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  • 1
    Publication Date: 2020-12-14
    Description: In this paper we present the geological evidence of paleotsunamis in the Augusta area together with some paleoseismological implication derived from the discovery of multiple inundation events. It is well known that eastern Sicily has been affected in historical time by large earthquakes (CPTI Working group, 2004) and its southern sector in particular was strongly hit by the 1693 and 1169 events that were followed by devastating tsunamis. The Augusta Bay area is one of the locations where the information available from historical reports on tsunami effects (hit localities, inundated areas and run-up distribution) stimulated our curiosity in searching for the geological signature of tsunamis. The research was carried out through a multi-theme approach consisting of historical studies, geomorphological and geological surveys, coring campaigns, laboratory analyses (paleontological, radiometric, SEM, X-Ray, susceptibility, tephra, etc.).
    Description: Published
    Description: Roma
    Description: 3.2. Tettonica attiva
    Description: open
    Keywords: tsunami deposits ; Augusta Bay ; off-fault paleoseismology ; Eastern Sicily ; 04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Extended abstract
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  • 2
    Publication Date: 2017-04-04
    Description: Eastern Sicily has been affected in historical times by large earthquakes followed by devastating tsunamis, such as the 1169, 1693 and 1908 events. In order to provide a long term assessment for tsunami recurrence and related hazard, we developed a multi-disciplinary study, with a paleoseismological approach, aimed to recognize and date historical and paleo-tsunami deposits. Starting from information on the effects of known tsunamis (hit localities, inundation areas, run-up heights) and with a geomorphological approach, we selected several sites, such as coastal lakes, marshes and lagoons, potentially suitable for preserving tsunami deposits. In these sites 64 test gouge cores have been dug by hand and engine coring. In order to reconstruct paleoenvironments and to identify potential paleo-tsunami deposits, sedimentological and paleontological analyses were carried out. Magnetic and X-ray analyses were used to highlight susceptibility variations and peculiar small-scale sedimentary structures not detectable trough the standard stratigraphic analysis. Moreover, radiocarbon dating and tephra identification provide age ranges of the tsunami deposits and constrains for sedimentation rates allowing the correlation with historical events. At Capo Peloro in north-eastern Sicily, combining archaeological, historical, and C14 data, we associated two tsunami deposits, to the 1783 and 17 A.D. earthquakes. We collected also evidence for the occurrence of multiple inundations at sites in the eastern flank of Mt Etna: three events in the past 580 yr at Anguillara site and four events in the past 4000 yr at Gurna site. In south-eastern Sicily, in the Augusta bay, combining historical, tephrostratigraphical and C14 dating, we reconstructed a tsunami inundation history composed of six events in the past 4000 yr, the two most recent ones are related to the 1693 and 1169 earthquakes.
    Description: Submitted
    Description: 3.2. Tettonica attiva
    Description: open
    Keywords: tsunami deposits ; sedimentation processes ; micropaleontology ; off-fault paleoseismology ; coastal hazards ; tephra ; 04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
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  • 3
    Publication Date: 2017-04-04
    Description: The aim of this work is to present geological evidence of liquefactions triggered by earthquakes in eastern-Sicily and to analyze their characteristics. Liquefaction prone areas have been selected on the basis of the historical observations and by using aerial photographs, geological maps and field investigations.Though the difficulties caused by the intense human activity (urban settlement, industrial development, fluvial regimentation etc.), field investigations allowed us to recognize evidence of 2 liquefaction at several sites in the eastern flank of Mt. Etna and in the Catania plain to the south, where these phenomena are described by historical reports. In two sites we analyzed in details artificial exposures showing evidences of liquefaction features in the outcropping Holocene deposits: (1) the Minissale trench, in the Mascali area, and (2) the Agnone trench, in the Catania plain both placed onto the Gela foredeep.
    Description: Published
    Description: Roma
    Description: 3.2. Tettonica attiva
    Description: open
    Keywords: liquefaction ; Sicily ; off-fault paleoseismology ; historical earthquake ; 04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Extended abstract
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  • 4
    Publication Date: 2017-04-04
    Description: Eastern Sicily has been affected in historical times by large earthquakes followed by devastating tsunamis, such as the 1169, 1693 and 1908 events. In order to provide a long-term assessment for tsunami recurrence and related hazards, we developed a multi-disciplinary study, with a paleoseismo-logical approach, aimed to recognize and date historical and paleotsunami deposits. Starting from information on the effects of known tsunamis (hit localities, inundation areas, run-up heights) and with a geomorphological approach, we selected several sites—such as coastal lakes, marshes and lagoons—potentially suitable for preserving tsunami deposits. In these sites, 64 test gouge cores have been dug by hand and engine coring. In order to reconstruct paleoenvironments and to identify potential paleotsunami deposits, sedimentological and paleontological analyses were carried out. Magnetic and X-ray analyses were used to highlight susceptibility variations and peculiar small-scale sedimentary structures not detectable through the standard stratigraphic investigation. Moreover, radiocarbon dating and tephra identification provide age ranges of the tsunami deposits and constraints for sedimentation rates allowing the correlation with historical events. At Capo Peloro in northeastern Sicily, combining archaeological, historical, and C14 data, we associated two tsunami deposits with the earthquakes occurred in 1783 and 17 A.D. We also collected evidence for the occurrence of multiple inundations at sites in the eastern flank of Mt. Etna: three events in the past 580 yrs at the Anguillara site and four events in the past 4000 yrs at the Gurna site. In southeastern Sicily, in the Augusta bay, combining historical, tephrostratigraphical and C14 dating, we reconstructed a tsunami inundation history composed of six events in the past 4000 yrs; the two most recent ones are related to the 1693 and 1169 earthquakes.
    Description: Published
    Description: 109-146
    Description: 3.2. Tettonica attiva
    Description: 3.5. Geologia e storia dei vulcani ed evoluzione dei magmi
    Description: reserved
    Keywords: Tsunami deposits ; sedimentation processes ; micropaleontology ; tephra ; environmental analyses ; off-fault paleoseismology ; coastal hazards ; 04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology ; 04. Solid Earth::04.04. Geology::04.04.02. Geochronology ; 04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
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