Destroying the ancient cities of Pompeii and Herculaneum, the infamous volcano Mount Vesuvius still poses as a threat to Italian cities nearby. When this unpredictable volcano erupted in 79 CE, thousands were killed and many were left in the ash that captured the area. We know so much about this eruption because of an eyewitness named Pliny the Younger. He wrote letters after the eruption that told about the type of eruption and the destruction it caused, all from his view of the two day catastrophe many miles away (Ball, 2014).
Currently, this large volcano stands at 4,203 feet (Wikipedia, 2014), but it has not always been that way. The composite, otherwise known as stratovolcano, was constantly added to by the running over of lava from the cone, while rock and other pyroclastic debris were ejected as well. Initially formed by the subduction of the African under the Eurasian plate, the water from the oceanic African plate caused the melting point of the mantle to lower, creating the magma that led to the volcano (Wikipedia, 2014). Then, seventeen thousand years ago a caldera was formed from an explosion and then within it grew the cone of Mount Vesuvius (Wikipedia, 2014).
In 62 CE, there was an earthquake that is thought to be the start to the volcanic activity that caused the explosion of 79. It caused much damage around the Bay of Naples, and especially to Pompeii (Wikipedia, 2014). Researchers believe that the tectonic activity caused new activity in the volcano, with tremors becoming more frequent within days of the eruption (Wikipedia, 2014). The morning the most destructive eruption occurred, Pliny described it as “an umbrella pine, for it rose to a great height on a sort of trunk and then split off into branches…. Sometim...
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...han ten kilometers below the surface (Wikipedia, 2014). It is monitored by the multiple stations of the Osservatorio Vesuvio, who use many techniques to track the level of the magma. They measure ground movement and analyze the gases emitted from the volcano in order to do so (Wikipedia, 2014). Because Mount Vesuvius is not a danger in the near future, it was declared a national park. There is a network of paths around the mountain that leads to the summit, open to visitors (Wikipedia, 2014).
Works Cited
Ball, Jessica. “Mount Vesuvius – Italy.” Mount Vesuvius, Italy: Maps Facts, Eruption Pictures, Pompeii. Geology.com, 2014. Web. 7 May 2014.
"Mount Vesuvius." Wikipedia. Wikimedia Foundation, 6 May 2014. Web. 11 May 2014.
Owens, James. "Ancient Roman Life Preserved at Pompeii." Mysteries of the Ancient World. National Geographic, 16 Aug 2010. Web. 7 May 2014.
Sebastian Pether’s piece of work called The Eruption of Vesuvius (1835) combines the silver watery reflection of the moon with the hot red molten lava that is flowing down its mountainsides. Though during Pether’s generation he wasn’t the only one to paint the well-known Mount Vesuvius, Joseph Wright of Derby also painted 30 paintings of the volcano. This art piece is currently located at the Nelson-Atkins Museum of Art. The piece is oil media on panel that is framed with a beautifully designed border, where it is hanging on a wall in the one of the rooms, with a one-dimension view. The quality of the piece owes itself to the color and lighting, which captures your immediate attention and guides the viewer through the piece.
On the afternoon of 24th August 79 AD, a volcano called Mt. Vesuvius erupted, which resulted in destroyed lives of citizens, it was estimated that there were 10 to 12 thousand people who occupied the city .The cities of Pompeii, Herculaneum and a few others were severely affected by the eruption. The cities are well known for its beautiful landscapes and its temperate climate.Pompeii is based in the south, close to Naples in the region of Campania in Italy.The eruption started a series of events such as pumice,rocks and ashes falling down and caused hot volcanic gases to rise high in the sky, people from around 100 miles away could see the event unfolding.The remains of Pompeii and other cities was frozen in time due to the pyroclastic surges
There are several prominent geographical features that played a major role in the daily life of Pompeii. The geographical location of Pompeii, its economic and industrial activity, entertainment and the Roman influence in the city’s architecture all convey different geographical features. These features contributed in shaping the way the city’s inhabitants went about their daily lives, and all had a profound impact on Pompeii
On May 22, 1915, an explosive eruption at Lassen Peak devastated nearby areas and rained volcanic ash farther 200 miles to the east! This explosion was the most powerful in a series of eruptions from 1914 through 1917. ...
Nearly two millenniums ago a massive eruption rocked the Roman city of Pompeii, destroying buildings and coating the town in deep layers of volcanic ash. Fortunately, this same ash served as a tool for preservation and has allowed archaeologists to discover the remains of various types of Pompeii’s art. The values, beliefs, and daily workings of Roman culture have been brought to new light through the paintings, mosaics, statues and other forms of art found in the lost city of Pompeii.
First, one must know a little information about this volcano. Mount Shasta is located in Siskiyou County, California. This volcano is the second highest peak in the southern end of the Cascade Range and is still active, though not enough for people to notice. At 14,179 feet it is also the most voluminous stratovolcano located in the Cascade Volcanic Arc. The mountains complex shape is due to the four overlapping volcanic cones it consists of, including the most prominent, main summit, Shastina. The other cones include: Sargents Ridge cone, Misery Hill cone, and Hotlum cone. Sargents Ridge cone is the oldest of all the cones that make up the mountain. Though it is now dissected by a glacial valley, a portion of it can still be seen on the mountain. Misery Hill makes up a large part of the present mountain. the fourth cone, the Hotlum cone is formed from eruptive products and is located on the northeastern side of Mount Shasta. Three of the four major vents on the mountain are aligned with a north trending zone that passes through the mountains summit. This linear alignment parallels local faults, which suggests that the bedrock structure has influenced and partially controlled the dimensions in which Mount Shasta develops (Mie...
The eruption on Mount Saint Helens has a specific cause and comes with many effects. A multifold of people would say that the “mountain looked like the site of an atomic blast” (Bredeson 30). That is a very accurate depiction as it took great power to inflict as much damage as it did. The reason for this impressive amount of force is that when magma is built up with pressure and an earthquake hits, the pressure gets magnified and the volcano explodes (Lewis). This is exactly what happened inside Mount Saint Helens. Furthermore, it has been revealed that “The earthquake that triggered the explosion was a 5.2 on the Richter scale” (Gunn 559). The earthquake to the magma can be compared as a match to gasoline. Even though the earthquake was not huge, the scale of the eruption was much greater than that of the earthquake (Gunn 560). The earthquake was only the trigger that allowed for more devastating things to occur. Thirteen hundred feet of the volcano were lost in the explosion followed by landslides, mudslides, and lava flows...
57 people were killed, and 200 homes, 47 bridges, 15 miles (24 km) of railways and 185 miles (300 km) of highway were destroyed. The eruption blew the top of the mountain off, reducing its summit from 9,677 feet to 8,364 feet in elevation and replacing it with a mile-wide horeshoe-shaped crater. Like most of the other volcanoes in the Cascade Range, St. Helens is a great cone of rubble, consisting of lava rock interlayered with ash, pumice and other deposits. Volcanic cones of this internal structure are called composite cones or stratovolcanoes. Mount St. Helens includes layers of basalt and andesite through which several domes of dacite lava have erupted.
Stories about volcanoes are captivating. Myths come in different versions, but all of them are capable of capturing yours, and everybody’s imagination.
Super volcanoes are formed when magma rises from the mantle to create a scorching reservoir in the Earth's
while trying to help the residents of Pompeii. Today the type of eruption that Mount Vesuvius
Pompeii is possibly the best-documented catastrophe in Antiquity. Because of it, we know now how the Pompeians lived because they left behind an extensive legacy of art, including monuments, sculptures and paintings. Pompeii lay on a plateau of ancient lava near the Bay of Naples in western Italy in a region called Campania, less than 1.6 kilometers from the foot of Mount Vesuvius. With the coast to the west and the Apennine Mountains to the East, Campania is a fertile plain, traversed by two major rivers and rich soil. However, in the early days, it was not a remarkable city. Scholars have not been able to identify Pompeii’s original inhabitants. The first people to settle in this region were probably prehistoric hunters and fishers. By at least the eight century B.C., a group of Italic people known as the Oscans occupied the region; they most likely established Pompeii, although the exact date of its origin is unknown. “The root of the word Pompeii would appear to be the Oscan word for the number five, pompe, which suggests that either the community consisted of five hamlets or, perhaps, was settled by a family group (gens Pompeia)”(Kraus 7). In the course of the eight century B.C., Greek and Etruscan colonization stimulated the development of Pompeii as a city around the area of the Forum. A point for important trade routes, it became a place for trading towards the inland. Up until the middle of the 5th century B.C., the city was dominated politically by the Etruscans.
Firstly, I believe the eruption of Santorini was more powerful than first estimated, due to the presence of a shallow sea inside the Theran crater, with the volcano situated in the centre of that sea. (This is the theory of Professor Steve Sparks of Bristol University)
Mount Vesuvius is a volcano located in southern Italy, near the bay of Naples and the city of Naples. It is the only active volcano on the European mainland. Vesuvius rises to a height of 1277 m (4190 ft). Vesuvio (Vesuvius) is probably the most famous volcano on earth, and is one of the most dangerous.