The early eruptive stages of Mount St. Helens are known as the "Ape Canyon Stage" (around 40-35,000 years ago), the "Cougar Stage" (ca. 20-18,000 years ago), and the "Swift Creek Stage" (roughly 13-8,000 years ago).
A dormancy of about 4,000 years was broken around 2500 BCE with the start of the Smith Creek eruptive period, when eruptions of large amounts of ash and yellowish-brown pumice covered thousands of square miles. An eruption in 1900 BCE was the largest known eruption from St. Helens during the Holocene epoch, judged by the volume of one of the tephra layers from that period. This eruptive period lasted until about 1600 BCE and left 18 inches (46 cm) deep deposits of material 50 miles (80 km) distant.
The next eruptive period, the Castle Creek period, began about 400 BCE, and is characterized by a change in composition of St. Helens' lava, with the addition of olivine and basalt. Another 400 years of dormancy ensued.
The Sugar Bowl eruptive period was short and markedly different from other periods in Mount St. Helens history. It produced the only unequivocal laterally directed blast known from Mount St. Helens before the 1980 eruptions.
Roughly 700 years of dormancy were broken in about 1480, when large amounts of pale gray dacite pumice and ash started to erupt, beginning the Kalama period. The eruption in 1480 was several times larger than the May 18, 1980, eruption. In 1482, another large eruption rivaling the 1980 eruption in volume is known to have occurred. St. Helens reached its greatest height and achieved its highly symmetrical form by the time the Kalama eruptive cycle ended, about 1647. A 57-year eruptive period started in 1800. There were at least a dozen reported small eruptions of ash from 1831 to 1857, including a fairly large one in 1842.
Mount St. Helens is most notorious for its catastrophic eruption on May 18, 1980, at 8:32 am PDT.
Mount Bromo last erupted in 2016, with its most recent minor eruption occurring in January of that year.
Mount Teide erupted in 1706 due to the accumulation of pressure from the movement of magma beneath the surface. This pressure eventually led to a volcanic eruption, releasing lava, ash, and gases into the surrounding area.
Mount Pinatubo is an active volcano, and there is always a possibility for future eruptions. However, it is difficult to predict when or if it will erupt again. Monitoring and research efforts are in place to assess the volcano's activity and provide early warnings if an eruption is imminent.
Mount Shasta's last known eruption occurred around 1786, based on historical records and studying the geology of the area. The volcano is currently considered to be dormant, with no signs of imminent eruption.
Mount Nyiragongo erupted on the 21 January 2002 in the Democratic republic of Congo.
an earthquake that was under it
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Mount Saint Helens is located in Gifford Pinchot National Forest, Washington 98616.
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Mount St. Helens erupted on May 18, 1980. It was a catastrophic eruption that resulted in the loss of lives and significant destruction of the surrounding area.
The eruption of Mount St. Helens in 1980 was relatively short, lasting for about nine hours. However, the effects of the eruption, including the eruption column and pyroclastic flows, had long-lasting impacts on the surrounding area.
Mount St. Hellens i think...
No, Mount Everest will not erupt because it is not a volcano.
Mount Everest does not erupt as it is not a volcano.
An extinct volcano has not had an eruption for at least 10,000 years and is not expected to erupt again in a comparable time scale of the future
Mount Erebus did not erupt in 2011. The last known eruption of Mount Erebus in Antarctica occurred in 2018.