The 1980 eruption of Mount St Helens was a VEI 5.
It has blowen in the past at VEI 5-6, so can expect the same in the furure
The eruption, which is still going on, is a VEI-0.
Mount St. Helens had a volcanic explosivity index (VEI) of 5 during its eruption on May 18, 1980. This VEI level indicates a significant explosive eruption that released a large amount of volcanic ash and caused widespread devastation in the surrounding area.
The 1951 eruption of Mount Lamington in Papua New Guinea was estimated to have a Volcanic Explosivity Index (VEI) of 4. The Richter Scale is not typically used to measure the size of volcanic eruptions; instead, the VEI is commonly used to classify and compare the explosiveness of volcanic eruptions.
bob
Ithink it was very violent
The 1980 eruption of Mount St Helens was a VEI 5.
It has blowen in the past at VEI 5-6, so can expect the same in the furure
The eruption, which is still going on, is a VEI-0.
No. "Category 5" is a rating on a system, used for hurricanes. Mount Pinatubo is a volcano. Volcanoes do not have a rating system but eruptions do: Volcanic Explosivity Index, which ranges from VEI 0 to VEI 8. On this scale the 1991 eruption of Mount Pinatubo was a VEI 6.
Geologist believe Mt. Fuji was formed approximatey 600,000 years ago during the Pleistocene era. The last recorded eruption was the Hōei eruption, which started on Decemeber16, 1707 and ended about January 1, 1708.
Mount St. Helens had a volcanic explosivity index (VEI) of 5 during its eruption on May 18, 1980. This VEI level indicates a significant explosive eruption that released a large amount of volcanic ash and caused widespread devastation in the surrounding area.
The 1951 eruption of Mount Lamington in Papua New Guinea was estimated to have a Volcanic Explosivity Index (VEI) of 4. The Richter Scale is not typically used to measure the size of volcanic eruptions; instead, the VEI is commonly used to classify and compare the explosiveness of volcanic eruptions.
The Volcanic Explosivity Index (VEI) of Mount Nyiragongo's eruption in 2011 is classified as a VEI 1 event. This indicates a relatively mild eruption characterized by effusive lava flows rather than explosive activity. The eruption primarily involved the outpouring of lava, with significant flows observed, but it did not produce significant ash plumes or explosive ejecta typical of higher VEI ratings. Overall, the 2011 event was notable for its lava lake activity rather than explosive eruptions.
De vei pleca was created in 2000.
Battle of Lang Vei happened in 1968.