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Another example of migrating Yellowstone swarm activity occurred in 2008-2009 in northern Yellowstone Lake. This energetic swarm exhibited an extraordinarily high migration rate of ~1 km/day and is interpreted to be associated with magma injection along a pre-existing vertical fracture at a volumetric rate of up to 5 m3/s. This process produced a succession of migrating swarm fronts (Figure 3). Very few repeating earthquakes were identified, and the authors concluded that the sequence was initiated by volcanic pressurization that caused the generation of new fractures.
Two major swarm sequences at the western edge of the caldera are interpreted as magmatic fluid induced: the 1985 swarm, and the relatively recent 2010 swarm. Both contained numerous repeating earthquakes. Also in both cases, modeling of fluid injection on vertical volcanic dikes was used to show that expansion of the swarm fronts was a result of flow along pre-existing fractures of hot pressurized waters (hydrothermal fluid) for the 2010 swarm, and of magmatic fluids for the 1985 swarm.
Also in both cases, modeling of fluid injection on vertical volcanic dikes was used to show that expansion of the swarm fronts was a result of flow along pre-existing fractures of hot pressurized waters (hydrothermal fluid) for the 2010 swarm, and of magmatic fluids for the 1985 swarm.
Very few repeating earthquakes were identified, and the authors concluded that the sequence was initiated by volcanic pressurization that caused the generation of new fractures.