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The geology, volcanic activity, and age of Bouvetøya, South Atlantic

dc.contributor.authorPrestvik, Tore
dc.date.accessioned2018-11-30T10:50:08Z
dc.date.available2018-11-30T10:50:08Z
dc.date.issued1982-07
dc.descriptionInternational Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.en
dc.description.abstractThe volcanic cone of Bouvetøya is built up of two formations. The older formation, of predominantly pyrodastic rocks which are typically hydrothermally altered, is overlain by a formation of mainly lava flows. The rocks present on the island constitute a transitional volcanic series. K/Ar dating indicates that surface rocks were formed as early as 1.4 Ma B.P. The rocks of Nyrøysa are 0.4-0.5 Ma, showing that this platform, which formed between 1955 and 1958, represents a landslide type deposit rather than a recent eruption as has previously been suggested by several workers. Various kinds of evidence suggest that the volcanic activity, or a cycle of activity, of Bvuvet0ya is now in a declining phase.en
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationPRESTVIK, Tore (1982). The geology, volcanic activity, and age of Bouvetøya, South Atlantic. "Arquipélago. Série Ciências da Natureza", 3: 115-123.pt_PT
dc.identifier.urihttp://hdl.handle.net/10400.3/4912
dc.language.isoengpt_PT
dc.publisherUniversidade dos Açorespt_PT
dc.subjectGeologyen
dc.subjectVolcanismen
dc.titleThe geology, volcanic activity, and age of Bouvetøya, South Atlanticen
dc.typejournal article
dspace.entity.typePublication
oaire.citation.conferencePlacePonta Delgada, Açorespt_PT
oaire.citation.endPage123pt_PT
oaire.citation.startPage115pt_PT
oaire.citation.titleArquipélago. Série Ciências da Naturezapt_PT
oaire.citation.volume3pt_PT
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT

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