About: J-Anomaly Ridge

An Entity of Type: place, from Named Graph: http://dbpedia.org, within Data Space: dbpedia.org

The J-Anomaly Ridge is a bathymetric feature in the North Atlantic Ocean, extending southwest from the eastern end of the Grand Banks of Newfoundland. It has a length of about 400 km (250 mi) and rises 1,200 m (3,900 ft) above the general level of the Sohm Abyssal Plain. The ridge consists of anomalously thick oceanic crust that formed as a result of a major volcanic pulse during the Cretaceous.

Property	Value
dbo:abstract	The J-Anomaly Ridge is a bathymetric feature in the North Atlantic Ocean, extending southwest from the eastern end of the Grand Banks of Newfoundland. It has a length of about 400 km (250 mi) and rises 1,200 m (3,900 ft) above the general level of the Sohm Abyssal Plain. The ridge consists of anomalously thick oceanic crust that formed as a result of a major volcanic pulse during the Cretaceous. (en)
dbo:country	dbr:Canada
dbo:province	dbr:Newfoundland_and_Labrador
dbo:wikiPageExternalLink	https://www.marineregions.org/gazetteer.php%3Fp=details&id=35592%7Ctitle=Marine
dbo:wikiPageID	66710693 (xsd:integer)
dbo:wikiPageLength	1898 (xsd:nonNegativeInteger)
dbo:wikiPageRevisionID	1028083026 (xsd:integer)
dbo:wikiPageWikiLink	dbr:Cretaceous dbr:Grand_Banks_of_Newfoundland dbc:Cretaceous_volcanism dbr:Bathymetric dbc:Volcanism_of_Newfoundland_and_Labrador dbc:Underwater_ridges_of_the_Atlantic_Ocean dbc:Oceanography_of_Canada dbr:Sohm_Abyssal_Plain dbr:Oceanic_crust dbr:North_Atlantic_Ocean
dbp:wikiPageUsesTemplate	dbt:Marine-geo-stub dbt:Newfoundland-geo-stub dbt:Cite_web dbt:Convert dbt:Coord dbt:Reflist dbt:Cite_cgndb
dcterms:subject	dbc:Cretaceous_volcanism dbc:Volcanism_of_Newfoundland_and_Labrador dbc:Underwater_ridges_of_the_Atlantic_Ocean dbc:Oceanography_of_Canada
georss:point	40.5 -51.0
rdf:type	owl:Thing dbo:Place dbo:Location schema:Place geo:SpatialThing
rdfs:comment	The J-Anomaly Ridge is a bathymetric feature in the North Atlantic Ocean, extending southwest from the eastern end of the Grand Banks of Newfoundland. It has a length of about 400 km (250 mi) and rises 1,200 m (3,900 ft) above the general level of the Sohm Abyssal Plain. The ridge consists of anomalously thick oceanic crust that formed as a result of a major volcanic pulse during the Cretaceous. (en)
rdfs:label	J-Anomaly Ridge (en)
owl:sameAs	wikidata:J-Anomaly Ridge https://global.dbpedia.org/id/G1ZcD
geo:geometry	POINT(-51 40.5)
geo:lat	40.500000 (xsd:float)
geo:long	-51.000000 (xsd:float)
prov:wasDerivedFrom	wikipedia-en:J-Anomaly_Ridge?oldid=1028083026&ns=0
foaf:isPrimaryTopicOf	wikipedia-en:J-Anomaly_Ridge
is dbo:wikiPageWikiLink of	dbr:Fogo_Seamounts dbr:Outline_of_oceanography
is foaf:primaryTopic of	wikipedia-en:J-Anomaly_Ridge