Wet Beaver Creek Research Paper

On September 17th, 2015 our group went on the Orange Trail of the State Botanical Garden of Georgia in Athens, Georgia to collect data for our lab. The biome of this area that we explored fit a temperate deciduous forest type. We walked along the trail and picked random spots to start measuring our transects. We measured DBH size and canopy coverage at 10, 20, 30, and 40 meters respectively along each transect for a total of six transects. We used a densitometer to measure the percent of canopy coverage of the tree closest to the center of the sampling points along each of the transects. We used a measuring tape to measure out 10, 20, 30, and 40 meters respectively along each of the six

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

Little Cottonwood Canyon is a site bursting with geological history, rock formations earthquake potential on the fault, prehistoric glacial formations, landslides, and many hazards associated with it. The Wasatch fault is bound to have a enormous earthquake in the future and has left behind numerous scars. The mountains have been engraved by glacial formations dated back to the Ice Age (~14,000 years ago). Rock falls and landslides have left hefty boulders as indication of erosion and moisture in the rocks. The hazards on this mountain range are mass wasting, radon, earthquakes, and flooding of Little Cottonwood Creek.

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

Dry Creek station was likely built in the spring of 1860 by Bolivar Roberts and his crew. It was one of the last stations to be built by the Pony Express. It is located four miles north of Highway 50, in Lander County, Nevada. The station was used by the Pony Express and Overland Stage as a home station (historic). The Pony Express riders would go from Dry Creek westward to the north (expedition.com). The riders had a high chance of getting attacked by the Native Americans and this proved to be true at Dry Creek. They had early problems with the Indians, which caused an attack on the workers of the station on May 21, 1860. On this day William Streeper, a carrier of heavy mail and two others found the scalped and mutilated body of the station

Designed by Lee Schmidt and Brian Curley, this 18-hole championship golf course proves the perfect course for any player. Maintained to the highest of standards, the wide fairways and wavy greens prove to be easily playable, and have become a trademark at Copper Canyon. If this doesn't encourage you to play here, perhaps you will be indulged by the surrounding landscapes that prove to make Copper Canyon a truly special course. You will also find that the surrounding landscapes is not all that this golf course offers in regards to its beauty, as over 11 beautiful lakes are featured on the course itself, making an all round mesmerizing golf course.

About two hundred forty one thousand two hundred twelve people live in Cumberland County, and all of those people somehow pollute the Conodoguinet Creek. The Conodoguinet Creek is a tributary to the Susquehanna river, which is the longest river on the American East Coast, spanning 464 miles long and draining into the Atlantic ocean. Many things, such as livestock, construction sites, fossil fuels and fertilizers, all go into the Conodoguinet creek. Now, that is A LOT of pollution that can (or will) go into the creek. This does not just affect the Conodoguinet Creek, but everything that the creek drains into, like the Susquehanna river, then the Chesapeake bay, and then the Atlantic ocean, which covers over 20% of thie whole globe! As you

As the spread of this region contains coastal borders as well as a “natural region biogeography of gulf coast prairies and marshes”. Where the two defining attributes to the area plays a role in the salinity of the soil which require a plant to be highly salt tolerant. Because of the marshes and coastal waters containments of salt evapotranspiration of the water increases the salinity of the surrounded areas subsequently resulting in the visibility of the Live Oak in the area. Live Oak’s visibility in the area is marked by a stripping pattern indicated on the map can then be inferred that the species has a high salt tolerance because of its successional status persisted over time such as the century tree found at Texas A&M University which has held place for over a hundred

At the beginning of the month we stopped at the sweetwater river crossing because the land was ideal for camping and lavish for the animals. At nightfall we were attacked by another tribe of native americans, this battle was faster although more meaningful because 7 of my close friends died in the battle. Joseph and Tom both died in the battle leaving Tom, Dave and I left in the council. Joseph's death was early on in the battle, him and his family were slaughtered horrifically as joseph was fighting off the indians he watched as his daughter was decapitated and wife's throat was cut open as she screamed and pleaded, Joseph upon watching was distracted from the task at hand and was stabbed in the stomach and was left to bleed to death on the

Voted the second most beautiful vista in America, Mount Washington is a well-known overlook of downtown Pittsburgh. Mount Washington, now a beautiful mountain with a tree covered Cliffside, was not always known for its sights. Many are unaware of the dirty environment that it used to be. Once known as Coal Hill, Mount Washington was the location of many coal mines. Back in the late 1800’s, this mountain was the source that fueled and built Pittsburgh. From the ravaging coal minds to the breathtaking Inclines, there is a lot of history that is hidden under the beautiful area which we now know as Mount Washington.

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.

Have you ever been to Washington or Mt. Rainier? Mt. Rainier is a national park in Washington, where about 1-2 million people visit each year. Mt. Rainier is a Tall mountain that reaches up to 14,410 feet above sea level. It is one of the tallest places in all of Washington!

The landscape of the watershed ranges between 500 feet and 5000 feet in elevation (seattle.gov). The lower watershed includes the Cedar River and the basins downstream of Cedar Falls to Landsburg, while the upper region includes mountain valleys and ridges above Cedar Falls to the eastern end at the Cascade Mountains (seattle.gov). 95% of the lower region is covered with second-growth forest ranging from 70 to 199 years old, and are mostly conifer forest or mixed conifer/deciduous forest (seattle.gov). The upper watershed is the area that would make better suitable habitat for the Golden Eagle. The upper region has a larger range of forest types than the lower region, and is dominated by conifer forests, including some old growth forest (seattle.gov). 95% of all the old growth found in the watershed is located in the upper region; about 13,155 acres total (seattle.gov). The sizes of the old growth fragments range from a few acres to 3,000 acres (seattle.gov). Most of the old growth is above 2,500 feet in elevation and west of the Cedar River delta

The American beaver’s selective personality extends into habitat selection as well. Factors affecting beaver settlement include vegetation cover, stream gradient, bank slope, hydrological order, and proximity to established colonies (Alejandro G. Pietrek et al. 2015). Beaver habitats are more likely to occur where there is an abundance of woody vegetation (Paul D. Curtis et al. 2004). Researchers in New Mexico introduced beavers on a river in the Chihuahuan desert, and found that they were selective about which pools of water to live near, and that the spots where they resided typically had increased woody plant diversity. (Isidro A. Barela

To analyze the need for a pulse flow in the lower Colorado River, we assessed the historical streamflow data of the Colorado River. We first created a time series, Figure 3, of the streamflow of the Colorado River below the Yuma Main Canal in Arizona, which is a few miles upstream from where the pulse flow was added at the Morelos Dam. Each data point represents the monthly mean streamflow rate (discharge rate) in cubic feet per second, from 1963 to 2016, as reported by the United States Geological Survey (USGS, 2017). The red linear trend line in Figure 3 shows the overall trend in the streamflow rate during this time period.