Mount Etna Deformation
This animation depicts a time-series of ground deformation at Mount Etna Volcano between 1992 and 2001. The deformation results from changes in the volume of a shallow chamber centered approximately 5 km (3 miles) below sea level. The accumulation of magma in this chamber results in the inflation, or expansion, of the volcano, while the release of magma from the chamber results in deflation or contraction.
Radar data shows Mt Etna deforming.
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Credits
Please give credit for this item to:
ESA/NASA/JPL-Caltech
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Visualizer
- Vincent Realmuto (NASA/JPL CalTech)
Release date
This page was originally published on Thursday, October 17, 2013.
This page was last updated on Friday, August 2, 2024 at 3:44 PM EDT.
Related papers
Lundgren, P., and others (2004), Gravity and magma induced spreading of Mount Etna volcano revealed by satellite radar interferometry, Geophys. Res. Lett., 31, L04602, doi:10.1029/2003GL018736.
Lundgren, P., and others (2004), Gravity and magma induced spreading of Mount Etna volcano revealed by satellite radar interferometry, Geophys. Res. Lett., 31, L04602, doi:10.1029/2003GL018736.
Datasets used
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Differential Interferometry [ERS-1 and ERS-2: SAR]
ID: 720
Note: While we identify the data sets used on this page, we do not store any further details, nor the data sets themselves on our site.