Tanaga

Observations of Deformation

Volcano number:311080
Region:
Country:United States
Geodetic measurements?Yes
Deformation observation?Yes
Measurement method(s):InSAR
Duration of observation:2004 - 2009
Inferred cause(s) of deformation:Magmatic
Characteristics of deformation:

During October – November 2005, an episode of surface uplift (3 – 5 cm) occurred encompassing┬áboth Tanaga and Takawanga volcanoes. The broad region of uplift is modelled as a pressurising magma reservoir using a point source or a shallow-dipping prolate source that is elongate in the east-west direction. The source depth is inferred to be 5 – 8 km with a volume increase of 0.002 – 0.008 km┬│.

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
http://www.avo.alaska.edu/volcanoes/volcinfo.php?volcname=Tanaga
Location:51.885, -178.146
REST API endpoint (JSON):https://comet.nerc.ac.uk/wp-json/volcanodb/v1/volcano/1045

Latest Sentinel-1 Data

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