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Industrialization impacts on the environment
Acid rain impacts on environment
Industrialization impacts on the environment
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The Adirondacks are a group of mountains surrounded by many lakes and rivers, that cover over 5,000 square miles in the northeastern part of New York. There are a lot of large tourist villages on every lake. Motor boating and other water activities take place on almost every lake in the area. It is a vacation paradise for thousands. But, industrial emissions from Canada and the Ohio river valley always drift to this area and cause acid rain.
This silent killer is destroying these beautiful lakes and their surrounding watersheds. Acid rain has an adverse effect on the lakes, and their surrounding watersheds, of the Adirondacks in New York State.Acid rain is defined as chemically polluted rainfall. It's causes are: coal burning plants, industrial factories, smelters, and car emissions. It's formed by water molecules combining with the sulfur dioxide emitted by the burning of coal and with nitrogen oxide from auto emissions.
The result is an acidity level that's harmful to fish, wildlife, plants, and trees. Already, 1,200 lakes in the U.S. have been completely acidified so the lake water is unfit for human use and little or nothing can live in it.Such is the case in the Adirondacks, which are a group of mountains surrounded by many lakes and rivers. They cover over 5,000 square miles in the northeastern part of New York state. It's an area where large resort villages are around the Saranac river and Lake George.
Lumbering and mining for iron and graphite go on in this area and it was once a place for major industry. Unfortunately, this is an area where acid rain has become a regular part of the water that flows through it.In recent years, acid rain hasn't really been in the news because people have felt that the problem has been taken care of so, therefore, it's not around anymore. However there has been no evidence that the acidification of lakes in the Northeastern U.S. has stopped or even slowed down. The analysis of sediments from lakes in the Adirondacks has shown that acidity started rising in the 1930's and 40's and has been rising steadily ever since. There are two possible reasons for this.
Scientists have been studying the chemistry of the rain and they've discovered that while the deposition of sulfuric acid has decreased in the last two years, the deposition of nitric acid has increased. This means that the acidity of the rainfall hasn't really changed.
This is a report based on three days of observations and testing in the region known as the Peterborough drumlin field. It will address a variety of regional elements, such as climate, soil, vegetation, hydrology, geomorphology, and geology. A variety of sites located on the Canadian Shield, the zone of thick glacial deposits to the south, and the transition between them will be the focus of the report. It is supplemented with previous research on the region. September 8, 1999, day one of the field study involved an area of largely granite bedrock that is part of the Canadian Shield and is the most northern point of study (see Map 2). September 9, 1999, day two, involved three main areas of study: the Bridgenorth esker (Map 3), Mark S. Burnham Park (Map 4), and the Rice Lake drumlin (Map 6). These sites are in areas of thick glacial deposits. September 10, 1999, day three, involved studying the Warsaw Caves (see Map 5) as a transition zone between Precambrian Shield rock to the north and Paleozoic rock to the south. A general map of the entire study region is provided by Map 1.
The Appalachian Mountains in the nineteenth century landscapes are often depicted in a grand, glorious, and often spiritually uplifting form. The Hudson River School artists painting in the romantic style engages viewers to tell a story through naturally occurring images as well as interior knowledge of the times at hand.
The Mixedwood Plains ecozone is composed of waterfalls, rivers, plains, and wetlands. The last continental ice sheet covering the ecozone melted 11 000 years ago, leaving thick clay deposits. Underneath, the ecozone is sedimentary rock, while up above, it is mostly plains and rolling hills with some notable features being Manitoulin Island, the Great Lakes, and the Niagara Escarpment. More than 6000 drumlins span the ecozone, as do bodies of freshwater. Approximately 42% of the total surface is made up of lakes and rivers, including four Great Lakes – Superior, Huron, Erie, and Ontario – as well as the St. Lawrence River.
More specifically, Trois-Rivieres is located in an area with flat and rolling hills, and fertile soils that play a huge part of Trois-Rivieres’s economy. The formation of the Great Lakes-St Lawrence Lowlands happened during the Paleozoic era. “The Great Lakes-St Lowlands were formed by the effects of glaciation. This is caused the city’s rolling landscape where flat plains are interrupted with glacial hills and deep river valleys. After the glacial period, when a large volume of water melted out from the glaciers, the lakes were large, even larger than they are today. However, the lakes shrank to their present size, and flat plains of sediments remained. These sediments formed excellent soil for farming” (Pandya, n.d). This process left behind a large amount of sediment rock, which was beneficial for the manufacturing industry.
The average elevation in the Hudson Plains is 120m above sea level. It is a flat lowland area. The land is made up of mineral soils, with few outcrops of underlying sandstone and shale. This land was created when the weight of glaciers depressed the Hudson Bay region and the ocean waters flooded areas up to 300 km inland from the current coastline. Then, during the retreat of the huge continental ice sheets, drainage into the Hudson Bay was blocked and lakes (Agassiz and Ojibway for example) were formed along th...
The area surrounding the Cuyahoga River is notorious for being extremely polluted and industrialized. An exception to this is Cuyahoga Valley National Park. This area has a rich history and has been used as a source of livelihood, industrialization, and recreation for centuries. This rural oasis takes up nearly thirty two square miles in northeastern Ohio and is the only National Park in the state. It became recognized as an official National Park in 2000 and before was known as the Cuyahoga Valley National Recreation Area. Cuyahoga Valley National Park preserves a rural landscape along the Cuyahoga River and serves as a contrast to the otherwise metropolitan setting.
Algonquin Park is the oldest and most famous provincial park in Ontario and one of the largest in Canada. It stretches across 7,725 kilometers of wild and beautiful lakes and forests, bogs and rivers, cliffs and beaches. This is why Algonquin is also known as a canoeist's and camper's paradise as far as the eye can see.
Tedesco, Mark A. "This Fine Piece of Water: An Environmental History of Long Island Sound." Journal of the American Planning Association 69 (2003): 321. BigChalk. 9 Nov. 2005.
The tundra artic plains completely covering most of the earth’s lands north of the coniferous forest belt. The tundra’s ecosystem is very sensitive. It doesn’t have a good ability to restore itself. Controlled by sedge, heath, willow, moss, and lichen. Plains that are pretty much alike, called alpine tundra, occur above the timberline in the high mountains of the world. Even the Antarctic area has a couple of its own arctic regions itself.
The United States Environmental Protection Agency (2005) defines mountaintop removal as “a mining practice where the tops of mountains are removed, exposing the seams of coal.” Coal companies throughout Appalachia adopted this process as a means of acquiring coal faster. People in support of mountaintop removal concentrate, not only on the cheap, plentiful energy which is produced, but also the supposed increase in safer occupation opportunities for miners. Such individuals also argue that flattened land provides space for airports, prisons, and shopping centers. However, mountaintop removal has serious consequences, which need to be revealed.
Acid rain has been proven to have damage forests, fresh waters and soils, killing insect and aquatic life-forms. It also causes damage to buildings and impacts on human health. Many people do not know what acid rain actually is. Acid rain is any form of precipitation that is unusually acidic, low pH levels, higher than normal amounts of sulfuric and nitric acid, occurs naturally and from man made sources. Forms when gases react in the atmosphere with water, oxygen, and other chemicals (what is acid rain?). The only water that will not have some amount of acidity is pure water. Pure water has a pH of 7 which is neutral; regular, unpolluted rain water has a pH of around 5.6. The acidity in rain water comes from the presence of Carbon Dioxide, Nitrogen Oxide, and Sulfur Dioxide. CO2 reacts with water to form carbonic acid. Nitrogen and water react during lightning storms, forming Nitric Oxide. NO is then oxidized to form N02. The NO2 reacts with water to form nitric acid. Due to this, the pH is lowered to be slightly acidic (Acid Rain). Acid rain can occur naturally in the environment, but the problem occurs when human interaction is the cause of the acidic levels.
As swans drift with the current on a secluded lake in upper Canada they think not of the water they are in but of dreams of the past and wants for the future. On the other hand, seals off the coast of Northern California fear for their lives every day of humans exploiting their natural habitat. Many things can endanger water born animals, and most all of these come directly from humans. The pollutants of water come from many sources both close and far away from the water body itself. Wastes of humans are the major cause of pollution in the water, such materials include sewage, chemicals among other notable items. First, the composition water: water is odorless, tasteless and a transparent liquid. Though in large quantities water appears to have a bluish tint, it maintains the transparent tendency when observed in smaller quantities. Water covers approximately seventy percent of the Earth's surface in the solid and liquid form. Pollutants can be carried over a great distance by combining with evaporating moisture, forming clouds and then the wind taking the clouds to the larger body of water. This process is called acid rain and it is a major source of water pollution. Acid rain has been a problem since the Industrial Revolution, and has kept growing ever since. With acid rain moving over to a fresh water body, the plants and animals could experience pollution that they never had to deal with before and they could possibly die for the sudden change without them having time to adapt, if this is possible.
The Arctic Tundra The Tundra is located in the northern regions of North America, Europe, Asia, and Africa. as well as a few regions of Antarctica. The Tundra is the second largest vegetation. zone in Canada. It can be divided into three different sections: the High Arctic Tundra, the Low Arctic Tundra and the Alpine Tundra.
The Great Lakes, including Lake Superior, Lake Michigan, Lake Huron, Lake Erie and Lake Ontario, are the largest freshwater lakes in the world, accounts for about 18% of the world 's fresh water resources. They are rich in water and other resources and the area of the Great Lakes extend more than 1200 km. The storage capacity of Great Lakes is about 23000 km3 and the surface area is around 244000 km2. Nowadays 1/10 of the Americans and a quarter of Canadians live in the lakes. Some of the world 's largest industrial center is built on here. Almost 25% of total agricultural production in Canada and 7% in the United States will yield in this area. Although the area of the lake is large, it could be affected by a wide range of pollutions
The foundation of the Great Lakes began around three billion years ago, which is known as the Precambrian Era. The Precambrian Era contains numerous ecological events, which consists of volcanic activity to erosion to the mountains and hills seen today being formed. Then during the Pleistocene Epoch or known as the “Ice Age, occurred between 1.6 million and 10,000 years ago. At least four times during the Pleistocene Epoch, large masses of ice advanced and retreated over the surface of what is now North America. As the glaciers advanced, giant sheets of ice flowed across the land, leveling mountains and carving out massive ...