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Short note on volcano
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Article Summary of Mount St. Helens
In the article Making Sense of Mount St. Helens by Steve Nash, the author discusses the huge, catastrophic eruption in 1980, the environmental impact of the eruption, biological legacies, how the eruption helps better understand the process of succession, and the resurgence of scientific research at Mount St. Helens. Nash talks about the restrained locution of ecology, and what occurred in 1980 was not just a "disturbance." It instantly altered the still Fuji-form symmetry volcanic look, with lush forests, meadows, and clear, snow-fed lakes extending north around a huge, deep side-blown crater (Nash, 2010). The eruption's first phase was the largest avalanche in recorded history, with speeds up to 70 meters per second. This was followed within seconds by a blast that elevated matter up into the sky that rained ash over 11 states. Mudflows began almost immediately, hurling liquefied sand, gravel, rock, earth, and other debris down the North Fork Toutle River Valley, some of it eventually reached the Columbia River. The May 18, 1980 eruption was the most economically destructive volcanic event in U.S. history, 57 people were killed.
Despite the enormous destruction and loss created by this eruption, it also set forth an equal potential for creation. The eruption created an opportunity for scientists and researchers to study the changes the natural destruction formed on the landscape. Following the eruption, Nash talked about a scientist, Virginia Dale, who made a research proposal a few days after the eruption. "There was a lot of interest in how life was going to return to the area" she says now. "A general sense was that life had been wiped out in the blast zone, so a big question was what's goi...
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...are, especially where we know what's happened for 30 years” (Nash, 2010).
Mount St. Helens has helped revise one of ecology's oldest preoccupations: trying to recapitulate the story of how communities of plants and animals assemble themselves over time--how one suite of species succeeds another (Nash, 2010). The author explains that there is far more biological diversity at Mount St. Helens today than before the eruption. That after 30 years, Mount St. Helens had a boisterous return of thousands of species. But, the reassembly of the former evergreen forest could take hundreds of years, or it may not return at all. More eruptions may generate a different outcome, or Global warming might just bring a more open, pine-dominated forest instead. Mount St. Helens has become a biological hot spot for the whole Cascade Range, from California to British Columbia (Nash, 2010).
In this book, Kolbert travels to many places to find out what is happening with global warming. Quite often she ran into the same fear at the places she went, the fear for loss before the next generation. When she went to Alaska, many people were fleeing from their homes because the sea ice surrounding them, creating a buffer zone for storms, was melting and that was causing houses to just be swept away.
The Logging Industry vs. The Old Growth Forests of the Pacific Northwest and the Northern Spotted Owl.
In this research paper, I will address the changes that occurred within the ecosystem of Yellowstone National Park since the reintroduction of the grey wolves. The paper will consist of four sections; the first section will include the history behind the extirpation and subsequent reintroduction of the gray wolf in Northern America. The second section will explore the political controversy that surrounds the reintroduction of the gray wolf in Yellowstone. The third section will contain discuss the gray wolf and its impact on the ecosystem of Yellowstone. I will conclude my essay by explaining how the gray wolves act as climate change buffers in Yellowstone amidst global warming.
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.
We don’t often stop to consider the impact that simply living our human lives has on the other species that once called our neighbourhoods their home. The Fraser Valley, “one of the most important and complex ecosystems in the country” (Thom, p. 171), has been dramatically altered to make a more convenient landscape for housing and farming. In this process, critical habitat has been destroyed and many species that were once abundant have disappeared from our area (Cuthbert p. 24). Urbanization is ongoing and is thought to be the most significant threat to the incredible biodiversity found throughout British Columbia, and particularly the population-dense Lower Mainland (Harding, p. 355). Biodiversity, the “complex web that sustains life on this planet” (Austin, et al., p. 5), is vital for our survival as humans (Cuthbert p. 74). Any loss of biodiversity affects the entire ecosystem and all organisms within it (Fetene et al., p. 52). In the quest to house the ever-expanding human population, we must also consider habitat conservation and seek to preserve the rich biodiversity found in the Fraser Valley that supports and enriches our lives.
The plants growing among Montana’s peaks and valleys range from tall evergreen trees to grasses. The mountainous areas are covered with forests. However, at each level, from the mountaintops to the valleys, there are different, distinct collections of plant life. The mountainsides are largely covered with towering spruce, pine, cedar, and Douglas fir trees (Av2
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. ...
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
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.
A volcano is a mountain that opens downward to a pool of molten rock below the surface of the earth. When pressure builds up, eruptions occur. In another definition it is a mountain
Earth has physically changed millions of times due to moving tectonic plates which has formed our planets mountains; altering the way our environment looks. Volcanoes, (formed when magma from the upper mantle heads to the surface, causing the land to rise) are one of nature’s finest spectacles. These geographical forces have erupted many times; from small-scale eruptions to cataclysmic ones; making them a force to consider about. Therefore the past is useful in predicting possible future eruptions as in terms of the effects they can have on civilisation, they are unpredictable in what they can produce.
Many of us know Mount Shasta to be a beautiful mountain and a popular tourist location in California. However, this mountain is much more than that, this mountain is actually a volcano. Volcanoes come with a number of hazards and a volcano of this size is of no exception. Previous eruptions on Mount Shasta have given us an idea of the power this volcano has and the damage it may do. With this information scientists are able to predict what may happen should another explosion occur.
Boom! A once ice-capped mountain peak explodes as ash fills the air. “‘Vancouver, Vancouver, this is it!’”Those were the last words of expert geologist David Johnston (Gunn 561). In 1980, Mount Saint Helens of the state of Washington erupted, filling the air with ash and causing mudflows powerful enough to lift tons. It decimated everything in its path. The eruptions, mudflows, and ash caused great damage on the landscape, yet it gave us information on how catastrophes happen and how they affect society and the surrounding landscape. The data acquired can also help us understand the way the landscape was formed. Mount Saint Helens caused much damage, but also helped people understand the science behind it.
37,600 years ago with dacite and andesite eruptions of pumice and ash. Mudflows were very significant forces in all of St. Helens' eruptive cycles. Starting around 2500 BC eruptions of large amounts of ash and yellowish-brown pumice covered thousands of square miles. This eruptive cycle lasted until about 1600 BC. After 400 years of inactivity, St. Helens came alive again around 1200 BC. This cycle, which lasted until about 800 BC, is characterized by smaller volume eruptions.
Digging up the dirt on Mauna Loa. (Hawaiian volcano studied) Science News v144, n25-26 December 18th, 1993 414 (1 page)