ingv:https://data.ingv.it/metadata/iso19115/420.xml
eng
utf8
dataset
Istituto Nazionale di Geofisica e Vulcanologia - INGV
ufficiogestionedati@ingv.it
http://istituto.ingv.it/it/ufficio-gestione-dati
pointOfContact
2024-01-23
Linee Guida RNDT
2.0
WGS84
Historical catalog of Major explosions and paroxysms at Stromboli (Italy)
Catalogo storico di esplosioni maggiori e parossismi di Stromboli
2020-07
publication
1.1
ingv:https://doi.org/10.13127/stromboli/strcatalog
Istituto Nazionale di Geofisica e Vulcanologia - INGV
ufficiogestionedati@ingv.it
http://www.ingv.it
owner
Istituto Nazionale di Geofisica e Vulcanologia - INGV
ufficiogestionedati@ingv.it
http://istituto.ingv.it/it/ufficio-gestione-dati
resourceProvider
Istituto Nazionale di Geofisica e Vulcanologia - INGV
ufficiogestionedati@ingv.it
http://istituto.ingv.it/it/ufficio-gestione-dati
publisher
Bevilacqua, Andrea
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
andrea.bevilacqua@ingv.it
https://orcid.org/0000-0002-0724-2593
ORCID
author
Pompilio, Massimo
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
massimo.pompilio@ingv.it
https://orcid.org/0000-0002-0742-0679
ORCID
author
Landi, Patrizia
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
patrizia.landi@ingv.it
https://orcid.org/0000-0002-8463-5710
ORCID
author
Del Carlo, Paola
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
paola.delcarlo@ingv.it
https://orcid.org/0000-0001-5506-4579
ORCID
author
Di Roberto, Alessio
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
alessio.diroberto@ingv.it
https://orcid.org/0000-0003-1167-8290
ORCID
author
Piccione, Caterina
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
caterina.piccione@ingv.it
https://orcid.org/0000-0001-5873-307X
ORCID
author
Neri, Augusto
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
augusto.neri@ingv.it
https://orcid.org/0000-0002-3536-3624
ORCID
author
ingv:https://doi.org/10.13127/stromboli/strcatalog
This is the dataset of the major explosions and paroxysms record at Stromboli from 1879 to 1960, as reconstructed through a detailed review of scientific literature of the last ca. 145 years. The catalog includes the calendar date and phenomena descriptions for 125 explosive events, of which 36 were paroxysms.
We summarized the event information content in five columns - (i) noise and earthquakes, (ii) ash plume, (iii) large ejecta, (iv) PDC and tsunami, (v) lava flows. Where possible, the extracts contained the description of any volcanic activity at least one month before the eruption and one month after. The catalog also includes a sequence of extracts from the original literature sources that helped us in the complex characterization of the less recent events. When that was possible, we relied on the detailed definition of major explosions and paroxysms in [Rosi et al., 2013, Geol Soc Lon Mem 37, 475–492]. In other cases, we had to utilize the original definitions in [Barberi et al., 1993, Acta Vulcanol 3, 173-187], due to the lack of enough quantitative information in the historical sources.
In general, while we reached a consensus about all the paroxysms, several possible major explosions remained not clearly distinguishable from particularly violent episodes of Strombolian activity. Thus, our historical record also includes the quantification of the main sources of uncertainty, i.e. the possibility of major explosions of uncertain characterization because of insufficient information. We thus categorized as uncertain 48 major explosions.
completed
Bevilacqua, Andrea
Istituto Nazionale di Geofisica e Vulcanologia - INGV
andrea.bevilacqua@ingv.it
https://orcid.org/0000-0002-0724-2593
ORCID
pointOfContact
irregular
https://data.ingv.it/dataset/cover/420.jpg
thumbnail
image/jpeg
EU
open data
Local
Spatial scope
2019-05-22
publication
SCIENCE.natural and applied sciences.earth sciences.geology.volcanology
EuroVoc
2020-09-04T10:40:44
publication
Natural risk zones
GEMET - INSPIRE themes, version 1.0
2008-06-01
publication
paroxysms
major explosions
theme
otherRestrictions
Creative Commons Attribution 4.0 International (CC BY 4.0)
otherRestrictions
no limitations to public access
http://publications.europa.eu/resource/authority/licence/CC_BY
unclassified
vector
1000
eng
utf8
geoscientificInformation
Stromboli, Italy
Stromboli
15.19
15.24
38.77
38.81
1879-02-04
1975-11-05
Stromboli
15.2141, 38.7913
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
ufficiogestionedati@ingv.it
http://www.ingv.it
distributor
https://www.pi.ingv.it/banche-dati/historical-catalog-of-major-explosions-and-paroxysms-at-stromboli-italy/
WWW:LINK-1.0-http--link
other
homepage
accessPoint
dataset
m
1
Commission Regulation (EU) No 1089/2010 of 23 November 2010 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards interoperability of spatial data sets and services
2010-12-08
Publication
This data set is conformant with the INSPIRE Implementing Rules for the interoperability of spatial data sets and services
true
We considered the area affected by large ballistic projectiles as the main discriminant factor to distinguish between normal activity, major explosions and paroxysms. This area is limited to the Crater Terrace in case of normal activity, to the summit area of the volcano during major explosions, and extends almost to the entire island, and sometimes beyond, during the paroxysms (Barberi et al., 1993). We also considered several other factors, including the height of the plume, the amount of ash and scoria fallout, the occurrence and strength of any associated shock wave. The occurrence of PDC and/or tsunami associated to the violent explosive activity was assumed as a marker for a paroxysm too (Rosi et al., 2013). The determination of the hour and minute of the explosion in the historical documents usually distinguishes the most violent phenomena.
A digital version of the literature sources referenced is available from the corresponding author (A.B.). The modeling and estimation of inter-event time and temporal rate of major explosions and paroxysms at Stromboli volcano, basing on this catalog, is detailed in Bevilacqua et al., 2020.