Observations of Deformation
| Volcano number: | 311240 |
|---|---|
| Region: | Alaska |
| Country: | United States |
| Geodetic measurements? | Yes |
| Deformation observation? | Yes |
| Measurement method(s): | InSAR |
| Duration of observation: | 1992 - 2009 |
| Inferred cause(s) of deformation: | Surface deposits |
| Characteristics of deformation: | Subsidence of lava flows is observed at Cleveland. This includes lavas from the 2001 eruption on the western flank of the volcano that are subsiding at 2 – 4 cm/yr. |
| Reference(s): | Lu Z., Dzurisin, D., Wicks, C., Power, J., Kwoun, O., & Rykhus, R. (2007). Diverse deformation patterns of Aleutian volcanoes from satellite interferometric synthetic aperture radar (InSAR). In J. Eichelberger, E. Gordeev, P. Izbekov, M. Kasahara, & J. Lees (Eds.), Volcanism and subduction: The Kamchatka region (Vol. 172, pp. 249–261). American Geophysical Union, Geophysical Monograph. |
| 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=Cleveland | |
| Location: | 52.825, -169.944 |
| REST API endpoint (JSON): | https://comet.nerc.ac.uk/wp-json/volcanodb/v1/volcano/1000 |
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