Debris flow on Mt. Rainier: Why volcanoes are dangerous even when not erupting
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.
We talk a lot about the hazards that are present at Washington's Rainier mostly in terms of what might happen if the volcano erupts. However, remember that even when Rainier is showing no signs of activity, volcanic hazards can still be present (video). Case in point is the debris flow that occurred on Rainier last week. The Landslide Blog posted an excellent video of the June 25 event that seems to start as a debris avalanche/landslide but as the flow runs down the slopes of the volcano, some parts begin to appear lahar-like as meltwater from the snow, ice and glaciers on the volcano is incorporated into the flow itself. This footage is pretty spectacular as you can see the dust portion of the flow get left behind from the faster moving ground debris that runs out downslope. (And for those of you who might be curious, that initial part of the avalanche is as close to what a pyroclastic flow on Rainier might look like if you were near the summit).
A debris flow captured on video from Mt. Rainier, June 25, 2011.
Rainier has a long history of lahars (see map below), many of which are not related to volcanism - they are mostly glacially-derived meltwater releases that pick up debris along the way. This is why the volcano has a sophisticated lahar-warning system installed on the volcano as part of the hazard mitigation on the volcano because these types of lahars can occur with little-to-no warning. The lahar warning system utilizes sirens to warn the towns downvalley from Rainier that a lahar has been detected and to move to higher ground. Most of the town would have ~40 minutes (or more) to move people to safety (out of the river valleys) if a lahar is detected on the main edifice of Rainier. Usually flows like this are caused by heavy rains or melting, which prompts the collection and then release of water high on the slopes of the volcano. Rainier is also a very unstable volcano as much of the summit area has been extensively hydrothermally altered (pdf), so it is not surprising to see lahars and avalanches such as these on the volcano.
Lahar/mudflow inundation of the Rainier area over the last 5,600 years. Image courtesy of the USGS.
UPDATE 1:30 PM Eastern: Oh wow, here is a great look at the June 25 debris flow at Rainier.
Just a reminder that volcanoes are hazardous even if they haven't erupted in over a century.
Top left: Mt. Rainier in Washington.
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