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Statements

Subject Item
dbr:Benton_Fault
rdf:type
owl:Thing dbo:WorldHeritageSite geo:SpatialThing
rdfs:label
Benton Fault
rdfs:comment
The Benton Fault is a geological fault in southern Pembrokeshire in Wales that was active as a normal fault during the deposition of the Old Red Sandstone during the Devonian period, forming a thick half graben. During the Carboniferous, the Benton Fault was strongly inverted as part of the Variscan Orogeny.
geo:lat
51.75
geo:long
-4.989999771118164
dct:subject
dbc:Geology_of_Wales
dbo:wikiPageID
28836782
dbo:wikiPageRevisionID
1115691874
dbo:wikiPageWikiLink
dbr:Pembrokeshire dbr:Carboniferous dbr:Inversion_(geology) dbr:Devonian dbr:List_of_geological_faults_of_Wales dbr:Old_Red_Sandstone dbc:Geology_of_Wales dbr:Half_graben dbr:Variscan_Orogeny dbr:Wales dbr:Fault_(geology)
owl:sameAs
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dbt:Use_dmy_dates dbt:Geology-stub dbt:Short_description dbt:Authority_control dbt:Coord dbt:Wales-geo-stub dbt:Reflist
georss:point
51.75 -4.99
dbo:abstract
The Benton Fault is a geological fault in southern Pembrokeshire in Wales that was active as a normal fault during the deposition of the Old Red Sandstone during the Devonian period, forming a thick half graben. During the Carboniferous, the Benton Fault was strongly inverted as part of the Variscan Orogeny.
gold:hypernym
dbr:Fault
prov:wasDerivedFrom
wikipedia-en:Benton_Fault?oldid=1115691874&ns=0
dbo:wikiPageLength
1595
foaf:isPrimaryTopicOf
wikipedia-en:Benton_Fault
geo:geometry
POINT(-4.9899997711182 51.75)