Novarupta
Novarupta is a volcano located on the Alaska Peninsula on a slope of Trident Volcano in Katmai [National Park and Preserve], about southwest of Anchorage. Novarupta was formed in 1912, during the largest volcanic eruption of the 20th century, in which it released 30 times the volume of magma of the 1980 eruption of Mount St. Helens.
Eruption of 1912
The 1912 eruption that formed Novarupta was the largest to occur during the 20th century. It began on June 6, 1912, and culminated in a series of violent eruptions. Rated a 6 on the volcanic explosivity index, the 60-hour-long eruption expelled of ash, thirty times as much as the 1980 eruption of Mount St. Helens. The erupted magma of rhyolite, dacite, and andesite resulted in more than of air fall tuff and approximately of pyroclastic ash-flow tuff. During the 20th century, only the 1991 eruption of Mount Pinatubo in the Philippines and the 1902 eruption of Santa María in Guatemala were of comparable magnitude; Mount Pinatubo ejected of tephra, and Santa María just slightly less.The Novarupta eruption occurred about from the peak of Mount Katmai Volcano and below the post-eruption Mount Katmai summit. During the eruption a large quantity of magma erupted from beneath the Mount Katmai area, resulting in the formation of a wide, funnel-shaped vent and the collapse of Mount Katmai's summit, creating a deep, caldera.
The eruption ended with the extrusion of a lava dome of rhyolite that plugged the vent. The high and wide dome it created forms what is now referred to as Novarupta.
Despite the magnitude of the eruption, no deaths directly resulted. Eyewitness accounts from people located downwind in the path of a thick ash cloud described the gradual lowering of visibility to next to nothing. Ash threatened to contaminate drinking water and destroyed food resources, but the Alaska Natives were aided in their survival by traditional knowledge passed down through generations from previous eruptions. However, the Native villages experiencing the heaviest ash falls were abandoned and the inhabitants relocated.
Valley of Ten Thousand Smokes
Pyroclastic flows from the eruption formed the Valley of [Ten Thousand Smokes], named by botanist Robert F. Griggs, who explored the volcano's aftermath for the National Geographic Society in 1916.The eruption that formed the Valley of Ten Thousand Smokes is one of the few in recorded history to have produced welded tuff, resulting in numerous fumaroles that persisted for 15 years.