Cedar River Watershed Research Paper

The topography of the watersheds throughout Sevier County vary amongst three different watersheds in the Upper Tennessee River Basin (Upper). The Holston River Watershed covers approximately 999 square miles and it drains into the Tennessee River (Holston). The Pigeon River Watershed is partially located in Tennessee with only 153 square miles of its 704 square miles in Tennessee, and it drains into the Pigeon River (Pigeon). The Lower French Broad River Watershed is made up of 796 square miles, and it drains into the French Broad River (Lower).

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

Cedarville University is a college I would like to attend. There are almost 3,500 undergraduate students currently attending Cedarville. It has several large academic departments, including nursing, business administration, and education. Cedarville has a presence in 47 states and U.S. provinces, as well as 28 countries, including France, Germany, Ireland, and Wales. (Supplee 41)

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

This was attributed to the ranges of vegetation type with elevation and slope, with mixed conifer tree species growing at higher elevations with increased tree cover. Similar patterns can be identified with the Rim Fire in the Stanislaus National Forest. The Pinus ponderosa (ponderosa pine) or Calocedrus decurrens (incense cedar) tree species tend to favor higher elevations, slopes between 0 - 45 degrees, and aspects between 0 - 33 degrees from North (Myers).

a canoe or kayak trip, the Ogeechee Tiver is a great place to spend an afternoon outdoors. Put a boat in one of the many landings or stay along the banks; anyone with a fishing license can fish legally along the banks of public rivers. Find your lucky fishing hole as the river is filled with red breast, suckers, shad, rock crappie, bass, and catfish. Enjoy the scenic views of high bluffs and wildlife as you drift down the river that runs wild across the flat land of Jenkins County. Public access to the river is available at the Bull Hole located in the Herndon Community, Scarboro Landing located at the Scarboro Community just off Highway 17 South, Old

After viewing each habitat it became easier to understand how each overlaps the other. You will have vegetation in the pine flatwoods that should be growing in the forested wetlands and other vegetation growing in the forested wetlands that should only be growing in the live oak hammock. It is understandable how someone who is surveying this area would have a difficult time determining the exact habitat they are in.

Historically, this region was host to communities of Native Americans (East West Gateway Council of Governments, 2007, Leland, 1953). The abundance of freshwater and navigable rivers has attracted communities of people, and subsequently, commerce (Foley, 2000). Naturally, resources throughout the land have been extracted and utilized to further build these communities and attract prospective businesses. In the 19th century, this watershed was impacted by mining, logging, and grazing practices. In the early 20th century, logging dominated resource extraction (East West Gateway Council of Governments, 2007) which swiftly impacted the landscape. Ultimately, as logging stressed this region’s resources, state legislation allowed the federal government to purchase large tracts of land to establish national forest. Soon after, the national mobilization of the Civilian Conservation Corps, during the height

USDA - US Forest Service - AEM (n.d.). Mount St. Helens Research. Retrieved September 17, 2013, from

Multiple Japanese settlements started to increase in rustic communities of the Columbia River Basin, despite the Issei’s harsh labor in the early 20th century, the discrimination led to growing anti-Japanese arrogances on the West Coast, even the feeling had developed against the seeming Chinese competition. Nampa, and Caldwell Idaho drove out the Japanese workers this led to white mobs around Coeur d’ Alene and in Poland to threaten the Japanese railroad workers. Pressures led to the (“Gentleman’s Agreement”) between the U.S. which effectually limited the numbers of laborers that could travel from Japan in 1908.

The Colorado River Basin is also home to a range of habitats and ecosystems from mountain to desert to

The Shawnee National Forest is one of the most prominent forest in not only Southern Illinois, but also the United States and around the world. A large portion of the Shawnee National Forest provides fish and wildlife habitat. These habitats provide a wide variety of activities to the local area and create quite an economic impact for the region.

The reason why the Delta wetlands is larger than twenty years ago is because of deposition. It takes all of the dirt and sediments underneath the river and deposits all of the sediments and dirt into the marsh bigger and expanding the delta wetlands that’s why the soil is so soft and mushy is because there is a lot of water in the soil.

The Tillamook State Forest is located in the Northwest part of Oregon. It stretches from the west side of the Coastal Mountain Range over to the North Coast. In all it is about 800 square miles with elevations from sea level to 3500 feet (Greenwald & Garty, n.d). In the Tillamook State Forest is also called the Tillamook Rainforest. This area is one of the wettest in the United States getting about 100 inches of rain year round, with the higher elevations getting snow during the winter. The forest is home to several animals and insects. Some of the most noted animals are grizzly bear, spotted owl, white tailed deer, elk, and in diminished numbers gray wolf, and California condor (Greenwald & Garty, n.d). There are about 300 miles of

In area one, the douglas fir was the dominant one in the area , then following that was the bay . This only shows only two species allocating in the area that siphons resources. If one declines, the other dominants , this does not show as much diversity in that aspect. In area 2, there was spread of dominance, the species that had the greater dominance was oregon white following that was the black oak, then the live oak then the bay. This shows more diversity than area 1.