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Kolbeinsey Ridge

From Wikipedia, the free encyclopedia
Segment of the Mid-Atlantic Ridge north of Iceland in the Arctic Ocean
Map showing the location of the Kolbeinsey Ridge and other major geological features of the northernmost Atlantic

TheKolbeinsey Ridge is a segment of theMid-Atlantic Ridge located to the north ofIceland in the Arctic Ocean. It is bounded to the south by the Tjörnes Fracture Zone, which connects the submarine ridge to the on-shore Northern Volcanic Zone rifting center in eastern Iceland.[1] The volcanic islandsKolbeinsey andGrímsey lie along the Kolbeinsey Ridge.

Bacteria

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In 1992,Robert Huber andKarl Stetter discovered a new species ofthermophilicbacteria here and named itA. pyrophilus.[2]

See also

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References

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  1. ^G. L. Johnson; J. R. Southall; P. W. Young; P. R. Vogt (10 October 1972). "Origin and structure of the Iceland Plateau and Kolbeinsey Ridge".Journal of Geophysical Research.77 (29):5688–5696.Bibcode:1972JGR....77.5688J.doi:10.1029/JB077I029P05688.ISSN 0148-0227.Wikidata Q97487827.
  2. ^O., Huber, Robert. Stetter, Karl (1992).Aquifex pyrophilus gen. nov. sp. nov., represents a novel group of marine hyperthermophilic hydrogen-oxidizing bacteria. Fischer.OCLC 750884111.{{cite book}}: CS1 maint: multiple names: authors list (link)
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Minor plates
Microplates
Ancient plates
Oceanic ridges
Ancient oceanic ridges


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