_of_the_United_States dbr:West_Virginia dbr:Allegheny_Mountains dbr:Carbonate_rock dbr:Grainstone dbr:Greenbrier_River dbr:Kentucky dbr:Bluefield_Formation dbr:Solutional_cave dbr:Geological_unit dbr:List_of_types_of_limestone dbr:Packstone dbr:Stratigraphic dbr:Mississippian_epoch dbr:Alderson_Limestone dbr:Denmar_Limestone dbr:Greenville_Shale dbr:Pickaway_Limestone dbr:Taggard_Shale dbr:Union_Limestone
dbp:age Middle Mississippian (en)
dbp:caption The Sinks of Gandy is developed in the Greenbrier Limestone Formation in West Virginia. (en)
dbp:country dbr:United_States
dbp:extent Kentucky, Maryland, Virginia, and West Virginia (en)
dbp:name Greenbrier Limestone (en)
dbp:namedfor dbr:Greenbrier_River
dbp:overlies Maccrady Formation and Price Formation (en)
dbp:period Mississippian (en)
dbp:prilithology dbr:Limestone
dbp:region dbr:Allegheny_Mountains
dbp:subunits Denmar Limestone, Taggard Shale, Pickaway Limestone, Union Limestone, Greenville Shale, and Alderson Limestone. (en)
dbp:thickness 120 m (en)
dbp:type sedimentary (en)
dbp:underlies dbr:Bluefield_Formation
dbp:wikiPageUsesTemplate dbt:Infobox_rockunit dbt:Short_description dbt:Stratigraphic_column_of_West_Virginia dbt:Chronostratigraphy_of_Maryland dbt:Chronostratigraphy_of_Virginia dbt:WestVirginia-geologic-formation-stub
dct:subject dbc:Carboniferous_West_Virginia dbc:Geologic_formations_of_West_Virginia dbc:Mississippian_United_States dbc:Limestone_formations_of_the_United_States
rdfs:comment The Greenbrier Limestone, also known locally as the "Big Lime", is an extensive limestone unit deposited during the Middle Mississippian Epoch (345.3 ± 2.1 – 326.4 ± 1.6 Ma), part of the Carboniferous Period. This rock stratum is present below ground in much of West Virginia and neighboring Kentucky, and extends somewhat into adjacent western Maryland and southwestern Virginia. The name derives from the Greenbrier River in West Virginia. Numerous solution caves are developed within the Greenbrier Formation. (en) Le calcaire de Greenbrier (en anglais Greenbrier Limestone, connu localement sous le nom de Big Lime) est une formation calcaire, qui s'est déposée pendant le Viséen (ou Mississippien moyen, 345.3 ± 2.1 – 326.4 ± 1.6 Ma) et qui s'étend sur toute la Virginie-Occidentale, le Kentucky, l'ouest du Maryland et le sud-ouest de la Virginie. Il est ainsi nommé en référence à la rivière . La couche a par endroits plus de 120 mètres d'épaisseur et contient des gisements de pétrole et de gaz. En Virginie-Occidentale, le calcaire comporte de nombreuses grottes. (fr)
rdfs:label Calcaire de Greenbrier (fr) Greenbrier Group (en)
owl:sameAs yago-res:Greenbrier Group wikidata:Greenbrier Group dbpedia-fr:Greenbrier Group https://global.dbpedia.org/id/2iuwR
prov:wasDerivedFrom wikipedia-en:Greenbrier_Group?oldid=1117419346&ns=0
foaf:depiction wiki-commons:Special:FilePath/SinksofGandyCreek1.jpg
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is dbp:overlies of dbr:Bluefield_Formation
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is foaf:primaryTopic of wikipedia-en:Greenbrier_Group