How to Trigger a Volcanic Eruption on Purpose
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Click to Open Overlay GalleryThe vast majority of fictional attempts to get a large explosive device into a volcano — something like a nuclear bomb — and the explosion from the bomb will cause the volcano to erupt. In most cases, the bomb needs to be delivered deep into the volcano (usually schematically shown as the “big vat of magma” that doesn’t exist) to get the plan to work. The idea is the explosion in the magma will cause it to continue to erupt. No one has ever tried this in reality (although we have bombed lava flows to no effect). I’ve also heard people say that merely drilling into a volcano could case an eruption by releasing the pressure building in the volcano, however, this sort of thing happens a lot without dire consequences (unless you own the drill rig). Interestingly, both of these ideas are also suggested when discussing how to stop a volcano from erupting — again, mostly by lowering the pressure in the volcano or blocking the magma from reaching the surface.
Why do volcanoes erupt in the first place?
Click to Open Overlay GalleryThe other way you can get a magma to erupt, usually explosively, is the addition of outside water. Think about the 2010 eruption of Eyjafjallajökull — that eruption was made much more explosive by all the melted snow/ice on the volcano that mixed with the magma (however, it was likely triggered by an injection of new, hot magma). If the right ratio of water-to-magma exists, then the explosive mixing of magma and water can be self-sustaining, meaning that the explosive eruption will continue propagating until the supply of water or magma runs out. However, too little water means that you likely don’t sustain the explosive mixing, too much water and you quench (solidify) too much of the magma.
What could trigger an eruption?
There are many theories of what can trigger a volcano to erupt. Some are as simple as the buoyancy of magma — it is less dense than the surrounding rock, so it rises until it intersects the surface. Likely, this is only the dominant process as volcanoes that produce lava flows like Kilauea. If you want an explosive volcanic eruption, you want to produce bubbles (and lots of them) by (1) decompressing the magma, causing gases to come out of solution; (2) crystallizing minerals to concentrate water/volatiles in the remaining magma or (3) heating the magma with a new intrusion. A release in pressure can be accomplished a number of ways, including the failure of the roof above the magma body (a volcanic landslide is a great way), the buoyant rise of the magma or through some less common factors like melting of a glacier (likely too slow a process to trigger a specific eruption), excessive precipitation to erode the volcano, changes in atmospheric pressure or maybe even Earth tides caused by the pull of the Sun and Moon (rare, mostly in already active volcanoes). Once you’ve produced bubbles, you need to concentrate them towards the top of the magma body, maybe through a earthquake — think about shaking an open bottle of soda with bubbles on the side: They all float to the top. However, in all these cases, you likely need a volcano that is “primed” to erupt — that is, one that has eruptible magma that just needs to be “tipped” into erupting.
What you’d need to potentially make it work — and why that likely wouldn’t work either.
Armed with this information, if you want to try to get a volcano to erupt, you’ll need to do a few things:
- Find a volcano that is already showing some signs of magma intruding at shallow depths. This might be high levels of volcanic gases, shallow earthquakes, deformation of the volcano. You want something “primed” to go.
- Figure out a way to release the lithostatic pressure keeping the “cork” on the volcano so that the bubbles can form.
- Figure out how to get a lot of water into the volcano quickly … but not too quickly.
How I’d try to do it.
Click to Open Overlay GalleryAnd now, the real problem
Now, you might be thinking “he’s got this whole thing figured out.” Thanks, I try. However, I don’t have it all figured out because there is one more problem I haven’t mentioned. That problem is time. Sure, I could do all these things but one thing that volcanologists don’t have a good grasp on is the timing — how long between the triggers of an eruption and the actual eruption. In some cases, it looks like seconds, like the earthquake and landslide at Mount St. Helens that triggered the 1980 eruption. In some cases, the trigger could take months or even a year as seems to be suggested by some volcanoes in Chile after large earthquakes. So, you might go through all the trouble only to have really no control on when the volcano will erupt — again, not the best plan if you’re planning to shock the world with evil genius. Heck, there is a pretty good chance that the volcano might not even erupt — so many variables go into this that even picking an ideal volcano that is ready to blow might not do it — and all your activity might impede an eruption rather than cause it. This all just shows how little we know about the exact mechanisms that can cause a specific volcano to erupt. So, as you draft your plans for world conquest, cross “hold the world hostage as I cause a volcano to erupt” from the list. You have a better chance at steering an asteroid into the planet than getting Yellowstone to explode at your whim.
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