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British Geological Survey, Keyworth, Nottingham NG12 5GG, UK (e-mail: ldjon@bgs.ac.uk)
Received for publication 3 March 2006. Accepted for publication 4 August 2006.
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| Introduction |
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There can be few more hazardous situation than that of monitoring a volcanic andesite lava dome for signs of an impending collapse. Partial collapse of a lava dome generates hot, fast-moving pyroclastic density currents, which are categorized as pyroclastic surge or block-and-ash flow deposits based on sedimentary structures. Monitoring in such circumstances requires that measurements are taken from a distance that minimizes the threat from eruption and from asphyxiation by volcanic gases. The method also needs to be rapid to minimize the time spent by the monitoring team in the hazardous zone. The techniques described here are applicable to the monitoring of any unstable slopes and active landslide where hazardous conditions threaten the survey team.
| Survey location |
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