Perspectives on Tsunami Hazard Reduction [electronic resource] : Observations, Theory and Planning /

The promontory of Gargano in the southern Adriatic Sea represents one of the most interesting Italian coastal zones subjected to tsunami hazard. Figure la gives the geographical map of Italy; with a box embracing the region of Gargano; details of that region are in turn sketched in Figure lb. Because of the incompleteness of the earthquake and tsunami catalogues, no reports on tsunamis in this area are available prior to 1600 AD. The Gargano events have been recently revised in order to establish their reliability and to attain the phenomenological reconstruction of the tsunamis (Guidoboni and Tinti, 1987 and 1988; Tinti et. al. , 1995). This work fits the general purpose of assessing tsunami hazard along the Italian coasts and represents a continuation of a previous study, where the first quantitative description of the 1627 tsunami from a numerical modeling viewpoint was performed (Tinti and Piatanesi, 1996). The earthquake took place on 30 July 1627 about mid-day and was followed by four large aftershocks. It claimed more than 5,000 victims and destroyed completely numerous villages in the northern Gargano area, with the most severe damage located between S. Severo and Lesina. The earthquake excited a tsunami with the most impressive effects in proximity of the Lesina Lake where the most reliable contemporary chronicles report about an initial sea water withdrawal of about 2 miles and a subsequent penetration inland.

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Main Authors: Hebenstreit, Gerald. editor., SpringerLink (Online service)
Format: Texto biblioteca
Language:eng
Published: Dordrecht : Springer Netherlands : Imprint: Springer, 1997
Subjects:Earth sciences., Geophysics., Hydrogeology., Oceanography., Environmental management., Ecotoxicology., Earth Sciences., Geophysics/Geodesy., Environmental Management.,
Online Access:http://dx.doi.org/10.1007/978-94-015-8859-1
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id KOHA-OAI-TEST:192454
record_format koha
institution COLPOS
collection Koha
country México
countrycode MX
component Bibliográfico
access En linea
En linea
databasecode cat-colpos
tag biblioteca
region America del Norte
libraryname Departamento de documentación y biblioteca de COLPOS
language eng
topic Earth sciences.
Geophysics.
Hydrogeology.
Oceanography.
Environmental management.
Ecotoxicology.
Earth Sciences.
Hydrogeology.
Oceanography.
Geophysics/Geodesy.
Ecotoxicology.
Environmental Management.
Earth sciences.
Geophysics.
Hydrogeology.
Oceanography.
Environmental management.
Ecotoxicology.
Earth Sciences.
Hydrogeology.
Oceanography.
Geophysics/Geodesy.
Ecotoxicology.
Environmental Management.
spellingShingle Earth sciences.
Geophysics.
Hydrogeology.
Oceanography.
Environmental management.
Ecotoxicology.
Earth Sciences.
Hydrogeology.
Oceanography.
Geophysics/Geodesy.
Ecotoxicology.
Environmental Management.
Earth sciences.
Geophysics.
Hydrogeology.
Oceanography.
Environmental management.
Ecotoxicology.
Earth Sciences.
Hydrogeology.
Oceanography.
Geophysics/Geodesy.
Ecotoxicology.
Environmental Management.
Hebenstreit, Gerald. editor.
SpringerLink (Online service)
Perspectives on Tsunami Hazard Reduction [electronic resource] : Observations, Theory and Planning /
description The promontory of Gargano in the southern Adriatic Sea represents one of the most interesting Italian coastal zones subjected to tsunami hazard. Figure la gives the geographical map of Italy; with a box embracing the region of Gargano; details of that region are in turn sketched in Figure lb. Because of the incompleteness of the earthquake and tsunami catalogues, no reports on tsunamis in this area are available prior to 1600 AD. The Gargano events have been recently revised in order to establish their reliability and to attain the phenomenological reconstruction of the tsunamis (Guidoboni and Tinti, 1987 and 1988; Tinti et. al. , 1995). This work fits the general purpose of assessing tsunami hazard along the Italian coasts and represents a continuation of a previous study, where the first quantitative description of the 1627 tsunami from a numerical modeling viewpoint was performed (Tinti and Piatanesi, 1996). The earthquake took place on 30 July 1627 about mid-day and was followed by four large aftershocks. It claimed more than 5,000 victims and destroyed completely numerous villages in the northern Gargano area, with the most severe damage located between S. Severo and Lesina. The earthquake excited a tsunami with the most impressive effects in proximity of the Lesina Lake where the most reliable contemporary chronicles report about an initial sea water withdrawal of about 2 miles and a subsequent penetration inland.
format Texto
topic_facet Earth sciences.
Geophysics.
Hydrogeology.
Oceanography.
Environmental management.
Ecotoxicology.
Earth Sciences.
Hydrogeology.
Oceanography.
Geophysics/Geodesy.
Ecotoxicology.
Environmental Management.
author Hebenstreit, Gerald. editor.
SpringerLink (Online service)
author_facet Hebenstreit, Gerald. editor.
SpringerLink (Online service)
author_sort Hebenstreit, Gerald. editor.
title Perspectives on Tsunami Hazard Reduction [electronic resource] : Observations, Theory and Planning /
title_short Perspectives on Tsunami Hazard Reduction [electronic resource] : Observations, Theory and Planning /
title_full Perspectives on Tsunami Hazard Reduction [electronic resource] : Observations, Theory and Planning /
title_fullStr Perspectives on Tsunami Hazard Reduction [electronic resource] : Observations, Theory and Planning /
title_full_unstemmed Perspectives on Tsunami Hazard Reduction [electronic resource] : Observations, Theory and Planning /
title_sort perspectives on tsunami hazard reduction [electronic resource] : observations, theory and planning /
publisher Dordrecht : Springer Netherlands : Imprint: Springer,
publishDate 1997
url http://dx.doi.org/10.1007/978-94-015-8859-1
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spelling KOHA-OAI-TEST:1924542018-07-30T23:16:50ZPerspectives on Tsunami Hazard Reduction [electronic resource] : Observations, Theory and Planning / Hebenstreit, Gerald. editor. SpringerLink (Online service) textDordrecht : Springer Netherlands : Imprint: Springer,1997.engThe promontory of Gargano in the southern Adriatic Sea represents one of the most interesting Italian coastal zones subjected to tsunami hazard. Figure la gives the geographical map of Italy; with a box embracing the region of Gargano; details of that region are in turn sketched in Figure lb. Because of the incompleteness of the earthquake and tsunami catalogues, no reports on tsunamis in this area are available prior to 1600 AD. The Gargano events have been recently revised in order to establish their reliability and to attain the phenomenological reconstruction of the tsunamis (Guidoboni and Tinti, 1987 and 1988; Tinti et. al. , 1995). This work fits the general purpose of assessing tsunami hazard along the Italian coasts and represents a continuation of a previous study, where the first quantitative description of the 1627 tsunami from a numerical modeling viewpoint was performed (Tinti and Piatanesi, 1996). The earthquake took place on 30 July 1627 about mid-day and was followed by four large aftershocks. It claimed more than 5,000 victims and destroyed completely numerous villages in the northern Gargano area, with the most severe damage located between S. Severo and Lesina. The earthquake excited a tsunami with the most impressive effects in proximity of the Lesina Lake where the most reliable contemporary chronicles report about an initial sea water withdrawal of about 2 miles and a subsequent penetration inland.Tsunami Observations -- Coastal Effects and Damage Due to the 3rd June, 1994 Java Tsunami -- Expert Tsunami Database for the Pacific: Motivation, Design, and Proof-of-Concept Demonstration -- Local Responses to the October 4, 1994 Tsunami Warning: Washington, Oregon, and California -- Precise Tsunami Observation System in the Deep Ocean by an Ocean Bottom Cable Network for the Prediction of Earthquakes and Tsunamis -- Tsunami Theory -- Asperity Distribution of Alaskan-Aleutian Earthquakes: Implications for Seismic and Tsunami Hazards -- Numerical Simulation of 1993 July 12 Tsunami Near Hokkaido: Its Propagation and Flooding onto Aonae District, Okushiri Island -- Inverse and Forward Tsunami Modeling of the 1993 Hokkaido Tsunami -- Numerical Simulations of the 1627 Gargano Tsunami (Southern Italy) to Locate the Earthquake Source -- Tsunami Detection and Warning Capability using Nearshore Submerged Pressure Transducers — Case Study of the 4 October 1994 Shikotan Tsunami -- Short-Term Forecasts of Inundation During Teletsunamis in the Eastern North Pacific Ocean -- A Natural Warning of Tsunami Arrival -- Tsunami Hazard Planning -- The New Tsunami Warning System of the Japan Meteorological Agency -- Reducing Tsunami Hazards Along U.S. Coastlines -- Overview -- A Long-term Perspective.The promontory of Gargano in the southern Adriatic Sea represents one of the most interesting Italian coastal zones subjected to tsunami hazard. Figure la gives the geographical map of Italy; with a box embracing the region of Gargano; details of that region are in turn sketched in Figure lb. Because of the incompleteness of the earthquake and tsunami catalogues, no reports on tsunamis in this area are available prior to 1600 AD. The Gargano events have been recently revised in order to establish their reliability and to attain the phenomenological reconstruction of the tsunamis (Guidoboni and Tinti, 1987 and 1988; Tinti et. al. , 1995). This work fits the general purpose of assessing tsunami hazard along the Italian coasts and represents a continuation of a previous study, where the first quantitative description of the 1627 tsunami from a numerical modeling viewpoint was performed (Tinti and Piatanesi, 1996). The earthquake took place on 30 July 1627 about mid-day and was followed by four large aftershocks. It claimed more than 5,000 victims and destroyed completely numerous villages in the northern Gargano area, with the most severe damage located between S. Severo and Lesina. The earthquake excited a tsunami with the most impressive effects in proximity of the Lesina Lake where the most reliable contemporary chronicles report about an initial sea water withdrawal of about 2 miles and a subsequent penetration inland.Earth sciences.Geophysics.Hydrogeology.Oceanography.Environmental management.Ecotoxicology.Earth Sciences.Hydrogeology.Oceanography.Geophysics/Geodesy.Ecotoxicology.Environmental Management.Springer eBookshttp://dx.doi.org/10.1007/978-94-015-8859-1URN:ISBN:9789401588591