Seismic and Geodetic Investigation of the 1996-1998 Earthquake Swarm at Strandline Lake, Alaska
Microearthquake (< M3.0) swarms occur frequently in volcanic environments, but do not always culminate in an eruption. Such non-eruptive swarms may be caused by stresses induced by magma intrusion, hydrothermal fluid circulation, or regional tectonic processes, such as slow-slip earthquakes. Stra...
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| Format: | Others |
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Scholar Commons
2010
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| Online Access: | https://scholarcommons.usf.edu/etd/1681 https://scholarcommons.usf.edu/cgi/viewcontent.cgi?article=2680&context=etd |