Physics
Scientific paper
May 2003
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30i..36m&link_type=abstract
Geophysical Research Letters, Volume 30, Issue 9, pp. 36-1, CiteID 1483, DOI 10.1029/2002GL016773
Physics
7
Seismology: Volcano Seismology (8419), Volcanology: Eruption Monitoring (7280), Information Related To Geographic Region: South America
Scientific paper
Significant seismic activity is generally recorded on volcanoes covered by an icecap. This work was carried out in order to quantify the role of the glaciers in the generation of seismicity for Cotopaxi volcano. We compared the seismic activity registered on the glacier and on the rock near the snout of the north flank glacier. We focused on the analysis of low frequency events (<5 Hz) similar to volcanic LP events when recorded on rock base. The particle motion analysis helps to estimate source locations, which are distributed in crevasses areas. High incident angles suggest a superficial origin. These events are interpreted as icequakes for which we propose as source mechanism a fluid-driven crack model triggered by ice cracking or hydraulic transients. The low quality factor values estimated are consistent with the resonance of an ice crack filled with water. This work shows that low frequency icequakes can be confusingly taken as volcanic LP events.
Araujo Sebastián
Lesage Philippe
Métaxian Jean-Philippe
Mora Mauricio
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