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Statements

Subject Item
dbr:List_of_fossiliferous_stratigraphic_units_in_Missouri
dbo:wikiPageWikiLink
dbr:Bonneterre_Formation
Subject Item
dbr:Bonneterre_Formation
rdf:type
dbo:MilitaryUnit geo:SpatialThing
rdfs:label
Bonneterre Formation
rdfs:comment
The Bonneterre Formation is an Upper Cambrian geologic formation which outcrops in the St. Francois Mountains of the Missouri Ozarks. The Bonneterre is a major host rock for the lead ores of the Missouri Lead Belt. The formation is dominantly dolomite with areas or layers of pure limestone. A shaley or glauconitic zone occurs in the lower portion and the base contains sand and conglomerate or breccia where the formation overlaps the Lamotte and lies directly on the granite of the mountain core.
dbp:name
Bonneterre Formation
geo:lat
37.63600158691406
geo:long
-90.5780029296875
foaf:depiction
n15:Galena_in_dolostone_(Bonneterre_Dolomite,_Upper_Cambrian;_Flat_Rock,_Old_Lead_Belt,_Missouri,_USA)_2_(40704497164).jpg
dcterms:subject
dbc:Dolomite_formations dbc:Cambrian_Illinois dbc:Cambrian_Minnesota dbc:Cambrian_Missouri dbc:Landforms_of_the_Ozarks dbc:Guzhangian dbc:Geologic_formations_of_Minnesota dbc:Geologic_formations_of_Missouri dbc:Geologic_formations_of_Illinois dbc:Reef_deposits dbc:Cambrian_northern_paleotemperate_deposits dbc:Paleontology_in_Missouri dbc:Cambrian_System_of_North_America dbc:St._Francois_Mountains
dbo:wikiPageID
43246627
dbo:wikiPageRevisionID
1060815133
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dbr:Davis_Formation
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dbo:thumbnail
n15:Galena_in_dolostone_(Bonneterre_Dolomite,_Upper_Cambrian;_Flat_Rock,_Old_Lead_Belt,_Missouri,_USA)_2_(40704497164).jpg?width=300
dbp:age
~ dbr:Guzhangian
dbp:caption
Galena in Bonneterre Dolomite
dbp:period
Guzhangian
dbp:region
dbr:Illinois dbr:Missouri dbr:Minnesota
dbp:type
dbr:Formation_(stratigraphy)
georss:point
37.636 -90.578
dbo:abstract
The Bonneterre Formation is an Upper Cambrian geologic formation which outcrops in the St. Francois Mountains of the Missouri Ozarks. The Bonneterre is a major host rock for the lead ores of the Missouri Lead Belt. The Bonneterre Formation lies conformably on the and in places lies directly on the Proterozoic igneous core of the mountains. The Bonneterre is conformably overlain by the Davis Formation. In the outcrop area the Bonneterre has an average thickness of 375 to 400 feet. It is present in the subsurface throughout Missouri and has a maximum recorded thickness of 1580 feet under Pemiscot County in the Missouri Bootheel. The formation is dominantly dolomite with areas or layers of pure limestone. A shaley or glauconitic zone occurs in the lower portion and the base contains sand and conglomerate or breccia where the formation overlaps the Lamotte and lies directly on the granite of the mountain core.
dbp:otherlithology
dbr:Sandstone dbr:Shale dbr:Limestone
dbp:overlies
dbr:Lamotte_Sandstone
dbp:prilithology
dbr:Dolomite_(rock)
gold:hypernym
dbr:Formation
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wikipedia-en:Bonneterre_Formation?oldid=1060815133&ns=0
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5244
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wikipedia-en:Bonneterre_Formation
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POINT(-90.578002929688 37.636001586914)
Subject Item
dbr:Davis_Formation
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dbr:Bonneterre_Formation
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dbr:Bonneterre_Formation
Subject Item
dbr:Elvins_Group
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dbr:Bonneterre_Formation
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dbr:Bonneterre_Formation
Subject Item
dbr:Southeast_Missouri_Lead_District
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dbr:Bonneterre_Formation
Subject Item
dbr:Ozarks
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dbr:Bonneterre_Formation
Subject Item
dbr:Eau_Claire_Formation
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dbr:Bonneterre_Formation
Subject Item
wikipedia-en:Bonneterre_Formation
foaf:primaryTopic
dbr:Bonneterre_Formation