Quantitative volcanic susceptibility analysis of Lanzarote and Chinijo Islands based on kernel density estimation via a linear diffusion process.
Risk management stakeholders in high-populated volcanic islands should be provided with the latest high-quality volcanic information. We present here the first volcanic susceptibility map of Lanzarote and Chinijo Islands and their submarine flanks based on updated chronostratigraphical and volcano structural data, as well as on the geomorphological analysis of the bathymetric data of the submarine flanks. The role of the structural elements in the volcanic susceptibility analysis has been reviewed: vents have been considered since they indicate where previous eruptions took place; eruptive fissures provide information about the stress field as they are the superficial expression of the dyke conduit; eroded dykes have been discarded since they are single non-feeder dykes intruded in deep parts of Miocene-Pliocene volcanic edifices; main faults have been taken into account only in those cases where they could modified the superficial movement of magma. The application of kernel density estimation via a linear diffusion process for the volcanic susceptibility assessment has been applied successfully to Lanzarote and could be applied to other fissure volcanic fields worldwide since the results provide information about the probable area where an eruption could take place but also about the main direction of the probable volcanic fissures.
Spanish Geological Survey, Unit of Canary Islands, Alonso Alvarado, 43, 2°A, 35003, Las Palmas de Gran Canaria, Spain.
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Galindo
University of La Laguna, Department of Geography, 38207, La Laguna. Tenerife, Spain.
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Romero
Spanish Geological Survey, Unit of Canary Islands, Alonso Alvarado, 43, 2°A, 35003, Las Palmas de Gran Canaria, Spain.
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Sánchez
University of Las Palmas de Gran Canaria, Faculty of Teacher Training, Special Didactics Department, 35004, Las Palmas de Gran Canaria, Spain.
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Morales