Journal article
Steady downslope movement on the western flank of Arenal volcano, Costa Rica
- Abstract:
-
The edifice of a volcano is a unique deformational environment, dependent not just on active volcanic processes but also on its composition, structure, and morphology. We measured the deformation of Volcn Arenal, Costa Rica, using interferograms constructed from both ALOS and RadarSat data between 2005 and 2009. The volcano's western flanks are moving downslope at an angle of ∼55° below the horizontal plane and a consistent rate of at least ∼7 cm/yr. We use the pattern, rate, and direction of...
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- Publication status:
- Published
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- Publisher copy:
- 10.1029/2010GC003263
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Bibliographic Details
- Journal:
- GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
- Volume:
- 11
- Issue:
- 12
- Pages:
- n/a-n/a
- Publication date:
- 2010-12-11
- DOI:
- EISSN:
-
1525-2027
- ISSN:
-
1525-2027
- Source identifiers:
-
110368
Item Description
- Language:
- English
- Keywords:
- Pubs id:
-
pubs:110368
- UUID:
-
uuid:67955348-70b4-49b4-bbcd-ae5be9387135
- Local pid:
- pubs:110368
- Deposit date:
- 2012-12-19
Terms of use
- Copyright date:
- 2010
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