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Eruption of mount vesuvius at Pompeii essay
Eruption of mount vesuvius at Pompeii essay
Mt. vesuvius eruption in 79 a.d
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It was noon when the peak of Vesuvius erupted, the eruption propelled a 20 mile high Colum into the stratosphere at twice the speed of sound. For the next 12 hours heavy showers of ash fell out of the cloud and onto Pompeii and eventually buried the streets under six feet of rouble. However this did not kill the people.
At first Herculaneum was protected by a westerly wind, but as the energy of the blast waned and the Colum of material could no longer be supported above the volcano it collapsed and a giant surge cloud of hot ash swept down the western flank and scorched and suffocated the people of Herculaneum. This was the first flow. In Pompeii people had survive the rock falls and were roaming the streets on top of the rubble blanket. The
surge clouds that had reached Herculaneum had no reached this far. Then in the morning another flow surged through Pompeii and burnt and suffocated everyone who remained there.
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
Geographical features played a prominent role in the daily life of Pompeii. A geographical feature is a natural or manmade feature of an environment. For the city of Pompeii, the location was a key aspect of its daily life. In addition, the economic activity and industry was important in the everyday life of Pompeii’s citizens. Evidence also suggests entertainment played a large role in the life of the city’s population. Archaeological remains also stress the Roman influence of its streets and buildings. All these features contributed to the daily life in Pompeii.
The private and public leisure activities of Pompeii and Herculaneum were largely abundant. Many activities could be participated in and were used often. These include Drama performances, gladiatorial games, drinking, gambling, brothels, exercise, gardens, baths and food and dining. All these were an important part of Pompeian and Herculaneum life. They were seen as important to keep the body and mind healthy in most cases. Though some opposed some of the activities like brothels, gambling and drinking. But all give a important look into the life of those in Pompeii and Herculaneum before the catastrophic eruption of Vesuvius which completely destroyed both towns and all its inhabitants.
Helens tallied up to be the most deadly and destructive eruption the United States had ever seen. “Approximately fifty-seven people were killed directly from the blast and 200 houses, 47 bridges, 15 miles (24 km) of railways and 185 miles (298 km) of highway were destroyed; two people were killed indirectly in accidents that resulted from poor visibility, and two more suffered fatal heart attacks from shoveling ash (Wikipedia 3)”. Just when it seemed the nightmare was over a second eruption occurred the following day. A quarter of the lava was fresh, and included ash, pumice, and volcanic bombs, and the rest was older molten rock. “The removal of the north side of the mountain (13% of the cone 's volume) reduced Mount St. Helens ' height by about 1,280 feet (390 m) and left a crater 1 to 2 miles (2 to 3 km) wide and 2,100 feet (640 m) deep with its north end open in a huge breach (Wikipedia 3)”. The downwind of the eruption also destroyed many agricultural crops such as wheat, apples, potatoes, and alfalfa. Overall Mount St. Helens was a major blow that cost the US 1.1 billion dollars, and struck fear into the hearts of all of America on May 18th,
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. ...
In March 18, 1880 Mount St. Helens there was a catastrophic eruption that caused a huge volume of ash; the ash plume would be over central Colorado within 16 hours. After years of dedicated monitoring (knowing where to volcano is, unlike an earthquake not knowing exactly where this geological even is exactly) there was been increasing accuracy in forecasting eruptions.
covers the area, causing people, animals, and structures to practically disintegrate. Even years afterwards people were still dying and having
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...
Mount Vesuvius is located in the Bay of Naples in Southern Italy. Its Latitude and Longitude is 40.8224° N, 14.4289° E. It is a stratovolcano and has a height of 1277 meters (1490 feet) and base of 48 kilometers (30 miles). Mount Vesuvius has erupted over 30 times and has a repose time that can last for months or even years between eruptions. Its eruptions are explosive and is dominated by pyroclastic flows. The eruption materials are usually an ash cloud with lightening that spews out dense ash falls. The lava can shoot up to 4km into the air. The most famous eruptions of Mt. Vesuvius were in 79 A.D. which destroyed the cities of Herculaneum and Pompeii. The cities were covered in 20 feet of volcanic debris. The estimated death toll was over 1000 people. The
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.
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.
Within a thousand kilometres falling ash, lava flows and the utter explosive force of the eruption would kill practically all life. Volcanic ash would cover places as far away as Iowa and the
Across cultures, continents, and worlds, the majority of things within the scope of our very own humanity can be boiled down to two things: those who are dominant, and those who get dominated. Within these statuses lie stories of power struggles, rebellion, the rising and falling of those with influence, and the interconnection between a being with power and the people under his ruling. Through the visual works catered to this subject, we will discuss themes such as the power of immortalization, divinity amongst humans, what it really means to be a ruler, and many other details making up the ever-present, multifaceted relationship between rulers and their subject. With the assistance of the Blanton Museum of Art, I will be able to showcase
while trying to help the residents of Pompeii. Today the type of eruption that Mount Vesuvius
the eruptive history of Somma-Vesuvius (1). Each was preceded by a long period of stillness, which in the case of the 79 A.D. eruption lasted about 700 years. These eruptions were fed by viscous water-rich phonotitic to tephritic phonolitic magmas that appear to have differentiated in shallow crustal conditions. They are believed to have slowly filled a reservoir where differentiation was driven by compositional convection. A minimum depth of about 3 km was inferred for the top of the magmatic reservoir from