Item talk:Q260782
From geokb
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"name": "Volcanic unrest at Nevados de Chill\u00e1n (Southern Andean Volcanic Zone) from January 2019 to November 2020, imaged by DInSAR",
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"abstract": "The volcanic complex of Nevados de Chill\u00e1n, located in the Southern Volcanic Zone (SVZ) of the Andes, has been active for the past 640\u00a0\u00b1\u00a020\u00a0ka. Its volcanic activity includes dome forming eruptions, explosive events, and\u00a0lava flows. The most recent eruption cycle started in January 2016. We employ DInSAR time-series from Sentinel-1 data to investigate the unrest episode from January 2019 to November 2020. Two distinct periods of unrest are recognized in the time series. The first period (from January to October 2019) coincides with explosive events, dome growth inside the active\u00a0crater, and a decrease in seismic activity but does not present a significant deformation. The second period (October 2019 to November 2020) is characterized by a displacement towards the sensor's line-of-sight of 100\u2013120\u00a0mm. The observed surface deformation is compatible with an inflation source approximately 1.5\u00a0km south-southwest of the present active vent, at 5.5\u00a0\u00b1\u00a00.5\u00a0km depth from the surface, and with a volume change of 0.044\u00a0\u00b1\u00a00.014\u00a0km3. The most likely explanation for the observed inflation of Nevados de Chillan is the intrusion of\u00a0magma\u00a0in a reservoir feeding the current eruption cycle.",
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