42 for Loowit’s 42nd vol. 5: Cataclysm
It’s a beautiful, quiet morning with spectacular weather, and then suddenly it isn’t. An earthquake strikes, the bulge gives way, and the volcano blows up and out.
This actually isn’t a particularly large eruption. Between the lateral blast, Plinian ash column, and the pyroclastic flows, it totals only about 1.4 cubic kilometers of material. Barely a VEI of 5. But if you’re in it, it seems large enough to have swallowed the world. It is, indeed, cataclysmic.
Imagine watching from Portland, OR as over 1,000 feet of the summit vanish.
The blast is so fierce that it propels singed branches and pinecones all the way to Klickitat (Mount Adams), 34 miles away.
The winds generally blow east, so eastern Washington end up under massive ash clouds. The roiling, boiling, gray mass blots out the sun, and leaves towns buried under inches of fine, sharp gray rock.
Meanwhile, back at the volcano, phreatic explosions, caused by chunks of juvenile lava flash-heating the ice from dismembered glaciers and water from debris-choked lakes, turn the formerly verdant lands into a cratered moonscape.
The most destructive eruption in living memory in the lower 48 leaves 57 people dead and entire regions devastated. No one who lives through that day will ever forget. It seems every living thing has been stripped from the slopes, never to return.
But we’ll soon see that volcanoes are as much agents of creation as destruction, and life is surprisingly tenacious in the face of a cataclysm.
Featured image: Great eruption of Mt St Helens, 2 PM, May 18, 1980. Caption and image credit: NPS /
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