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  • 2005-2009  (3)
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  • 1
    UID:
    gbv_607052430
    Format: 85 S , graph. Darst., Kt
    Note: Potsdam, Univ., Diss., 2009
    Additional Edition: Online-Ausg. Brune, Sascha Landslide generated tsunamis Potsdam, 2009
    Language: German
    Keywords: Hochschulschrift
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  • 2
    UID:
    gbv_607052376
    Format: Online-Ressource (PDF-Datei: 85 S., 10.066 kB) , graph. Darst., Kt
    Content: Submarine landslides can generate local tsunamis posing a hazard to human lives and coastal facilities. Two major related problems are: (i) quantitative estimation of tsunami hazard and (ii) early detection of the most dangerous landslides. This thesis focuses on both those issues by providing numerical modeling of landslide-induced tsunamis and by suggesting and justifying a new method for fast detection of tsunamigenic landslides by means of tiltmeters. Due to the proximity to the Sunda subduction zone, Indonesian coasts are prone to earthquake, but also landslide tsunamis. The aim of the GITEWS-project (German-Indonesian Tsunami Early Warning System) is to provide fast and reliable tsunami warnings, but also to deepen the knowledge about tsunami hazards. New bathymetric data at the Sunda Arc provide the opportunity to evaluate the hazard potential of landslide tsunamis for the adjacent Indonesian islands. I present nine large mass movements in proximity to Sumatra, Java, Sumbawa and Sumba, whereof the largest event displaced 20 kmđ of sediments. Using numerical modeling, I compute the generated tsunami of each event, its propagation and runup at the coast. Moreover, I investigate the age of the largest slope failures by relating them to the Great 1977 Sumba earthquake ...
    Note: Potsdam, Univ., Diss., 2009
    Additional Edition: Druckausg. Brune, Sascha Landslide generated tsunamis Potsdam, 2009
    Language: German
    Keywords: Indonesien ; Spitzbergen ; Erdrutsch ; Tsunami ; Tiltmeter ; Hochschulschrift
    URL: Volltext  (kostenfrei)
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  • 3
    UID:
    gbv_609542443
    Format: 9 , graph. Darst
    ISSN: 1525-2027
    Content: The present geological setting west of Svalbard closely parallels the situation off mid-Norway after the last glaciation, when crustal unloading by melting of ice induced very large earthquakes. Today, on the modern Svalbard margin, increasing bottom water temperatures are destabilizing marine gas hydrates, which are held in continental margin sediments consisting of interlayered contourite deposits and glacigenic debris flows. Both unloading earthquakes and hydrate failure have been identified as key factors causing several megalandslides off Norway during early Holocene deglaciation. The most prominent event was the Storegga Slide 8200 years B.P. which caused a tsunami up to 23 m high on the Faroe and Shetland islands. Here we show by numerical tsunami modeling that a smaller submarine landslide west of Svalbard, 100 m high and 130 km wide, would cause a tsunami capable of reaching northwest Europe and threatening coastal areas. A tsunami warning system based on tiltmeters would give a warning time of 1-4 h.
    In: Geochemistry, geophysics, geosystems, Hoboken, NJ : Wiley, 2000, 10(2009), 4, 1525-2027
    In: volume:10
    In: year:2009
    In: number:4
    In: extent:9
    Language: English
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