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Conclusion of mount saint helens eruption
Impact of economic activities
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Mount St. Helens is a volcano that is located in the state of Washington. This paper will provide an overview on the volcanic eruption of Mount St. Helens that happened in May of 1980. This paper will also cover how this eruption affected the Earth, the damages and death tolls of this eruption, the economic impact, and any permanent consequences.
Eruption of Mount St. Helens
According to History – Mt. St. Helens (n.d.), approximately at 8:32 a.m. on May 18, 1980, a 5.1 magnitude earthquake happened about one mile underneath Mount St. Helens. Which in turn triggered Mount St. Helens to erupt without any warning. This caused the largest debris avalanche in the Earth’s recorded history. This debris avalanche caused a blast that traveled outwards
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at over 300 miles per hour. The devastation area stretched nineteen miles east to west and twelve miles north from the volcano (History – Mt. St. Helens, n.d.). How Did This Eruption Affect the Earth? According to Lindsey (n.d.), when Mount St. Helens erupted, it was kind of like opening a champagne bottle: hot rocks, ash, gas, and steam exploded upward and outward. The outward blast spread the volcanic debris over approximately 230 miles and blew down 4 billion feet of timber. A raft of dead trees drifted around Spirit Lake in Washington. All around the southern half of the mountain, volcanic mudflows poured down through rivers and gullies. Recovery for this eruption didn’t start happening until the late 1980’s and it began in the farthest part away from the volcano. Ten years later the Spirit Lake terrain started to recover and by now most of this area is coming back to life (Lindsey, n.d.). Death Tolls According to Smith (1998, May), in 2000 the Hoffstadt Bluffs Visitor Center placed in plaque in the grove trees located on their grounds in memory of the victims of the Mount St. Helens eruption. Fifty-seven names are etched into that plaque, these are the people that lost their lives to the eruption of Mount St. Helens. They were loggers, campers, reporters, and scientists. In the beginning, there were thirty-six victims brought out of the eruption area. After all the searching, rescues and recoveries, there were still a lot of people who were never found. By the third week after the eruption twenty-five people were confirmed dead and forty-seven were still missing, and only fifteen of those missing people were found alive. Four of the victims were known to be inside the restricted areas that had been set up by the federal and local governments. One of them was a man named David Johnston; he was only five miles from the volcano and was the one that reported the volcano erupting. The second was a man named Harry Truman who refused to leave his lodge at Spirit Lake. Then there were volcanologists Bob Kaseweter and Beverly Wetherald, who had been taking readings at Spirit Lake when the volcano erupted. Some of the other victims were as far as thirteen miles from the volcano, and some were in areas that were considered “safe” (Smith, 1998 May). The Economic Impact According to Bagley (2013, Feb. 28), in terms of economic impact, the Mount St. Helens eruption was the most destructive in United States history. Fifty-seven people are known to have died. More than 200 homes were destroyed. More than 185 miles of roads were destroyed and fifteen miles of railways were damaged. Sewage ways were clogged up with ash, cars and building were damaged, and air traffic was temporarily shut down in the Northwest. The International Trade Commission estimated damages to timber, civil works, and agriculture to be about 1.1 billion dollars. Then Congress approved a 950 million dollar emergency fund to be set up for the Army Corps of Engineers, FEMA, and the Small Business Administration so they could help with recovery efforts (Bagley, 2013 Feb. 28). Any Permanent Consequences According to Long Term Effects (n.d.), the agriculture around the United States was also affected after the eruption of Mount St.
Helens. As much as twelve percent of the total crops were destroyed by the ash debris nationwide. Local farmland was affected significantly; almost all of the crops and livestock that were located in the valleys at the foot of the volcano were destroyed by the floodwaters, pyroclastic flows, and lahars, which seeped down the volcano. The higher than usual damage in those valleys is thought to be due to the high concentrations of the farmland, drawn by the fertile volcanic soil. A lot of the surrounding natural vegetation was destroyed also; sections of forests were either burnt away by the pyroclastic flows or washed away when Spirit Lake flooded. Two hundred and fifty square kilometers of forest were wiped away. Rivers were filled with sediment, which include streams filled with salmon and trout. Since most of the rivers and streams were filled it destroyed most of the local drainage system, which caused a much greater risk of flooding in this area (Long Term Effects, n.d.). Permanent consequences that resulted from this eruption include the wildlife and tree life around this area would never be the same again. Nobody knows what kinds of animals were living in that area that might have died when this volcano erupted. There were so many things that scientists had yet to discover in those areas that they won’t be able to discover
now. Mount St. Helens is a volcano that is located in the state of Washington. This paper provided an overview of the volcanic eruption of Mount St. Helens that happened in May of 1980. This paper also covered how this eruption affected the Earth, the damages and death tolls of this eruption, the economic impact, and any permanent consequences of this eruption.
MILLER, C. D. POTENTIAL HAZARDS FROM FUTURE ERUPTIONS IN THE VICINITY OF MOUNT SHASTAVOLCANO, NORTHERN CALIFORNIA. N.p.: US Government Printing Office, 1980. Print.
The Fredonia Earthquake that took place in Fredonia, Arizona on July 21st, 1959 was the largest earthquake to ever strike the state and it triggered a rockslide at Mather Point in the Grand Canyon.
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
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.
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.
Mount Tambora, located on the Island of Sumbawa, Indonesia is classified as a Stratovolcano. Also known as a composite volcano, Tambora is a tall conical volcano (cone like structure) where layers of the walls are built by hardened lava and volcanic ash. The term composite is used to describe the volcano due to the composite layered structure built from sequential outpourings of eruptive materials1. Among the most common types of volcanoes, Tambora also shares its destructive prowess with best-known volcanoes such as Krakota (1883) and Vesuvius (79 A.D). The Island of Sumbawa is located in the middle of the Lesser Sunda Islands chain (a group of islands in the southern Maritime Southeast Asia) and is in the province of West Nusa Tenggara3. A map of Mount Tambora is shown in Figure 1 to provide a better perspective of its location. Interestingly enough, Tambora forms its own peninsula on Sumbawa, known as the Sanggar Peninsula. In April of 1815, after years of dormancy, Mount Tambora erupted with great intensity, approximately 7 on the volcanic explosivity index, which is shown in Figure 2. It has been estimated that the eject volume of Tambora was 160 cubic kilometres, which represents the largest volcanic eruption in recorded history. The death toll has been projected to be at least 71,000 people, of who over 15% were killed directly from the eruption1. The remaining 75% have been thought to succumb to starvation and disease, as the eruptive fallout decimated the agricultural industry in the region. Following the eruption, a volcanic winter ensued. As sun become less abundant due to clouds of ash, crops and livestock perished. Please note that all definitions appearing in the footnotes are either taken from already referenced so...
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...
Helens is located in Skamania County, Washington at a latitude and longitude 46°11′28″N 122°11′40″W. Mt. St. Helens is a stratovolcano volcano that has an elevation of 2,549m (8363 ft.). The last eruption was 36 years ago and has erupted numerous times within the last 100 years. The eruptions are explosive with ash and pyroclastic flows. Mt. Helens erupted on May 15, 1980 with a VEI 5 rating. It was the only large eruption to happen in the contiguous 48 states since 1915. Fifty-seven people were kill, along with several farm animals. Two hundred miles of land and trees were obliterated. This area is now called the Mount St. Helens National Volcanic
Deep within the Washington wilderness in the shadows of Mount St. Helen lies the infamous Ape Canyon. Upon these steep shallow cliffs, strange encounters have emerged over the past century. In 1924 a group of seasoned miners set out on a routine expedition searching for gold. However, what they encountered changed their lives forever. It was here that allegedly famous attack by a group of sasquatches occurred. In the short autobiography, I Fought the Apemen of Mt. St. Helens by Fred Beck, one of the miners, recollects his parties encounter with the beast.
The first time I saw Mt. Rainier for myself, was last summer when my boyfriend and I drove to Washington. It was the most beautiful, peaceful looking mountain I have ever seen. However, underneath it's great beauty, it hides a deadly secret. Mt. Rainier is one of the most dangerous volcanoes that we have here in the United States. One of the reasons it is so dangerous is because of it's great beauty. People enjoy looking at it, and the area that surrounds it, so they have made their homes here. Mt Rainier is not the only volcano I am interested in, in fact this last summer I also went to Mt. St. Helens and Crater Lake. But it is the volcano I chose to research for this paper because it does have so much beauty and at the same time so much power. I already know the basics about volcanoes, how they form, the different types, etc., but I wanted to find out more about what would happen if this great volcano were to erupt, what type of eruption would it be, and how would it affect the people that live around it.
It was known as the great Alaska earthquake. On March 27, 1964, an earthquake with a magnitude of 9.2 struck the Prince William Sound region of Alaska. This earthquake is the second largest earthquake ever recorded in the world, the first as a magnitude 9.2 in Chile in 1960. In other words, this earthquake released 10 million times more energy than the atomic bomb dropped on Hiroshima Japan. Equally important, this (Abby Lautt) earthquake produced landslides and caused catastrophic damage covering an area of 130,000 square kilometers, which is the entire state of Alaska, parts of Canada and Washington. The earthquake lasted approximately four minutes with eleven substantial after shock occurring over the next 24hrs causing damages in the amount of almost $400,000 and killed 131 people.
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
1980 eruption of Mt. St. Helens and the 1991 eruption Mt. Pinatubo. (Ball, J. n.d.).
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