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  • 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring  (19)
  • Seismicity  (8)
  • Stromboli  (8)
  • Italy  (7)
Collection
  • 1
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    In:  Eos, Trans., Am. Geophys. Un., Leipzig, Birkhäuser Verlag, vol. 71, no. 46, pp. 1787-1788, pp. 2458, (ISBN: 0-12-018847-3)
    Publication Date: 1990
    Keywords: Seismicity ; Fault zone ; Migration of earthquakes ; Geol. aspects
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  • 2
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    In:  Eos Trans. AGU, Luxembourg, Conseil de l'Europe, vol. 86, no. 28, pp. 261 & 266, pp. L09602, (ISSN: 1340-4202)
    Publication Date: 2005
    Description: The digital preservation of the unique seismological heritage consisting of historical seismograms and earthquake bulletins, and of related documentation (e.g., observatory logbooks, station books, etc.), is critically important in order to avoid deterioration and loss over time [Kanamori, 1988]. Dissemination of this seismological material in digital form is of equal importance, to allow reanalysis of past earthquakes using modern techniques and the reevaluation of seismic hazard. This is of particular interest for those areas where little or no earthquake activity has occurred since the last significant historical earthquake. In 2001, the Istituto Nazionale di Geofisica e Vulcanologia (INGV) started an innovative project, Progetto SISMOS (i.e., Sismogrammi Storici), to scan (i.e., convert into digital form for storage on a computer), at very high resolution, and archive seismological paper records and related material. The Italian Ministry for the Environment originally funded the project to encompass the digitization of seismogram records of the Italian seismic observatories and of associated bulletins for the period 1895-1984 (i.e., from the early age of seismometry to the advent of the digital era)
    Keywords: digital ; historical ; Earthquake catalog ; Seismology ; Seismicity ; INGV ; Italy ; Europe ; Wave form analysis ; Simoni ; 7299 ; Seismology: ; General ; or ; miscellaneous ; 7294 ; Seismic ; instruments ; and ; networks ; 1734 ; History ; of ; Geophysics: ; Seismology
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  • 3
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    In:  Earth planet. Sci. Lett., Hannover, Conseil de l'Europe, vol. 204, no. 3-4, pp. 363-372, pp. L04301, (ISSN: 1340-4202)
    Publication Date: 2002
    Keywords: Fault zone ; Seismicity ; Rheology ; Statistical investigations ; post-seismic ; Stress ; Coulomb
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  • 4
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    In:  Bull. Seism. Soc. Am., Leipzig, Birkhäuser Verlag, vol. 85, no. 46, pp. 1475-1482, pp. 2458, (ISBN: 0-12-018847-3)
    Publication Date: 1995
    Keywords: Statistical investigations ; Earthquake hazard ; Earthquake precursor: prediction research ; Seismicity ; BSSA
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  • 5
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    In:  Earth planet. Sci. Lett., Luxembourg, Deutsche Geophys. Gesellschaft, vol. 226, no. 3-4, pp. 383-395, pp. 2417, (ISSN: 1340-4202)
    Publication Date: 2004
    Keywords: Seismicity ; Volcanology ; long ; distance ; triggering ; Earthquake ; Stress ; EPSL
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  • 6
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    Il Cigno Galileo Galilei
    In:  Roma, Il Cigno Galileo Galilei, vol. 70, pp. 158, (ISBN 3-9808780-0-7)
    Publication Date: 1992
    Keywords: Earthquake precursor: prediction research ; Japan ; China ; Italy ; Volcanology ; Russia ; Earthquake precursor: tilt ; Earthquake precursor: chemical (Rn, water(-level,...) ; Earthquake precursor: statistical anal. of seismicity ; Seismicity ; JZSCHAU
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  • 7
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    In:  Geophys. J. Int., Stockholm, Wissenschaftliche Buchgesellschaft, vol. 122, no. 1-2, pp. 938-952, pp. L15318, (ISSN: 1340-4202)
    Publication Date: 1995
    Keywords: Moment tensor ; Seismicity ; Tectonics ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; GJI
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  • 8
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    Kluwer Acad. Publ.
    In:  Dordrecht, Kluwer Acad. Publ., vol. 70, pp. 158, (ISBN 3-9808780-0-7)
    Publication Date: 1993
    Keywords: Tectonics ; Seismicity ; Greece ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geol. aspects ; Plate tectonics
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  • 9
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2013-09-28
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Boschi, Enzo -- New York, N.Y. -- Science. 2013 Sep 27;341(6153):1451. doi: 10.1126/science.341.6153.1451.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24072904" target="_blank"〉PubMed〈/a〉
    Keywords: *Cause of Death ; Disaster Planning/*legislation & jurisprudence ; *Earthquakes ; Humans ; Information Dissemination/*legislation & jurisprudence ; Italy
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 10
    Publication Date: 2021-06-09
    Description: The 11–13 January 2011 eruptive episode at Etna volcano occurred after several months of increasing ash emissions from the summit craters, and was heralded by increasing SO2 output, which peaked at ∼5000 megagrams/day several hours before the start of the eruptive activity. The eruptive episode began with a phase of Strombolian activity from a pit crater on the eastern flank of the SE‐Crater. Explosions became more intense with time and eventually became transitional between Strombolian and fountaining, before moving into a lava fountaining phase. Fountaining was accompanied by lava output from the lower rim of the pit crater. Emplacement of the resulting lava flow field, as well as associated lava fountain‐ and Strombolian‐phases, was tracked using a remote sensing network comprising both thermal and visible cameras. Thermal surveys completed once the eruptive episode had ended also allowed us to reconstruct the emplacement of the lava flow field. Using a high temporal resolution geostationary satellite data we were also able to construct a detailed record of the heat flux during the fountain‐fed flow phase and its subsequent cooling. The dense rock volume of erupted lava obtained from the satellite data was 1.2 × 106 m3; this was emplaced over a period of about 6 h to give a mean output rate of ∼55 m3 s−1. By comparison, geologic data allowed us to estimate dense rock volumes of ∼0.85 × 106 m3 for the pyroclastics erupted during the lava fountain phase, and 0.84–1.7 × 106 m3 for lavas erupted during the effusive phase, resulting in a total erupted dense rock volume of 1.7–2.5 × 106 m3 and a mean output rate of 78–117 m3 s−1. The sequence of events and quantitative results presented here shed light on the shallow feeding system of the volcano.
    Description: Published
    Description: B11207
    Description: 1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcani
    Description: JCR Journal
    Description: partially_open
    Keywords: Etna ; lava fountains ; 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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