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  • 1
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    POS 513 [POS513] Cruise Report (2017)
    GEOMAR
    In:  GEOMAR, Kiel, Germany, 18 pp.
    Details
    Publication Date: 2019-06-28
    Description: Dates, Ports: 09.05.2017 (Heraklion, Crete) – 24.05.2017 (Heraklion, Crete) Research subject: Tephrostratigraphy along the Aegean arc Chief Scientist: Dr. Armin Freundt, GEOMAR, Kiel Number of Scientists: 11 Project: Aegean Tephras
    Type: Report , NonPeerReviewed
    Format: text
    DOI: 10.3289/cr_pos513
    Location Call Number Limitation Availability
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    OceanRep: Report - Cruise Report
  • 2
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    POS522 Cruise report (2019)
    GEOMAR
    In:  GEOMAR, Kiel, Germany, 11 pp.
    Details
    Publication Date: 2019-06-26
    Description: R.V. Poseidon cruise no. 522 Dates, Ports: 10.04.2018 (Catania, Italy) – 29.04.2018 (Malaga, Spain) Research subject: Tephrostratigraphy of tsunami-related deposits at Stromboli Chief Scientist: Dr. Armin Freundt, GEOMAR, Kiel Number of Scientists: 11 Project: Stromboli tsunamis
    Type: Report , NonPeerReviewed
    Format: text
    DOI: 10.3289/cr_pos522
    Location Call Number Limitation Availability
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    OceanRep: Report - Cruise Report
  • 3
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    Volcanogenic tsunamis in lakes: examples from Nicaragua and general implications (2007)
    Birkhäuser
    In:  Pure and Applied Geophysics, 164 . pp. 527-545.
    Details
    Publication Date: 2019-09-23
    Description: This paper emphasizes the fact that tsunamis can occur in continental lakes and focuses on tsunami triggering by processes related to volcanic eruptions and instability of volcanic edifices. The two large lakes of Nicaragua, Lake Managua and Lake Nicaragua, host a section of the Central American Volcanic Arc including several active volcanoes. One case of a tsunami in Lake Managua triggered by an explosive volcanic eruption is documented in the geologic record. However, a number of events occurred in the past at both lakes which were probably tsunamigenic. These include massive intrusion of pyroclastic flows from Apoyo volcano as well as of flank-collapse avalanches from Mombacho volcano into Lake Nicaragua. Maar-forming phreatomagmatic eruptions, which repeatedly occurred in Lake Managua, are highly explosive phenomena able to create hugh water waves as was observed elsewhere. The shallow water depth of the Nicaraguan lakes is discussed as the major limiting factor of tsunami amplitude and propagation speed. The very low-profile shores facilitate substantial in-land flooding even of relatively small waves. Implications for conceiving a possible warning system are also discussed.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1007/s00024-006-0178-z
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    OceanRep: Article in a Scientific Journal - peer-reviewed
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