Abstract

Abstract. Hazard mapping in poorly known volcanic areas is complex since much evidence of volcanic and non-volcanic hazards is often hidden by vegetation and alteration. In this paper, we propose a semi-quantitative method based on hazard event tree and multi-hazard map constructions developed in the frame of the FP7 MIAVITA project. We applied this method to the Kanlaon volcano (Philippines), which is characterized by poor geologic and historical records. We combine updated geological (long-term) and historical (short-term) data, building an event tree for the main types of hazardous events at Kanlaon and their potential frequencies. We then propose an updated multi-hazard map for Kanlaon, which may serve as a working base map in the case of future unrest. The obtained results extend the information already contained in previous volcanic hazard maps of Kanlaon, highlighting (i) an extensive, potentially active ~5 km long summit area striking north–south, (ii) new morphological features on the eastern flank of the volcano, prone to receiving volcanic products expanding from the summit, and (iii) important riverbeds that may potentially accumulate devastating mudflows. This preliminary study constitutes a basis that may help local civil defence authorities in making more informed land use planning decisions and in anticipating future risk/hazards at Kanlaon. This multi-hazard mapping method may also be applied to other poorly known active volcanoes.

Highlights

  • Basis that may help local civil defence authorities in making more informed land use planning decisions and in anticipating future risk/hazards at Kanlaon

  • The goal of this paper is to provide an applicable hazard mapping method in volcanic areas characterized by a minimum level of geological data and historical records

  • To improve our geologic knowledge of Kanlaon, we studied the volcanic succession through field observations, remote sensing data with a 15 m resolution LANDSAT 7 image (2003), and a 2.5 m resolution stereo pair from the Panchromatic Remote-sensing Instrument for Stereo Mapping (PRISM) on board the Japanese satellite ALOS (Advanced Land Observing Satellite, 2009)

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Summary

Introduction

Basis that may help local civil defence authorities in making more informed land use planning decisions and in anticipating future risk/hazards at Kanlaon. This multi-hazard are commonly used in thHeyfideldroolforigskyasasenssdment (e.g. Vecchia, 2001; Douglas, 2007; Neri et al, 2008; Marzocchi et al., 2009; Crisci et al, 2010;EVaicratrihetSaly.,s2t0e11m) and elsewhere mapping method may be applied to other poorly known (IPCC, 2012). Each type of phenomenon is characterized by one or more intrinsic physical effects expressed through physical units. Physical intensity Scale defined from physical values that express scale the magnitude class of a physical effect (Table 2). Cinematic impact expressed in J, pressure or loading in Pa, thickness in m, peak ground acceleration in ms−2, etc

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