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Showing 1–4 of 4 results
Advanced filters: Author: Cecily J. Wolfe Clear advanced filters

  • Over the past decade, Kīlauea and Mauna Loa—adjacent volcanoes in Hawai‘i—have inflated and deflated in tandem, yet their shallow volcanic plumbing systems are separate. Numerical modelling of the volcanoes shows that dynamic stress transfer by asthenospheric pore pressure is a viable mechanism for volcano coupling in Hawai‘i.

    • Helge M. Gonnermann
    • James H. Foster
    • Asta Miklius
    Research
    Nature Geoscience
    Volume: 5, P: 826-829

  • Oceanic islands such as Iceland and Hawaii are thought to be the result of upwelling plumes of material from within the Earth's mantle. But at what depth do such plumes originate? New seismological analyses place the source as far down as the core-mantle boundary, 2,900 km beneath the Earth's surface.

    • Cecily J. Wolfe
    News & Views
    Nature
    Volume: 396, P: 212-213