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  • Geschichte Anfänge-  (1)
  • Icelandic rifting  (1)
  • 1
    Book
    Book
    Cambridge [u.a.] : Cambridge Univ. Press
    Keywords: Volcanism Effect of environment on ; Volcanism History ; Volcanology ; Eruption ; Vulkanismus ; Geoarchäologie ; Auswirkung ; Geschichtsschreibung ; Geschichte Anfänge- ; Eruption ; Vulkanismus ; Geoarchäologie ; Auswirkung ; Geschichtsschreibung
    Description / Table of Contents: "What does it take for a volcanic eruption to really shake the world? Did volcanic eruptions extinguish the dinosaurs, or help humans to evolve, only to decimate their populations with a super-eruption 73,000 years ago? Did they contribute to the ebb and flow of ancient empires, the French Revolution and the rise of fascism in Europe in the 19th century? These are some of the claims made for volcanic cataclysm. Volcanologist Clive Oppenheimer explores rich geological, historical, archaeological and palaeoenvironmental records (such as ice cores and tree rings) to tell the stories behind some of the greatest volcanic events of the past quarter of a billion years. He shows how a forensic approach to volcanology reveals the richness and complexity behind cause and effect, and argues that important lessons for future catastrophe risk management can be drawn from understanding events that took place even at the dawn of human origins"--
    Type of Medium: Book
    Pages: XV, 392 S. , Ill., graph. Darst., Kt. , 23 cm
    Edition: 1. publ.
    ISBN: 9780521641128 , 0521641128
    DDC: 551.21
    RVK:
    RVK:
    Language: English
    Note: Literaturverz. S. 369 - 384
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  • 2
    Publication Date: 2024-01-26
    Description: Recent Icelandic rifting events have illuminated the roles of centralized crustal magma reservoirs and lateral magma transport1-4, important characteristics of mid-ocean ridge magmatism1,5. A consequence of such shallow crustal processing of magmas4,5 is the overprinting of signatures that trace the origin, evolution and transport of melts in the uppermost mantle and lowermost crust6,7. Here we present unique insights into processes occurring in this zone from integrated petrologic and geochemical studies of the 2021 Fagradalsfjall eruption on the Reykjanes Peninsula in Iceland. Geochemical analyses of basalts erupted during the first 50 days of the eruption, combined with associated gas emissions, reveal direct sourcing from a near-Moho magma storage zone. Geochemical proxies, which signify different mantle compositions and melting conditions, changed at a rate unparalleled for individual basaltic eruptions globally. Initially, the erupted lava was dominated by melts sourced from the shallowest mantle but over the following three weeks became increasingly dominated by magmas generated at a greater depth. This exceptionally rapid trend in erupted compositions provides an unprecedented temporal record of magma mixing that filters the mantle signal, consistent with processing in near-Moho melt lenses containing 107-108 m3 of basaltic magma. Exposing previously inaccessible parts of this key magma processing zone to near-real-time investigations provides new insights into the timescales and operational mode of basaltic magma systems.
    Description: The NordSIMS ion microprobe facility acknowledges support by the Swedish Research Council (grant no. 2017-00671), the Swedish Museum of Natural History and the University of Iceland; this is NordSIMS publication no. 713. The involvement of S.A.H. was partly in relation to H2020 project EUROVOLC, funded by the European Commission (grant no. 731070). This work was supported by the Icelandic Research Fund, grant no. 228933-051. A.A. ackowledges funding from Italian Ministero Istruzione Università e Ricerca (Miur), grant PRIN2017-2017LMNLAW
    Description: Published
    Description: 529–534
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
    Keywords: Fagradalsfjall ; Icelandic rifting ; geochemistry ; petrology ; 04.08. Volcanology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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