Wait a second!
More handpicked essays just for you.
More handpicked essays just for you.
Famous volcano Mount Vesuvius
Differences between mt vesuvius and mt st helens
Don’t take our word for it - see why 10 million students trust us with their essay needs.
Recommended: Famous volcano Mount Vesuvius
Mount Vesuvius and mounts St Helen's are both volcano's, but what are the differences and what are the similarities . That is a question i've been wondering how and when did they erupt . and there are a lot of similarities with the bout one. And they have an lot of differences as they both are stratovolcano
As for the differences Vesuvius erupted in 79 A.D as for St Helen erupted in 1980 A.D . As well, many people died during Vesuvius and only 57 people died during Helens eruption St Helen had an advanced technology that said it was about to erupt will Vesuvius did not have a advanced notice and the eruptions happened to different places Vesuvius was in Italy while Helen's was in Washington . As of for the size of the eruption Vesuvius was
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
On May 18th, 1980, one of the most prominent volcanic eruptions in US History took place in the state of Washington. Mount St. Helens had been dormant for almost 100 years before March 15th. On this day, two months before the eruption several small earthquakes shook the earth. This indicated a magma buildup below the surface, and the first minor event that would lead to one of the greatest eruptions the US has ever known. Following the first set of earthquakes, “Steam explosions blasted a 60- to 75-m (200- to 250-ft) wide crater through the volcano 's summit ice cap and covered the snow-clad southeast sector with dark ash. Within a week the crater had grown to about 400 m (1,300 ft) in diameter and two giant crack systems crossed the entire summit area. Eruptions occurred on average from
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.
The eruptions were very different too. Here are a few differences of Mt. St. Helens, it was 9,600 feet tall in a symmetrical cone shape, it erupted on May 11 1980 at 8:32am, the eruption blew the whole side of the mountain off and the eruption removed the upper 1,300 feet off forming a horseshoe shaped crater, it
This cycle, which lasted until about 800 BC, is characterized by smaller volume eruptions. Mt. Saint Helens woke up on March 20, 1980, with a Richter magnitude 4 earthquake. Steam venting started on March 27. By the end of April, the north side of the mountain started to bulge.
To start, these names are the names of two big volcanos, both in Washington State, both deadly, but on different scales. Mt. Rainier’s last eruption was 150 years ago. Yellowstone’s last eruption was 640,000 years ago. Yellowstone’s reputation of being the ultimate super volcano versus Mt. Rainier, the most dangerous volcano in the country. The difference between these volcanos is looks, damage, stability and tourism.
Many times in life things are not as they seem. What may look simple on the surface may be more complicated deeper within. Countless authors of short stories go on a journey to intricately craft the ultimate revelation as well as the subtle clues meant for the readers as they attempt to figure out the complete “truth” of the story. The various authors of these stories often use different literary techniques to help uncover the revelation their main characters undergo. Through the process of carefully developing their unique characters and through point of view, both Edith Wharton and Ernest Hemingway ultimately convey the significant revelation in the short stories, “Roman Fever” and “Hills Like White Elephants” respectively. The use of these two literary techniques is essential because they provide the readers with the necessary clues to realize the ultimate revelations.
Roman sarcophagus depicted mythological scenes since the 2nd and 3rd century AD, and over time we can see a gradual change in the way these myths were depicted. Beginning as a set of stories, they transformed into an expressive medium through which the myth could explicitly commemorate the live of the deceased and a way so Roman cultural requirements could be presented and explored. Specifically, myths that depict heroes on sarcophagi usually stress the virtue of the hero and the grief felt at their death. The virtue of heroes is commonly seen with men such as Herakles, and the completion of his twelve labours. Conversely, the Alcestis myth illustrates that women can be depicted as heroes as well. Alcestis was the subject of a Euripidian tragedy,
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
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)
These differences are in the makeup of the volcano, the impact on society, and the eruption itself. Mount Saint Helens, used to be a wonder of the world, but now a damage site of what happened on May 18, 1980. Mauna Loa is a tourist destination and one of the most active dispensers of lava and magma in the world. As shown, these volcanoes can’t be more different. Yet, each volcano has been a culprit to destruction, and have similarities within themselves. This report has expressed many similarities and differences and brought facts and knowledge to the historical eruptions by these impressive and ancient structures of
1980 eruption of Mt. St. Helens and the 1991 eruption Mt. Pinatubo. (Ball, J. n.d.).
Stratovolcanoes are the most common type of volcanoes. Mount Fuji, Japan and Mount Rainer in Washington state are examples of stratovolcanoes
Mount Vesuvius is a strato-volcano consisting of a volcanic cone (Gran Cono) that was built within a summit caldera (Mount Somma). The Somma-Vesuvius complex has formed over the last 25,000 years by means of a sequence of eruptions of variable explosiveness, ranging from the quiet lava outpourings that characterized much of the latest activity (for example from 1881 to 1899 and from 1926 to 1930) to the explosive Plinian eruptions, including the one that destroyed Pompeii and killed thousands of people in 79 A.D. At least seven Plinian eruptions have been identified in