Washington's 'forgotten giant' volcano stirs
gizmodo.com
gizmodo.com
I lived down range of Mount St. Helens when it had its major eruption in 1980. It was a regional disaster but the recovery was relatively quick and few people died despite the epic scale of it.
https://pubs.usgs.gov/publication/ofr98428
https://www.usgs.gov/media/images/mount-rainier-volcano-haza...
His "Ice Age Floods A to Z" series was must watch TV for me last winter.
You just described most modern news media.
Mt. St. Helens was a big deal in my childhood in Southern California, and I'm fairly certain that we were generously sprinkled with her ashes from 1,200mi away. It was not long afterward that yours truly earned the nickname "Mt. St. Helens" for my explosive temper and tendency to attack my bullies. Ah well!
Very little is happening around or under Mt. Adams. St. Helens is seeing actual noteworthy activity, and even that's still lower than magnitude 1 in almost every event, and those that get higher than 1 99.9999% of the time do not reach magnitude 2.
There isn't a huge amount to worry about from the volcanoes, unless a body of water intrudes into a magma chamber. Worry more about the Cascadia subduction zone letting a good one rip.
The Mt. Saint Helens eruption was precipitated by a landslide, which reduced pressure over the caldera, leading to a sideways-launched blowout of the volcano itself. That landslide might very well itself have been triggered by an earthquake.
Other possible mechanisms would be either the widening of a magma tube or fissure (permitting higher pressures to the surface), or the introduction of water (crustal or near subsurface) to a magma tube, with the ensuing steam explosion precipitating an eruption.
The role of water in vulcanism is something I'd not been aware of until relatively recently. The Ring of Fire volcanoes form largely around subduction faults, generally inland of where an oceanic plate subducts beneath a continental plate. The oceanic plate carries with it large volumes of seawater, and as that plate itself intersects with (and is absorbed into) the mantle, that incorporated water flashes to steam. The steam pressure itself then plays a major function in generating pressures and driving magma toward the surface. This is also why volcanic eruptions tend to have so much steam as part of the emergent material, so far as I understand.
Another recent eruption in which water (in this case seawater) played a huge role was the 2022 Hunga Tonga–Hunga Haʻapai event, occurring as seawater flooded into a large, shallow caldera, flashing to steam with explosive consequence. Whether or not that event was preciptated by an earthquake again isn't clear, but could be possible. Other mechanisms might have been a cascading failure of the overlying roof of the caldera, with smaller introductions of water expanding access and leading to the catastrophic failure and explosion.
There's some scientific research into the question:
"A review framework of how earthquakes trigger volcanic eruptions" (2021)
<https://www.nature.com/articles/s41467-021-21166-8>
"Can earthquakes trigger volcano eruptions? Here's the science." (2019)
<https://www.nationalgeographic.com/science/article/can-earth...>
Though the raw amounts of water in subducted seafloor are apparently immense. Something which really hadn't occurred to me until recently.
And another [https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/200...]