Item talk:Q234429
From geokb
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"abstract": "The 2004\u20132008 dome-building eruption at Mount St. Helens ended during winter 2007\u20132008 at a time when field observations were hampered by persistent bad weather. As a result, recognizing the end of the eruption was challenging\u2014but important for scientists trying to understand how and why long-lived eruptions end and for public officials and land managers responsible for hazards mitigation and access restrictions. In hindsight, the end of the eruption was presaged by a slight increase in seismicity in December 2007 that culminated on January 12\u201313, 2008, with a burst of more than 500 events, most of which occurred in association with several tremor-like signals and a spasmodic burst of long-period earthquakes. At about the same time, a series of regular, localized, small-amplitude tilt events\u2014thousands of which had been recorded during earlier phases of the eruption\u2014came to an end. Thereafter, seismicity declined to 10\u201320 events per day until January 27\u201328, when a spasmodic burst of about 50 volcano-tectonic earthquakes occurred over a span of 3\u00a0h. This was followed by a brief return of repetitive \u201cdrumbeat\u201d earthquakes that characterized much of the eruption. By January 31, however, seismicity had declined to 1\u20132 earthquakes per day, a rate similar to pre-eruption levels. We attribute the tilt and seismic observations to convulsive stagnation of a semisolid magma plug in the upper part of the conduit. The upward movement of the plug ceased when the excess driving pressure, which had gradually decreased throughout the eruption as a result of reservoir deflation and increasing overburden from the growing dome, was overcome by increasing friction as a result of cooling and crystallization of the plug.",
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