Observations of Deformation
|Duration of observation:||1993 - 2000, 2004 - 2009|
|Inferred cause(s) of deformation:||Magmatic, Surface deposits|
|Characteristics of deformation:|
Interferograms covering the volcano show two regions of subsidence. The first is location on the southeastern flank of the volcano with deformation occuring at rates of ~0.5 cm/yr. This deformation is modelled by a point source at <1 km depth and is thought to originate from cooling and degassing of magma intruded during eruptions in 1987 and 1996. A second region of subsidence at rates of ~1 mm/yr is seen on the lower southwestern flank. This is in a region of lava flows thought to originate from the 1963 eruption, and subsidence is therefore attributed to thermoelastic constraction of lava flows.
|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/1015|