The Water Systems And Landforms

Giving full credit to restricting the Mississippi River as the culprit for loss of wetlands is not accurate. The booming oil and gas exploration of the 1970’s and 1980’s merits a name on the marquee as well. The pipelines and canals used to transport the resources to the outside world placed a great deal of stress on the fragile wetlands. Erosion from the barges in and out of the marshes as well as the salt water allowed into the fresh water, providing a precarious habitat for fresh water species – flora and fauna alike. Plants provide root systems to hold soil in place. Fish and fowl provide an economy for the area. Enter

One of the largest geographic physical structures in the United States is the Colorado River. Human activity and its interaction with this great river have an interesting history. The resources provided by the river have been used by humans, and caused conflict for human populations as well. One of these conflicts is water distribution, and the effects drought conditions have played in this distribution throughout the southwestern region. Major cities such as Las Vegas, Los Angeles, San Diego, and other communities in the southwest depend on the river. It provides water for over 20 million people, irrigation for 2 million acres of land, four thousand megawatts of hydroelectric energy, and over twenty million annual visitors for

Surface water commonly is hydraulically connected to ground water, but the interactions are difficult to observe and measure (Winter, 1998). Interaction depends upon understanding the effect of topography, geology and climate of the groundwater

It's not actually a silly question. The Mississippi no longer fits the definition a river as "a natural watercourse flowing towards an ocean, a lake, a sea, or another river." Rather, the waterway has been shaped in many ways, big and small, to suit human needs. While it maybe not be tamed, it's far from wild -- and understanding the floods that are expected to crest in Louisiana soon means understanding dams, levees, and control structures as much as rain, climate, and geography. From almost the moment in the early 18th century when the French started to build New Orleans, settlers built levees, and in so doing, entered into a complex geoclimatic relationship with about 41 percent of the United

Questions and charts are from Geoscience Laboratory, 5th ed. (p. 155–167), by T. Freeman, 2009, New York, NY: John Wiley & Sons. Reprinted with permission.

Questions and charts are from Geoscience Laboratory, 5th ed. (p. 117-130), by T. Freeman, 2009, New York, NY: John Wiley & Sons. Reprinted with permission.

For this paper water structures and infrastructures were selected as focus points because the longer we wait to fix issues with them, the more expensive it will get, in other words, we are in a race against time. Studying the past it is easy to see how water availability made population explode in an area such as Southern California, where savvy marketing and great politics made it happen. Particularly, for Los Angeles and for the purposes of public narrative, Marc Reisner’s Cadillac Desert does a great job at understanding and identifying the politics and key figures in getting water to Los Angeles. Great hydrologic structures were created using both manpower and water politics. It is important to state that there are connections between water, politics, environment, and geography when analyzing what the biggest problems involving water structures and infrastructures (Reisner.) We must think of water as both a socio-political issue and a natural resource, whose fate is molded by the understanding of its connectivity to itself, man-made structures, geography, environment, and society. The classes taken in this program have taught us ideals that in order to become a great water resource manager, one must master the political and scientific knowledge to make decisions that are prosperous for society and the environment. Furthermore, one must know the United States’ hydrological history in order to gain manipulation upon the system that makes it both thrive and deteriorate.

Louisiana should be concerned about the wetlands because of the wildlife and fisheries. Without it, Louisiana would not be able to supply seafood and wildlife. Another concern, is the land going under and people could lose their homes. According to Allured and Martin, “the destruction of the wetlands came from the coastal and offshore oil and gas development” (p.332). Also, there is some thought that humans play a role in the destruction. According to Allured and Martin, “swamps symbolize as dark and chaotic places of the earth” and “marsh as a type of wet area that harbored disease” (p. 333). The importance of ascertaining the cause of the vanishing wetlands is to help restore the wetlands and protect from a hurricane

In his book, Cadillac Desert: The American West and Its Disappearing Water, Marc Reisner’s main thesis is to show the inefficiency, greed, and inherent difficulty in the American West’s never-ending struggle to turn its unwelcoming desert into a lush garden. One of his main sub-points is that the West is not meant to support millions of people. It has a wide range of geographic challenges throughout the entire region. Its inconsistency and diversity is a primary cause of its water problems. For example, Reisner notes that the West consists of “plains so arid that they could barely support bunchgrass; deserts that were fiercely hot and fiercely cold; streams that flooded a few weeks each year and went dry the rest; forests with trees so large it might take days to bring one down; . . . hail followed by drought followed by hail;” (23).

Questions and charts are from Geoscience Laboratory, 5th ed. (p. 133-150), by T. Freeman, 2009, New York, NY: John Wiley & Sons. Reprinted with permission.

Louisiana has many wetlands, rivers, lakes, and coastal plains. One river that stretches over a great part of Louisiana is the Mississippi River. Lake Pontchartrain is the

Hydrologic studies has always been the subdiscipline of environmental science that has most intrigued me; probably because the eco- and geological systems that comprise surface and shallow groundwater systems are so inexorably entwined and very delicate. Both of the virtual labs were interesting, and paint a clear picture of how we affect our hydrosphere and how that, in turn, affects us. Spotsylvania County and the city of Fredericksburg share four water treatment facilities that pull water from the Mott's Run Reservoir, the Ni River, and the Rappahannock River, which is the largest river in the local area, the other two being smaller tributaries that feed into it. The Rappahannock River is a significant body of water, providing the potable water for roughly a quarter-million people. Toward the coast the river sees mostly recreational and some light industrial use, and further upstream it is affected by many small to midsized agricultural operations that take place on the land adjacent to the river.

The Mississippi River influences the states of Louisiana in numerous ways. The river can be both beneficial and harmful to the state. It may help with industries, but at the same time it may be harming by taking away from Louisiana’s coastline. While erosion is widely considered to be a destructive occurrence, it does have some necessary features. For example, erosion provides many nutrients for animals living in the water, and it creates new deltas that many animals live in. Since the beginning of Louisiana, the Mississippi River has been a crucial factor in the creation and the development of Louisiana’s economy. It has helped with things like trade and the growth of crops. The Mississippi is also significant in the way Louisiana is shaped

A mass curve and double mass curve were created for the Red Deer basin at Drumheller in 1964. Precipitation data was collected from the city of Drumheller, which is approximately 0.6 km from the river measurement. On average the greatest amount of precipitation occurred in May, June, and July, but there was a large spike in precipitation in the month of September. The lowest amount of precipitation occurred in January, February and October. The double mass curve for this basin has a large gradual increase. Runoff for this basin is always greater than precipitation, but there is an area of large run off and storage during the end of the curve. This could be due to the large amount of precipitation that occurred in September, and storage

This paper discovers the water budget for Berkeley, California in comparison to Terre Haute, Indiana. The two cities precipitation differs throughout the twelve month calendar year where many of the heavy precipitation months are totally opposite. Berkeley California’s winters, where the majority of rain occurs and Terre Haute, Indiana where the rainfall is observed as consistently disseminated throughout the year evenly. This paper will also magnify geographic position, climate and elevation in contrast of the two cities that reflects the water budget outlined in Project 1: Water Balance defined in