Volcanic Hazards | Pyroclastic Flow, Pyroclastic Surge & Tephra
7:25
Study.com
Volcanic Hazards | Pyroclastic Flow, Pyroclastic Surge & Tephra
Learn about volcanic hazards and study pyroclastic flow, pyroclastic surge, and tephra. Explore the differences between these types of natural disasters.
117K viewsNov 23, 2013
Pyroclastic Flow Eruption
Pyroclastic flows may be even more destructive than previously thought | Science News
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8.4K views · 85 reactions | When a volcano erupts, pyroclastic flows are often the biggest danger to anyone nearby. These fast-flowing currents of rock, ash and hot gas are extremely difficult to study, so researchers created their own.  [Read the related Nature Geoscience paper here: https://go.nature.com/2Im1bYs] #GeologiaMag #Pyroclasticflow #Volcano #Eruption | Geologia Mag | Facebook
2:16
8.4K views · 85 reactions | When a volcano erupts, pyroclastic flows are often the biggest danger to anyone nearby. These fast-flowing currents of rock, ash and hot gas are extremely difficult to study, so researchers created their own.  [Read the related Nature Geoscience paper here: https://go.nature.com/2Im1bYs] #GeologiaMag #Pyroclasticflow #Volcano #Eruption | Geologia Mag | Facebook
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Pyroclastic flows from Unzen were generated by gravitational collapse of the growing lava dome, near the city of Shimabara, Nagasaki (1991). Most of the flows traveled from 1 to 3 km, but some flows reached more than 4 km, burning houses and killing people in the evacuated zone of Kita-kamikoba on the eastern foot of the volcano.The velocities of the flows ranged from 15 to 25 m/s on the gentle middle flank. Scientific paper: http://link.springer.com/article/10.1007/BF00301514#page-1 Other detai
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Pyroclastic flows from Unzen were generated by gravitational collapse of the growing lava dome, near the city of Shimabara, Nagasaki (1991). Most of the flows traveled from 1 to 3 km, but some flows reached more than 4 km, burning houses and killing people in the evacuated zone of Kita-kamikoba on the eastern foot of the volcano.The velocities of the flows ranged from 15 to 25 m/s on the gentle middle flank. Scientific paper: http://link.springer.com/article/10.1007/BF00301514#page-1 Other detai
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Pyroclastic flows from Unzen were generated by gravitational collapse of the growing lava dome, near the city of Shimabara, Nagasaki (1991). Most of the flows traveled from 1 to 3 km, but some flows reached more than 4 km, burning houses and killing people in the evacuated zone of Kita-kamikoba on the eastern foot of the volcano.The velocities of the flows ranged from 15 to 25 m/s on the gentle middle flank. Scientific paper: http://link.springer.com/article/10.1007/BF00301514#page-1 Other detai
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