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Why might part of an eruption column collapse to form a pyroclastic flow?
A collapse can occur if the eruption column becomes too dense, leading to instability. This density can be caused by the accumulation of dense volcanic materials like ash and pumice. When the column collapses, it can create a fast-moving pyroclastic flow that travels downslope, posing a significant hazard to surrounding areas.
What eruption of pyroclastic material was the most devastating?
That would be a matter of opinion, but a reasonable choice might be the eruption of Vesuvius that destroyed and buried Pompei in 76 CE.
How might an erupting volcano damage living things?
If it is an effusive eruption, the lava can burn living organisms. In an explosive eruption pyroclastic flows can sweep away, bury and/or burn living organisms. Ash can poison the soil and cause animals to suffocate. Plants and animals alike may be exposed to toxic gasses.
How many people died from heimaey eruption?
The Heimaey eruption might have caused problems, but no one died.
Why stadium don't collapse?
The reasons stadiums doesn't just collapse is because there are pillars to hold it. It might collapse when someone bombs or break the pillars.
What will happen if your respiratory center malfunctioned?
Your lungs might collapse
What effect might a volcanic eruption have on a climate or weather?
Polution maybe?
What kinds of unusual activity might be noticed before a volcanic eruption?
no there were not
What might the value be of a collapse stretcher from the Vietnam war?
see ebay
What are the five instances when balanced columns might be a good format to use for a document?
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What might happen if a major volcanic eruption every year?
Global temperatures might cool by several degrees
What are two ways which volcanic mountains might get smaller?
Volcanic mountains can get smaller through erosion, where wind, water, and ice gradually wear down the volcano's surface over time. They can also decrease in size through volcanic collapse, where the eruption of magma causes the structure of the volcano to weaken and collapse inward.
