Item talk:Q273003
From geokb
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"name": "Lava flow morphology at an erupting andesitic stratovolcano: A satellite perspective on El Reventador, Ecuador",
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"abstract": "Lava flows\u00a0pose a significant hazard to infrastructure and property located close to volcanoes, and understanding how flows advance is necessary to manage volcanic hazard during eruptions. Compared to low-silica basaltic flows, flows of andesitic composition are infrequently erupted and so relatively few studies of their characteristics and behaviour exist. We use El Reventador, Ecuador as a target to investigate andesitic lava flow properties during a 4.5\u202fyear period of extrusive eruption between February 2012 and August 2016. We use satellite radar to map the dimensions of 43 lava flows and look at variations in their emplacement behaviour over time. We find that flows descended the north and south flanks of El Reventador, and were mostly emplaced over durations shorter than the satellite repeat interval of 24\u202fdays. Flows ranged in length from 0.3 to 1.7\u202fkm, and the length of flows generally decreased over the observation period. We measure a decrease in flow volume with time that is correlated with a long-term exponential decrease in effusion rate, and propose that this behaviour is caused by temporary\u00a0magma\u00a0storage in the conduit acting as magma\u00a0capacitor\u00a0between the\u00a0magma reservoir\u00a0and the surface. We use the dimensions of flow lev\u00e9es and widths to estimate the flow\u00a0yield strengths. We observe that some flows were diverted by topographic obstacles, and compare measurements of decreased channel width and increased flow thickness at the obstacles with observations from\u00a0laboratory experiments.\u00a0Radar observations, such as those presented here, could be used to map and measure properties of evolving lava flow fields at other remote or difficult to monitor volcanoes.",
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