About: Lafferty Limestone

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The Lafferty Limestone is a Middle to Late Silurian geologic formation in the Ozark Plateaus of Arkansas. The name was introduced in 1921 by Hugh Dinsmore Miser in his study of Arkansas, replacing part of the upper St. Clair Limestone. Miser designated a type locality at Tate Spring, located 1.25 miles north of the site of the old Penters Bluff railroad station in Izard County, Arkansas, however, he did not assign a stratotype. As of 2017, a reference section has not been designated for this unit.

Property	Value
dbo:abstract	The Lafferty Limestone is a Middle to Late Silurian geologic formation in the Ozark Plateaus of Arkansas. The name was introduced in 1921 by Hugh Dinsmore Miser in his study of Arkansas, replacing part of the upper St. Clair Limestone. Miser designated a type locality at Tate Spring, located 1.25 miles north of the site of the old Penters Bluff railroad station in Izard County, Arkansas, however, he did not assign a stratotype. As of 2017, a reference section has not been designated for this unit. (en)
dbo:wikiPageID	56277093 (xsd:integer)
dbo:wikiPageLength	4047 (xsd:nonNegativeInteger)
dbo:wikiPageRevisionID	942036127 (xsd:integer)
dbo:wikiPageWikiLink	dbr:List_of_fossiliferous_stratigraphic_units_in_Arkansas dbr:United_States dbr:Izard_County,_Arkansas dbr:Limestone dbr:Penters_Chert dbr:Conodont dbr:Silurian dbr:Acodus dbr:Panderodus dbr:Formation_(geology) dbr:Arkansas dbc:Silurian_Arkansas dbr:Polygnathus dbr:Spathognathodus dbr:Formation_(stratigraphy) dbr:Paleontology_in_Arkansas dbr:Ozarkodina dbr:Stratotype dbr:St._Clair_Limestone dbr:Ozark_Plateau dbr:Belodella dbr:Distacodus dbr:Hindeodella dbr:Paltodus dbr:Plectospathodus dbr:Trichonodella dbr:Lonchodina dbr:Polygnathoides dbr:Ligonodina dbr:Neoprioniodus
dbp:age	dbr:Silurian
dbp:country	dbr:United_States
dbp:name	Lafferty Limestone (en)
dbp:namedby	Hugh Dinsmore Miser (en)
dbp:namedfor	West Lafferty Creek, Izard County, Arkansas (en)
dbp:overlies	dbr:St._Clair_Limestone
dbp:prilithology	dbr:Limestone
dbp:region	dbr:Arkansas
dbp:thickness	up to 97.5 feet (en)
dbp:type	dbr:Formation_(stratigraphy)
dbp:underlies	dbr:Penters_Chert
dbp:unitof	none (en)
dbp:wikiPageUsesTemplate	dbt:Infobox_rockunit dbt:Col-begin dbt:Col-end dbt:Portal dbt:Reflist dbt:US-geologic-formation-stub dbt:Col-1-of-4 dbt:Col-2-of-4 dbt:Col-3-of-4 dbt:Col-4-of-4
dcterms:subject	dbc:Silurian_Arkansas
rdfs:comment	The Lafferty Limestone is a Middle to Late Silurian geologic formation in the Ozark Plateaus of Arkansas. The name was introduced in 1921 by Hugh Dinsmore Miser in his study of Arkansas, replacing part of the upper St. Clair Limestone. Miser designated a type locality at Tate Spring, located 1.25 miles north of the site of the old Penters Bluff railroad station in Izard County, Arkansas, however, he did not assign a stratotype. As of 2017, a reference section has not been designated for this unit. (en)
rdfs:label	Lafferty Limestone (en)
owl:sameAs	wikidata:Lafferty Limestone https://global.dbpedia.org/id/4XvQy
prov:wasDerivedFrom	wikipedia-en:Lafferty_Limestone?oldid=942036127&ns=0
foaf:isPrimaryTopicOf	wikipedia-en:Lafferty_Limestone
is dbo:wikiPageWikiLink of	dbr:Penters_Chert dbr:St._Clair_Limestone
is dbp:overlies of	dbr:Penters_Chert
is foaf:primaryTopic of	wikipedia-en:Lafferty_Limestone

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