Mount St. Helens, a volcano in the Cascade Arc, erupted catastrophically on May 18, 1980 after months of rising activity and earthquake swarms. The eruption sent an ash plume 80,000 feet high, circling the globe within weeks and disrupting air travel. This episode of Stuff You Should Know explores the historical background of Mount St. Helens, the tragic events leading up to and during its 1980 eruption, and the devastating aftermath.
You'll learn about the warning signs from volcanologists, the massive lateral blast caused by an earthquake-triggered landslide, and the destruction wreaked in the surrounding area—from obliterated homes and infrastructure to the heartbreaking loss of life. The episode also touches on the mountain's continued activity and significance for ongoing volcanic research. Join Josh and Chuck for a dramatic yet sober retelling of this iconic eruption that reshaped the Pacific Northwest landscape.
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Mount St. Helens formed relatively quickly over 40,000 years as part of the Cascade Arc, created by tectonic plate subduction. The Puyallup people called it "Luet" after a volcanic fire tender woman, while Europeans named it after Baron St. Helens in 1792. Eruptions continued into the 19th-20th centuries.
In 1980, increased activity like quake storms raised concerns. Volcanologists David Johnston and Don Swanson urged evacuations despite local resistance from companies and residents. The governor eventually concurred.
On May 18, an earthquake caused the largest recorded landslide on Mount St. Helens' north side. This released pressure, causing a 24 megaton lateral blast of superheated steam and debris traveling up to 300 mph and devastation within 8 miles.
Mount St. Helens erupted in a massive Plinian eruption, sending an 80,000-foot ash plume that circled the globe in 15 days and disrupted air travel. The eruption cut the mountain's height by 1,300 feet.
Over 200 homes, 200 miles of roads/railways, and Spirit Lake were destroyed. The eruption claimed 57 lives, including geologist David Johnston, for whom Johnston Ridge is named.
Mount St. Helens remains active with new lava domes forming 2004-2008. Research continues on the mountain, providing insights into volcanic processes and ecosystem resilience.
1-Page Summary
The historical background of Mount St. Helens reveals a rich tapestry of geological events and indigenous folklore intertwined with European exploration.
The hosts highlight that geologically speaking, Mount St. Helens' formation occurred relatively quickly over about 40,000 years, becoming an active stratovolcano. The major eruption that happened around 4,000 years ago was so powerful that even now, 20 inches of tephra from the eruption can be found 62 miles away from the site.
Mount St. Helens is part of the Cascade Arc, formed when a younger tectonic plate was subducted under an older one. Rock and water heated up from this subduction, causing material to become less dense and rise toward the crust, which led to the formation of many cone-shaped mountains in the Pacific Northwest, including Mount St. Helens.
The indigenous Puyallup people named the mountain "Luet" after a volcanic fire tender woman. According to tribal legends, Mount St. Helens and surrounding mountains stem from a story where the creator God transformed them into mountains due to their quarrel over this woman. ...
Historical Context and Background of Mount St. Helens
The catastrophic 1980 eruption of Mount St. Helens was a significant geological event that provided valuable lessons about volcano monitoring, forecasting, and the sheer power of Earth's natural processes.
In the years leading up to 1980, Mount St. Helens exhibited clear warning signs of an eruption, drawing the attention of volcanologists and the local population. Research conducted by scientists, such as a 1975 paper predicting a likelihood of eruption within the century, pointed to the increasing possibility of volcanic activity. By March 20th, 1980, a 4.0 magnitude earthquake triggered a series of quake storms, fueling concerns about the volcano's impending activity.
Volcanologists including David Johnston and Don Swanson began advocating for evacuations, though they faced local resistance. Companies like Weyerhaeuser with logging contracts and residents such as Harry Truman, who ran a lodge on the mountain, were reluctant to leave. Despite the pressure to reopen the area, the governor of Washington eventually concurred with the scientists to maintain evacuations.
On March 27th, Mount St. Helens erupted, casting a 6,500-foot ash column into the sky and forming a significant crater approximately 1,600 feet wide at the summit. In the lead-up to the May eruption, signs like mudslides and growing craters continued. Around May 15th, some people, enticed by a period of reduced activity, returned to the area, increasing the potential number of victims when the eruption occurred.
An earthquake on May 18th resulted in the largest landslide in recorded history on Mount St. Helens' north side, causing over half a square mile of the mountain to disappear. The north flank, which had developed a massive bulge growing six feet per day, collapsed, releasing pent-up pressure and allowing superheated water beneath the mountain to flash into steam and expand rapidly.
Speakers Josh Clark and Chuck Bryant describe the event as a 24 megaton blast, 1600 times more potent than the Hiroshima atomic bomb, creating a hot, stone-laden cloud traveling at speeds of up to 300 miles per hour and temperatures reaching 660 deg ...
Events and Details of the 1980 Eruption
The eruption of Mount St. Helens left deep scars on the landscape and communities, with homes destroyed, lives lost, and the environment altered. Research continues to reveal insights into the resiliency of the ecosystem and the volcanic processes at work.
The violent 1980 eruption of Mount St. Helens wreaked havoc on the surrounding region. Over 200 homes and cabins, along with approximately 200 miles of road and railways, were obliterated. The eruption brought a cataclysmic change to the terrain, with Spirit Lake greatly altered.
Spirit Lake, once situated at the base of Mount St. Helens, was transformed into a larger and shallower body of water as its outlet was dammed by debris from the flood. To address flooding concerns and control the depth, a spillway tunnel was constructed five years later.
The eruption tragically claimed 57 lives. Among the victims was David Johnston, a geologist with the USGS who was monitoring Mount St. Helens. His efforts to advocate for the evacuation of the area saved thousands of lives. Johnston Ridge was named in his honor, remembering the place where he made his last radio transmission, "Vancouver, Vancouver, this is it."
Additionally, a ham radio operator named Jerry Martin, who was documenting the eruption, transmitted his observation of Johnston's camper being engulfed before experiencing the same fate. His last words, describing the camper covering up and the same fate approaching him, marked the extent of the immediate devastation north of the volcano.
The Impacts and Aftermath of the Eruption
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