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Titlebook: IAEG/AEG Annual Meeting Proceedings, San Francisco, California, 2018 - Volume 5; Geologic Hazards: Ea Abdul Shakoor,Kerry Cato Conference p

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IAEG/AEG Annual Meeting Proceedings, San Francisco, California, 2018 - Volume 5978-3-319-93136-4
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Neotectonics of the Hollywood Fault, Central Hollywood District, Los Angeles, California, U.S.A.ed, but rather, as now shown for the Central Hollywood District of Los Angeles, is driven mainly by crustal shortening indicated by uplift of the adjacent Santa Monica Mountains, by presence of the Hollywood Syncline and by the asymmetric (south verging), newly discovered “Yucca Street Anticline.” T
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Liquefaction Susceptibility Map of the Broader Thessaloniki Urban Arealarly in urban areas constructed in coastal areas. The first event close to an urban environment and studied in detail, was the 1906 San Francisco earthquake while the last decade, severe structural damages were induced due to soil liquefaction (CES 2010–2011, Great East Japan 2011, Emilia Romagna 2
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Fault-Landslide Interactions: Examples from the 2016 M7.8 ‘Kaikōura’, New Zealand, Earthquakehe southern extent of the rupture in northern Canterbury displays a remarkable complexity of rupture style, geometry and surface expression. Much of the surface trace is closely associated with a number of large, complex mechanism coseismic landslides. The spatial proximity of landslides and fault r
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Addressing Subsidence in Bangkok, Thailand and Houston, Texas: Scientific Comparisons and Data-Drivesubsidence occurs as a direct result of groundwater withdrawals for municipal supply, industrial use, and irrigation that depressurize and dewater aquifers. The impacts of subsidence are exacerbated in both cities because of flat, low-lying topography and the presence of unconsolidated clay layers t
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