Assessing future vent opening locations at the Somma‐Vesuvio volcanic complex: 1. A new information geodatabase with uncertainty characterizations. Issue 6 (17th June 2017)

• Record Type: Journal Article
• Authors: Tadini, A.; Bisson, M.; Neri, A.; Cioni, R.; Bevilacqua, A.; Aspinall, W. P.
• Is Part Of: Journal of geophysical research. Volume 122:Issue 6(2017)
• Page Start: 4336
• Page End: 4356
• Publication Date: 2017-06-17
• Subjects: Somma‐Vesuvio -- geodatabase -- vent opening -- spatial uncertainty -- hazard assessment; Geomagnetism -- Periodicals; Geochemistry -- Periodicals; Geophysics -- Periodicals; Earth sciences -- Periodicals; 551.1
• DOI: 10.1002/2016JB013858
• Languages: English
• ISSNs: 2169-9313

Abstract

Abstract: This study presents new and revised data sets about the spatial distribution of past volcanic vents, eruptive fissures, and regional/local structures of the Somma‐Vesuvio volcanic system (Italy). The innovative features of the study are the identification and quantification of important sources of uncertainty affecting interpretations of the data sets. In this regard, the spatial uncertainty of each feature is modeled by an uncertainty area, i.e., a geometric element typically represented by a polygon drawn around points or lines. The new data sets have been assembled as an updatable geodatabase that integrates and complements existing databases for Somma‐Vesuvio. The data are organized into 4 data sets and stored as 11 feature classes (points and lines for feature locations and polygons for the associated uncertainty areas), totaling more than 1700 elements. More specifically, volcanic vent and eruptive fissure elements are subdivided into feature classes according to their associated eruptive styles: (i) Plinian and sub‐Plinian eruptions (i.e., large‐ or medium‐scale explosive activity); (ii) violent Strombolian and continuous ash emission eruptions (i.e., small‐scale explosive activity); and (iii) effusive eruptions (including eruptions from both parasitic vents and eruptive fissures). Regional and local structures (i.e., deep faults) are represented as linear feature classes. To support interpretation of the eruption data, additional data sets are provided for Somma‐Vesuvio geological units and caldera morphological features. In the companion paper, the data presented here, and the associated uncertainties, are used to develop a first vent opening probability map for the Somma‐Vesuvio caldera, with specific attention focused on large or medium explosive events. Key Points: A new geodatabase for Somma‐Vesuvio eruptions and structures is presented with >1700 elements stored in 14 feature classes grouped in five data sets Innovative characterizations of spatial uncertainty areas for each feature are introduced as key new geodatabase information elements The new database is used in a companion paper to develop the first spatial probability vent opening map for the Somma‐Vesuvio caldera