About: 1955 Hawaiian submarine eruption

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

The 1955 Hawaiian submarine eruption was a submarine eruption that occurred 90 km (56 mi) northeast of Necker Island on August 20, 1955. Steaming water, water discoloration and an eruption column took place during the eruption. A possible pumice raft was also witnessed. The eruption originated about 4 km (2.5 mi) below sea level from an unnamed submarine volcano. The eruption produced a column of smoke several meters high. It is probably the westernmost historical eruption within the Hawaiian Islands. Another but less certain submarine eruption may have occurred on May 22, 1956 at the Kaʻena Ridge, 60 km (37 mi) northwest of Oʻahu in the Kaʻieʻie Waho Channel between that island and Kauaʻi.

Property Value
dbo:abstract
  • The 1955 Hawaiian submarine eruption was a submarine eruption that occurred 90 km (56 mi) northeast of Necker Island on August 20, 1955. Steaming water, water discoloration and an eruption column took place during the eruption. A possible pumice raft was also witnessed. The eruption originated about 4 km (2.5 mi) below sea level from an unnamed submarine volcano. The eruption produced a column of smoke several meters high. It is probably the westernmost historical eruption within the Hawaiian Islands. Another but less certain submarine eruption may have occurred on May 22, 1956 at the Kaʻena Ridge, 60 km (37 mi) northwest of Oʻahu in the Kaʻieʻie Waho Channel between that island and Kauaʻi. (en)
dbo:wikiPageID
  • 28710060 (xsd:integer)
dbo:wikiPageLength
  • 1714 (xsd:nonNegativeInteger)
dbo:wikiPageRevisionID
  • 1124558627 (xsd:integer)
dbo:wikiPageWikiLink
dbp:wikiPageUsesTemplate
dcterms:subject
gold:hypernym
georss:point
  • 23.583333333333332 -163.83333333333334
rdf:type
rdfs:comment
  • The 1955 Hawaiian submarine eruption was a submarine eruption that occurred 90 km (56 mi) northeast of Necker Island on August 20, 1955. Steaming water, water discoloration and an eruption column took place during the eruption. A possible pumice raft was also witnessed. The eruption originated about 4 km (2.5 mi) below sea level from an unnamed submarine volcano. The eruption produced a column of smoke several meters high. It is probably the westernmost historical eruption within the Hawaiian Islands. Another but less certain submarine eruption may have occurred on May 22, 1956 at the Kaʻena Ridge, 60 km (37 mi) northwest of Oʻahu in the Kaʻieʻie Waho Channel between that island and Kauaʻi. (en)
rdfs:label
  • 1955 Hawaiian submarine eruption (en)
owl:sameAs
geo:geometry
  • POINT(-163.83332824707 23.583333969116)
geo:lat
  • 23.583334 (xsd:float)
geo:long
  • -163.833328 (xsd:float)
prov:wasDerivedFrom
foaf:isPrimaryTopicOf
is dbo:wikiPageWikiLink of
is foaf:primaryTopic of
Powered by OpenLink Virtuoso    This material is Open Knowledge     W3C Semantic Web Technology     This material is Open Knowledge    Valid XHTML + RDFa
This content was extracted from Wikipedia and is licensed under the Creative Commons Attribution-ShareAlike 3.0 Unported License