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Evidence of recent volcanic activity on the ultraslow-spreading Gakkel ridge

Author

Listed:
  • M. H. Edwards

    (Hawaii Institute of Geophysics and Planetology, POST 815;)

  • G. J. Kurras

    (University of Hawaii at Manoa)

  • M. Tolstoy

    (Lamont-Doherty Earth Observatory, Columbia University)

  • D. R. Bohnenstiehl

    (Lamont-Doherty Earth Observatory, Columbia University)

  • B. J. Coakley

    (Tulane University)

  • J. R. Cochran

    (Lamont-Doherty Earth Observatory, Columbia University)

Abstract

Seafloor spreading is accommodated by volcanic and tectonic processes along the global mid-ocean ridge system. As spreading rate decreases the influence of volcanism also decreases1,2,3,4, and it is unknown whether significant volcanism occurs at all at ultraslow spreading rates (

Suggested Citation

  • M. H. Edwards & G. J. Kurras & M. Tolstoy & D. R. Bohnenstiehl & B. J. Coakley & J. R. Cochran, 2001. "Evidence of recent volcanic activity on the ultraslow-spreading Gakkel ridge," Nature, Nature, vol. 409(6822), pages 808-812, February.
    • Handle: RePEc:nat:nature:v:409:y:2001:i:6822:d:10.1038_35057258
    DOI: 10.1038/35057258
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    Cited by:

    1. Ivan Koulakov & Vera Schlindwein & Mingqi Liu & Taras Gerya & Andrey Jakovlev & Aleksey Ivanov, 2022. "Low-degree mantle melting controls the deep seismicity and explosive volcanism of the Gakkel Ridge," Nature Communications, Nature, vol. 13(1), pages 1-10, December.
    2. Zhiteng Yu & Satish C. Singh, 2023. "Increase of P-wave velocity due to melt in the mantle at the Gakkel Ridge," Nature Communications, Nature, vol. 14(1), pages 1-3, December.

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