Observations of Deformation
|Duration of observation:||1997 - 2007|
|Inferred cause(s) of deformation:||Hydrothermal, Magmatic|
|Characteristics of deformation:|
Korovin is part of the Atka volcanic center and has been considered a satellite vent of Kliuchef. Kliuchef showed a small amount of localised subsidence during 1997–1998, 1998–1999, and 2004 – 2005. Uplift in this region was then observed during 1999 – 2000, 2003 – 2004 and again in June 2006 continuing until the time of the last InSAR observations.
|Reference(s):||Lu, Z., and Dzurisin, D., 2014, InSAR imaging of Aleutian volcanoes: Chichester, UK, Springer-Praxis, 390 p.|
|U.S. Geological Survey Alaska Volcano Observatory (AVO) website|
|REST API endpoint (JSON):||https://comet.nerc.ac.uk/wp-json/volcanodb/v1/volcano/1021|