And that about wraps it up for Redoubt
I write the Eruptions blog on Big Think. I've been mesmerized with volcanoes (and geology) all my life. It helps that part of my family comes from the shadow of Nevado del Ruiz in Colombia, where I could see first hand the deadly effects of volcanic eruptions. Since then, I've taken a bit of a winding path to become a volcanologist. I started as a history major at Williams College, almost went into radio, but ended up migrating to geology, including an undergraduate thesis on Vinalhaven Island, Maine. I followed this up by changing coast to get my Ph.D. from Oregon State University. Then I ran a MC-ICP-MS lab at University of Washington for a spell (and wrote for an indie rock website). I spent three years as a postdoctoral scholar at University of California - Davis studying the inner workings of magmatic systems. I am now an assistant professor at Denison University and have projects in New Zealand, Chile and Oregon.
I am fascinated by volcanoes, their eruptions and how those eruptions interact with the people who live around the volcanoes. I started this blog after getting frustrated with the news reports of volcanic eruptions. Most of them get the information wrong and/or are just sensationalistic. I will try to summarize eruptions as they occur, translate some of the volcanic processes that are happening and comment on the reports themselves.
And no matter what people tell you, I definitely do not have a cat named Tephra. (OK, I do).
You can find out more about my research by visiting my website. If you have any comments, questions or information, feel free to contact me at eruptionsblog at gmail dot com.
Photo: The north flank of Mount Redoubt in early February 2009. Credit: Chris Waythomas / Alaska Volcano Observatory/U.S. Geological Survey
I've been following the waxing and waning of activity at Mt. Redoubt in Alaska for the past two months like many of you have. For a time there, the volcano had the nation's attention, both from the threat of a eruption near major shipping and oil hubs and from some questionable comments made by a certain Republican governor. However, nature sometimes doesn't play well with others, so after weeks of the Alaska Volcano Observatory's warnings that the volcano could erupt in "days to weeks", Redoubt seems to have returned to a state of calm. In fact, AVO reduced the alert level from Orange/Watch to Yellow/Advisory. They summarize the downgrade in the following statement released yesterday - part of an excellent summary of the current state of Redoubt, a history of the unrest and the potential future activity (a must read for anyone interested in Redoubt):
Over the past two weeks the overall level of seismic activity has
decreased, and the periods of sustained volcanic tremor, common during
late January and most of February, have been largely absent. Discrete
earthquakes are still occurring, but they are typically small and
their observed rate is similar to that detected prior to this period
of unrest. Volcanic gas emissions are still well above background
levels, and melting of the upper Drift glacier in the vicinity of the
1989-90 eruption vent is continuing. These conditions could persist
for many months and do not indicate that an eruption is imminent.
If we pick that apart, we can see a few things. The seismicity, which tend to be correlated with magma moving in the system, has ceased. However, volcano gas (carbon dioxide, sulfur dioxide, water amongst others) emissions are still elevated and melting continues near the 1989-90 dome. This means that the magma that intruded over the last few months - the magma that appears to have stopped moving - is still close enough to the vent to impart its heat and gases to rocks at that level. How close is that? The scientists at AVO think the magma is probably no shallower than 2 km, mostly likely as deep at 5 km, below the volcano. Why the magma stalled is anyone's guess, but this mass of magma rose for a time then stopped, and that is what drove the seismicity, degassing and melting we all saw since January. The consequence of this for future eruptions could be (1) nothing - most likely; (2) the slowed/stopped magma could "plug" the conduit, resulting in an increased in pressure of new magma that might produce a more explosive future eruption - less likely.
The thing that might be the most problematic with this period of unrest at Redoubt is what the fact that the volcano didn't erupt will mean to the public reaction that next time it starts to act up. AVO reputation is solid enough that I don't think the citizens of Alaska will not heed their future warnings (as has happened in other situations, such as at Nevado del Ruiz in Colombia), but there will be the chance that the media might make it a point that Redoubt did not erupt the last time it was "acting up."
This is the crux of the problem with mitigating disasters that we can't adequately predict just yet - how do you convince people that you know what you are doing. AVO did an excellent job in providing people with information and updates on the volcano, were very transparent in their evaluation and even so, Redoubt decided that it was going to throw us all for a loop (unlike Mt. Saint Helens in 2004). Does this mean that we volcanologists don't know what we're doing? Heck no. It is just that with a complex system like a volcano, we don't have nearly enough understanding of what triggers eruptions, what are definite signs of eruption and exactly when an eruption will occur. We may never reach that point, but to ever apply the "Boy who cried Wolf" analogy to volcanic monitoring is asking for a major disaster. AVO ends the update by warning that "It remains possible for conditions at the volcano to change rapidly, advancing from relatively low levels of unrest to eruption in time periods as short as 24 hours." We should take this to heart: as much as we don't like to admit it, nature still holds all the cards.
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