The mud volcanoes at Santa Barbara and Aragona (Sicily, Italy): a contribution to risk assessment
<p>The Santa Barbara and Aragona areas are affected by mud volcanism (MV) phenomena, consisting of continuous or intermittent emission of mud, water, and gases. This activity could be interrupted by paroxysmal events, with an eruptive column composed mainly of clay material, water, and gases....
Guardado en:
Autores principales: | , , , , , , |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Copernicus Publications
2021
|
Materias: | |
Acceso en línea: | https://doaj.org/article/4197602886d2444bbcd0d7ea5b9aca9e |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
id |
oai:doaj.org-article:4197602886d2444bbcd0d7ea5b9aca9e |
---|---|
record_format |
dspace |
spelling |
oai:doaj.org-article:4197602886d2444bbcd0d7ea5b9aca9e2021-11-10T06:52:31ZThe mud volcanoes at Santa Barbara and Aragona (Sicily, Italy): a contribution to risk assessment10.5194/nhess-21-3407-20211561-86331684-9981https://doaj.org/article/4197602886d2444bbcd0d7ea5b9aca9e2021-11-01T00:00:00Zhttps://nhess.copernicus.org/articles/21/3407/2021/nhess-21-3407-2021.pdfhttps://doaj.org/toc/1561-8633https://doaj.org/toc/1684-9981<p>The Santa Barbara and Aragona areas are affected by mud volcanism (MV) phenomena, consisting of continuous or intermittent emission of mud, water, and gases. This activity could be interrupted by paroxysmal events, with an eruptive column composed mainly of clay material, water, and gases. They are the most hazardous phenomena, and today it is impossible to define the potential parameters for modelling the phenomenon. In 2017, two digital surface models (DSMs) were performed by drone in both areas, thus allowing the mapping of the emission zones and the covered areas by the previous events.</p> <p>Detailed information about past paroxysms was obtained from historical sources, and, with the analysis of the 2017 DSMs, a preliminary hazard assessment was carried out for the first time at two sites. Two potentially hazardous paroxysm surfaces of 0.12 and 0.20 km<span class="inline-formula"><sup>2</sup></span> for Santa Barbara and Aragona respectively were defined. In May 2020, at Aragona, a new paroxysm covered a surface of 8721 m<span class="inline-formula"><sup>2</sup></span>. After this, a new detailed DSM was collected with the aim to make a comparison with the 2017 one. Since 2017, a seismic station was installed in Santa Barbara. From preliminary results, both seismic events and ambient noise showed a frequency of 5–10 Hz.</p>A. GattusoA. GattusoF. ItalianoG. CapassoA. D'AlessandroF. GrassaA. F. PisciottaD. RomanoD. RomanoD. RomanoCopernicus PublicationsarticleEnvironmental technology. Sanitary engineeringTD1-1066Geography. Anthropology. RecreationGEnvironmental sciencesGE1-350GeologyQE1-996.5ENNatural Hazards and Earth System Sciences, Vol 21, Pp 3407-3419 (2021) |
institution |
DOAJ |
collection |
DOAJ |
language |
EN |
topic |
Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 Geology QE1-996.5 |
spellingShingle |
Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 Geology QE1-996.5 A. Gattuso A. Gattuso F. Italiano G. Capasso A. D'Alessandro F. Grassa A. F. Pisciotta D. Romano D. Romano D. Romano The mud volcanoes at Santa Barbara and Aragona (Sicily, Italy): a contribution to risk assessment |
description |
<p>The Santa Barbara and Aragona areas are affected by mud volcanism (MV)
phenomena, consisting of continuous or intermittent emission of mud, water, and gases. This activity could be interrupted by paroxysmal events, with an eruptive column composed mainly of clay material, water, and gases. They are the most hazardous phenomena, and today it is impossible to define the potential parameters for modelling the phenomenon. In 2017, two digital surface models (DSMs) were performed by drone in both areas, thus allowing the mapping of the emission zones and the covered areas by the previous events.</p>
<p>Detailed information about past paroxysms was obtained from historical
sources, and, with the analysis of the 2017 DSMs, a preliminary hazard
assessment was carried out for the first time at two sites. Two potentially hazardous paroxysm surfaces of 0.12 and 0.20 km<span class="inline-formula"><sup>2</sup></span> for Santa Barbara and Aragona respectively were defined. In May 2020, at Aragona, a new paroxysm covered a surface of 8721 m<span class="inline-formula"><sup>2</sup></span>. After this, a new detailed DSM was collected with the aim to make a comparison with the 2017 one. Since 2017, a seismic station was installed in Santa Barbara. From preliminary results, both seismic events and ambient noise showed a frequency of 5–10 Hz.</p> |
format |
article |
author |
A. Gattuso A. Gattuso F. Italiano G. Capasso A. D'Alessandro F. Grassa A. F. Pisciotta D. Romano D. Romano D. Romano |
author_facet |
A. Gattuso A. Gattuso F. Italiano G. Capasso A. D'Alessandro F. Grassa A. F. Pisciotta D. Romano D. Romano D. Romano |
author_sort |
A. Gattuso |
title |
The mud volcanoes at Santa Barbara and Aragona (Sicily, Italy): a contribution to risk assessment |
title_short |
The mud volcanoes at Santa Barbara and Aragona (Sicily, Italy): a contribution to risk assessment |
title_full |
The mud volcanoes at Santa Barbara and Aragona (Sicily, Italy): a contribution to risk assessment |
title_fullStr |
The mud volcanoes at Santa Barbara and Aragona (Sicily, Italy): a contribution to risk assessment |
title_full_unstemmed |
The mud volcanoes at Santa Barbara and Aragona (Sicily, Italy): a contribution to risk assessment |
title_sort |
mud volcanoes at santa barbara and aragona (sicily, italy): a contribution to risk assessment |
publisher |
Copernicus Publications |
publishDate |
2021 |
url |
https://doaj.org/article/4197602886d2444bbcd0d7ea5b9aca9e |
work_keys_str_mv |
AT agattuso themudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT agattuso themudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT fitaliano themudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT gcapasso themudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT adalessandro themudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT fgrassa themudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT afpisciotta themudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT dromano themudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT dromano themudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT dromano themudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT agattuso mudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT agattuso mudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT fitaliano mudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT gcapasso mudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT adalessandro mudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT fgrassa mudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT afpisciotta mudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT dromano mudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT dromano mudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment AT dromano mudvolcanoesatsantabarbaraandaragonasicilyitalyacontributiontoriskassessment |
_version_ |
1718440462742716416 |