Vesuvius’ eruptions are classified as Plinian eruptions, each eruption has a chance to change Mt. Vesuvius’ geography. The cone of Mt. Vesuvius in 1980 is 4,198 feet (1,280 Meters) long, which is sort of large. Vesuvius has a ridge called Mount Somma, which is 1,968 feet long. The valley in between the one of the cones and Mount Somma is the Valle del Gigante. In Mt. Vesuvius’ glory, it is still active and very dangerous. Although Mt. Vesuvius is destructive, lots of the surrounding area is densely populated because of the rich soil from the pumice and ash. This makes Vesuvius popular, and to add onto that, Mt. Vesuvius’ is spectacular to look …show more content…
The Plinian eruption is the most dangerous one, shown by Vesuvius on that faithful day it buried Pompeii. They both can cause extreme, explosive outbursts. Glowing avalanches can be seen from these types of eruptions. Lots of gas, lava, and volcanic fragments are sometimes blown out of volcanoes. Lots of times the summit/core could be damaged or broken entirely because of the intensity of the Pelean and Plinian eruptions. The Pelean eruption generates pyroclastic flows, but the Plinian does not. Plinian eruptions can continuously generate magma for hours on end, though. The Plinian eruption can change global warming for decades or even