A little bit of Yellowstone earthquake perspective
So why is the current earthquake swarm at Yellowstone not likely to lead to an eruption? Well, mostly because we've had so many other swarms that don't lead to eruption, and this one shows no signs of it being any different.
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.
Old Faithful geyser at Yellowstone National Park.
A few thoughts about faulting, earthquakes and eruptions:
The earthquakes at Yellowstone have been universally attributed to fault movement rather than magmatic activity by the USGS and the researchers at the University of Utah. This is likely based on the moment solutions for the earthquakes (i.e., the sense of motion on the earthquake - side to side, dilation, etc.) and the fact that there are no directly correlative volcanic/magmatic symptoms to go with them (such as pronounced, short-term bulging, excessive hydrothermal venting, etc.) Now, a lot of you are concerned that maybe we're all misreading this and the earthquakes are being seen as merely tectonic because magma is moving things around down there.
Well, it is a little bit of a chicken-and-egg scenario: do fault move because of magmatic activity or is magma movement facilitated by fault movement. There is likely a little of both can could happen - an earthquake can trigger an eruption if the system is posed at the brink of an eruption and conversely, as we know, magmatic movement can trigger earthquakes because the crust has to accommodate the new material (it has to "make room"). So, how can we be sure that this isn't happening at Yellowstone - and remember, for extreme conclusions (like an impending eruption) we need exceptional evidence. (And take note, I'm not seismologist or structural geologist, so feel free to point out where I might be off in these descriptions).
(1) The moment tensor/focal mechanism solutions for these earthquakes are dominantly strike-slip - i.e., the "beach ball" symbol suggests the movement is side-to-side motion with some extension on the fault - or a transtensional movement with both some extension and shear. This sort of movement can be accomplished without magma just from movement along faults due to extension. However, before you get too excited ...
(2) The earthquakes are in the middle of an area of historical seismic activity that don't produce volcano eruptions. The previous activity is the best sign for what is to come is what typically happens. So, the fact that most earthquakes in this area, at that depth with this solution are tectonic rather than magmatic, it would indicate that the current swarm is saying the same thing. It is sort of like watching a guy who only hits singles but hit a home run years ago come up to bat and expect him to hit a home run merely because he's at bat. The earthquakes are commonplace at Yellowstone - just a normal at bat for the caldera.
(3) If this were, by some chance, to be magmatically related, we would expect to see a progressive shallowing of the earthquakes as the magma moved upwards (if we're worried about an eruption). So far, I have not seen either in the current swam. Even the most recent earthquakes are still at ~9-11 km / 5.6-6.8 mile depth. If you're worried about an eruption, you'd need the earthquakes to start progressing upwards - without it, it could be lateral movement of magma, or just microfaults adjusting at depth.
(4) Finally, although we have accessory anecdotal evidence of changes in the hydrothermal/magmatic system (e.g., Old Faithful isn't so faithful, the long-lived bulging under Yellowstone Lake, etc.), these correlations do not automatically lead to causation. The caldera system is very complex, so much so that events on one side of the caldera can likely be wholly unrelated to one on the other. Just because we might see signs of change in the active systems roughly correlated with an earthquake swarm doesn't mean that they must be related. However, it is a good idea to continue look for changes that could end up pointing towards a magmatic causation ... with enough evidence.
So, that is my take on this swarm and why we don't need to be panicked or concerned that things are being misread. There are very clear signs that scientists look for when dealing with earthquakes and their sources, especially when magma is involved.
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