A Report On The Buffalo Creek Basin

Introduction: The purpose of this research is to determine whether there has been a change in the overall water quality of the Lake Tarpon Basin, and if so, whether the quality has improved or worsened. The variables that will determine whether the quality has changed are: nutrients (phosphates and nitrates) and dissolved oxygen (DO). The expected changes are lower dissolved oxygen levels (from the already low levels), higher nitrogen levels (from the already high nitrogen levels), and the state qualifications still are not met for nutrients and dissolved oxygen (Levy, Flock, Burnes, Myers, Weed, River 2010). This topic relates to environmental management because the changes in water quality would be due to pollution, which relates to the question “How does human activity lead to the pollution of water stores?” The hypothesis that will be tested is that Lake Tarpon’s water quality will have worsened since the last measurements by Levy, Flock, Burnes, Myers, Weed, and Rivera in 2010.

The Chattahoochee River is located in Georgia and flows southwesterly towards Alabama. Evidence indicates that humans have been inhabitants of the Chattahoochee River for an extremely long period.

At the first station I was at, we were looking for macroinvertebrates and crustaceans. When we found one of the insects we had to determine which group they belonged in. One way to determine if the water is polluted is to look at which group the critters are mostly from. My group and I tested this by taking turns going into the creek and finding a rock to bring out. When we brought the rock out of the water and back to our group we had to make sure to turn the rock over because the critters normally live on the bottoms of the rocks and most likely would fall off if you didn’t turn it over. After we all took turns a couple of times

The Colorado River Basin starts in the Rocky Mountains and cuts through 1500 miles of canyon lands and deserts of seven US states and two Mexican states to supply a collection of dams and reservoirs with water to help irrigate cropland, support 40 million people, and provide hydroelectric power for the inland western United States [1,2]. From early settlement, rights over the river have been debated and reassigned to different states in the upper and lower basin; however, all the distribution patterns lead to excessive consumption of the resource. In 1922, the seven US states signed into the Colorado River Compact, which outlined the policy for the distribution rights to the water [3], however, this compact was written during an exceptionally

Factors that may have affected the accuracy of the readings, may have been that the observations and recordings of all abiotic data was collected from one area rather than multiple sites within the area. The students involved in data collection, had no previous experience in the use of certain equipment such as the soil thermometer and refractometer, therefore, results may have varied significantly due to inadequate/improper use of equipment.

The health of the Susquehanna River and Chesapeake Bay was found based on Biological (macroinvertebrates and wildlife) and Chemicals characteristics (pH, dissolved oxygen, phosphates, nitrates, etc.) as well as physical observations (amount of forested buffers, wetlands, etc.) Overall it was concluded that the health of the water was good to excellent. What was found was that many of the macroinvertebrates found in the water were sensitive or facultative, meaning the water quality was good enough for them to live in. Also, the level of ph, temperature, dissolved oxygen, phosphates, nitrates, and turbidity showed that the water quality was good. Finally, while we were canoeing down the Susquehanna River, observations were made on the land

The mill creek watershed is 166 square miles with 450,000 people. The main sources of water are rivers, aquifers, and rainwater. The major body of water is the Ohio River. The land around it is hilly.The Mill Creek lies at the heart, soul, and industrial center of Greater Cincinnati. This 28-mile stream begins in Liberty Township, travels through 34 communities, and flows into the Ohio River just west of downtown Cincinnati. The Mill Creek Watershed has withstood two centuries of urbanization and is poised for a comeback. The Mill Creek drew settlers over 200 years ago looking for rich, fertile farmland and water power to support industry, ultimately building Cincinnati into a prosperous industrial powerhouse.

The basin begins near Simmesport, La., and stretches 140 miles southward to the Gulf of Mexico. Currently, the Atchafalaya Basin is bound by natural ridges formed by levee building along active and abandoned courses of the Mississippi River.

Communities that was adjacent to Buffalo Creek. When operation of the mine commenced in 1945 the practice dumping of slurry or coal mining waste into the hollow also began. Coal companies who operated upstream of the communities dammed Buffalo Creek to facilitate mining operations, which created an earth dam that held back 130 million gallons of water and coal waste. On average, a thousand tons of slurry had to be dumped every day. Although there were many complaints about the safety of the coal company and its regulation of the Buffalo Creek site, nothing was ever done to improve the dam’s conditions. The Buffalo Creek project had three earth dams ranging in

The Neuse River has played a vital role throughout much of the history of North Carolina. In recent decades however the river has seen degradation of its health and ecology via massive amounts of point and non-point source pollution. The result has been numerous events of eutrophication, resulting in the ecological “dead zones” found throughout the river. Notable contributors of this pollution have been industrial plants and agriculture, most notably power plants and hog farms. As a result, federal and state agencies have enacted strict regulations and water quality standards and procedures to monitor the tributaries, estuarine areas, and main stem of the greater Neuse River watershed.

The Buffalo Creek flood of West Virginia is believed to be the most devastating coal relate disaster in West Virginia history. The flood occurred in the Buffalo Creek area of Logan County on February 26, 1972 when three dams broke and released 132 million gallons of water and coal waste known by miners as “gob,” and is a thick sludge-like material. The gob contains many toxic chemicals and pollutants such as mercury and arsenic that are left behind from the coal mining process. The wastewater would lie in settling ponds and dams until it could be properly disposed of. The water that was left over from processing coal would be disposed of in two different ways. Some of the water would be pumped from the dam back to the “tipple”, otherwise

Everything in its path is a book that describes the wreckage and aftermath of one of the most server floods to strike West Virginia. The flood struck Buffalo creek a small narrow town in the hollow of the Appalachians Mountains in the winter of 1972. Debris from hundreds of mine operations spills down the slope like ashes. Buffalo creek is one of those mountains hollow that some seventeen miles in length. Around five thousands residents lived along this hollow this small strip of land in 1972 all of whom had houses and lives were washed away by the horrific flood that stuck Buffalo creek. The town of Buffalo creek depends on the mines for their source of income and lively hood. When the flood struck all of the

[pic]we also noticed the different types of tools used to hunt from the lowest level to the most current level and retouched flakes prevailed during all periods we have determined by our excavations. This was a favorite weapon to hunt and perhaps used to hunt larger preys found in the area. The use of end scraper also prevailed for many years and it was probably used to tear up the skin to cover themselves in the cold winter time. Other tools were also found, but a significant lower number.

In Pensacola Bay the results of the Bay over time can be represented by various reports as in this report found in the years of 2007 and 2010 and from previous years in 2012-2013 reports for a rough comparison of data within past few years (2011-2014 period) and part of the first decade from (2000-2010 period). In the first set of data collected by Escambia County Utilities Authority (ECUA) that notes throughout the data on their table that demonstrates all values associated with samples taken as the Maximum contaminant Level (MCL), or the highest level of containment that is allowed in drinking water compared to Maximum Contaminant Level Goal (MCLG) that represents the level of water that represents no risk and allows for margin of safety (4). In the ECUA’s report the water quality from wells with which it uses to provide Escambia County its fresh water. Though this is not directly from Pensacola Bay, the ECUA report still reflects the

The St. Johns River is suffering from a significant environmental disaster because of toxic substances from municipal and industrial wastewater, fertilizer runoff, failing septic tanks, and stormwater. Consequently, over 55% of the river miles, 80.4% of acres of large water bodies, 59.4 % of estuaries, and 31.4% of coastline miles do not meet water quality standards in Florida (Florida Department of Environmental Protection 119). For that matter, studying those pollution problems that the river faces is vital since one can use this information to salvage the natural resource which is at the brink of destruction.