Interaction of pyroclastic density currents with human settlements: Evidence from ancient Pompeii
2005; Geological Society of America; Volume: 33; Issue: 6 Linguagem: Inglês
10.1130/g21294.1
ISSN1943-2682
AutoresLucia Gurioli, M. T. Pareschi, Elena Zanella, Roberto Lanza, Enrico Deluca, Marina Bisson,
Tópico(s)Geophysical and Geoelectrical Methods
ResumoResearch Article| June 01, 2005 Interaction of pyroclastic density currents with human settlements: Evidence from ancient Pompeii Lucia Gurioli; Lucia Gurioli 1Istituto Nazionale di Geofisica e Vulcanologia, Via della Faggiola 32, 56126 Pisa, Italy Search for other works by this author on: GSW Google Scholar M. Teresa Pareschi; M. Teresa Pareschi 1Istituto Nazionale di Geofisica e Vulcanologia, Via della Faggiola 32, 56126 Pisa, Italy Search for other works by this author on: GSW Google Scholar Elena Zanella; Elena Zanella 2 Dipartimento di Scienze della Terra, Università di Torino, Via Valperga Caluso 35, 10125 Torino, Italy Search for other works by this author on: GSW Google Scholar Roberto Lanza; Roberto Lanza 2 Dipartimento di Scienze della Terra, Università di Torino, Via Valperga Caluso 35, 10125 Torino, Italy Search for other works by this author on: GSW Google Scholar Enrico Deluca; Enrico Deluca 2 Dipartimento di Scienze della Terra, Università di Torino, Via Valperga Caluso 35, 10125 Torino, Italy Search for other works by this author on: GSW Google Scholar Marina Bisson Marina Bisson 3Istituto Nazionale di Geofisica e Vulcanologia, Via della Faggiola 32, 56126 Pisa, Italy Search for other works by this author on: GSW Google Scholar Author and Article Information Lucia Gurioli 1Istituto Nazionale di Geofisica e Vulcanologia, Via della Faggiola 32, 56126 Pisa, Italy M. Teresa Pareschi 1Istituto Nazionale di Geofisica e Vulcanologia, Via della Faggiola 32, 56126 Pisa, Italy Elena Zanella 2 Dipartimento di Scienze della Terra, Università di Torino, Via Valperga Caluso 35, 10125 Torino, Italy Roberto Lanza 2 Dipartimento di Scienze della Terra, Università di Torino, Via Valperga Caluso 35, 10125 Torino, Italy Enrico Deluca 2 Dipartimento di Scienze della Terra, Università di Torino, Via Valperga Caluso 35, 10125 Torino, Italy Marina Bisson 3Istituto Nazionale di Geofisica e Vulcanologia, Via della Faggiola 32, 56126 Pisa, Italy Publisher: Geological Society of America Received: 26 Oct 2004 Revision Received: 28 Jan 2005 Accepted: 04 Feb 2005 First Online: 03 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 The Geological Society of America, Inc. Geology (2005) 33 (6): 441–444. https://doi.org/10.1130/G21294.1 Article history Received: 26 Oct 2004 Revision Received: 28 Jan 2005 Accepted: 04 Feb 2005 First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Lucia Gurioli, M. Teresa Pareschi, Elena Zanella, Roberto Lanza, Enrico Deluca, Marina Bisson; Interaction of pyroclastic density currents with human settlements: Evidence from ancient Pompeii. Geology 2005;; 33 (6): 441–444. doi: https://doi.org/10.1130/G21294.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Integrating field observations and rock-magnetic measurements, we report how a turbulent pyroclastic density current interacted with and moved through an urban area. The data are from the most energetic, turbulent pyroclastic density current of the A.D. 79 eruption of Vesuvius, Italy, which partially destroyed the Roman city of Pompeii. Our results show that the urban fabric was able to divide the lower portion of the current into several streams that followed the city walls and the intracity roads. Vortices, revealed by upstream particle orientations and decreases in deposit temperature, formed downflow of obstacles or inside cavities. Although these perturbations affected only the lower part of the current and were localized, they could represent, in certain cases, cooler zones within which chances of human survival are increased. Our integrated field data for pyroclastic density current temperature and flow direction, collected for the first time across an urban environment, enable verification of coupled thermodynamic numerical models and their hazard simulation abilities. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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