Unrest and eruptions
Monogenetic cones at Mauna Kea (Hawaii, USA). Photo by Helena Albert. Credit: Geology and Helena Albert. |
Albert and colleagues show that seismic crises occur about a year, two to three months, and a few weeks before eruption, and that these correspond to magmatic intrusions and mixing at mid-crustal depths, followed by magma transport to the surface. They propose a general model for these eruptions in which early dike intrusions in the crust do not erupt (e.g., stalled intrusions) and make small plumbing systems, but they probably are key in creating a thermal and rheological pathway for later dikes to be able to reach the surface.
These observations provide a conceptual framework for better anticipating monogenetic eruptions in similar settings and magmatic fluxes and should lead to improved strategies for mitigation of their associated hazards and risks.
Reference:
Years to weeks of seismic unrest and magmatic intrusions precede monogenetic eruptions
Helena Albert et al., Central Geophysical Observatory, Spanish Geographic Institute (IGN), 28014, Madrid, Spain. DOI: 10.1130/G37239.1
Note: The above post is reprinted from materials provided by Geological Society of America.
http://www.geologypage.com/2016/02/unrest-and-eruptions.html
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