Mount Vesuvius Facts
- This creation of geological processes remains best known by the english language name of Mount Vesuvius. In Italian, however, it holds the very similar name of Vesuvio. The only alternate names it holds are simply translations into other languages.
- Regardless of the title one chooses to use for it, though, it stands out from other, similar features around the world. It’s erupted, usually violently, many times in known history. Its destruction of Pompei still ranks as one of the greatest such disasters ever.
- Due to its eruptive nature, it’s considered one of the most dangerous volcanoes in the world. That’s partly becasue of that tendency, to be certain. That’s greatly augmented, however, by the fact that about 3 million people live close enough to be affected.
- Despite all these facts, however, Mount Vesuvius remains one of the most popular tourist attractions in its part of the world. That’s largely due to the presence of the ruins of Pompei, as mentioned previously. About 2.5 million visitors flock there yearly.
- Because of this popularity, regardless of potential dangers, the local government declared the site a National Park in 1995! The summit itself is now open to visitors. Park authorities maintain a network of paths around the area, in addition to a spiral walkway.
Mount Vesuvius Physical Description
The breathtaking Mount Vesuvius immediately captures the attention of all those who visit the volcanic site. It does so partly because of the knowledge of its history, to be certain. Yet it also impresses most visitors due to its sheer physical dimensions as well.
The mountain as it exists today is what’s known by experts as a humpbacked peak. This primarily consists of a large cone, circled by a steep rim. This rim’s part of the summit caldera of the volcano. Once much higher, an earlier eruption lowered this significantly.
The magnificent mountain also boasts some remarkable measurements. The cone itself currently has a height equaling 4,203 ft (1,281 m) above sea level. These additionally sit more than 1,300 ft (400 m) above the 3.1 mi (5 km) long valley, named Atrio di Cavallo, nearby.
The cone of Mount Vesuvius itself also shows an additional feature that distinguishes it. At roughly 1,968 ft (600 m) up its slope, a large, semi-circular ridge appears. Known as Mount Somma, itself, this girdles the cone on the northern side, and rises to 3,714 ft (1,132 m).
Between Mount Somma and the cone lies what’s named the Valle del Gigante. At the summit of the cone is a large crater measuring roughly 1,000 feet (305 m) deep. That structure is also about 2,000 ft (610 m) across. That formed during an eruption that occurred in 1944.
Mount Vesuvius Location, Formation, and History
The stunning volcanic formation known around the world as Mount Vesuvius formed in a part of the world known for its abundance of natural marvels. In fact, its precise location likely doesn’t surprise anyone. That’s true since it sits in a part of the continent of Europe.
There, this masterpiece of geological processes lies within the borders of what’s now the country of Italy. More exactly, though, its exact location places it in the Gulf of Naples. That puts it inside the region comprising the administrative region known as Campania.
The site represents a type of stratovolcano. It originated due to the collision of two tectonic plates, the Eurasian and the African. The African plate moved under the other, and its water-soaked sediments lowered the melting point of the upper mantle, which pushed up.
Given that magma remains less dense than the surrounding solid rock, pressure pushed it upward. As often happens in such situations, this eventually found a weak spot at the surface of the Earth. There, it broke through, thus forming the volcano in its original form.
Evidence indicates that Mount Vesuvius first formed during its initial eruption around 25,000 years ago. Between that time and around 3,800 years ago, it experienced numerous powerful events. Subsequent to that, it entered a long phase of numerous, yet smaller eruptions.
It’s best known, however, for its destructive eruption in AD 79. Miraculously, one recorded eyewitness account adds to the scientific evidence. The massive blast ejected ash and stone up to 21 mi (33 km) into the air. Pompei and Herculaneum were both utterly destroyed.
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