Essay On Sediment Fingerprinting

In site one there was a high proportion of very unspherical rocks. According to this the hypothesis is right, in site two there is a lot more smother rocks medium sized and in site 3 there are very small pebbles which are very smooth and spherical. The pebbles get smoother and rounder while it goes downstream. Due to us only taking about 10 rocks our result may have been not right as there were some pebbles which were largely over sized. Most of the other load is dissolved by solution such as limestone and chalk

“Erosion occurs when the soil lacks protective vegetative cover”. (Pimentel, Kounang, 1998) “Soil erosion reduces the productivity of the land by loss of water, soil, organic matter, nutrients, biota, and depth of soil.” (Pimentel, Kounang, 1998) With no conservation methods in place in certain places like: no contour farming, no cover crop, no terraces, no water ways, and tillage on steep hills is asking for a loss of productivity from the land. The effects on the land that non-conservation methods have is horrible. “Its effects are pervasive, and its damages are long lasting. (Pimentel and others 1995a)” (Pimentel, Kounang, 1998) Soil loss is a bigger factor then most people think. For an example an comparison of how much soil is actually lost in certain environments: “On sloping agricultural land under tropical rainfall, as much as 400t/ha/yr of soil is lost (Pimentel unpublished report,1990).”(Pimentel, Kounang, 1998) “Under arid conditions with relatively strong winds, as much as 5600t/ha/yr of soil has been reported lost (Gupta and Raina 1996).” (Pimentel, Kounang, 1998) Soil loss is a huge factor when conservation practices are not put into place. “According to some investigators, approximately 75 billion tons a fertile soil are lost annually from the world’s agricultural systems (Myers 1993).” (Pimentel, Kounang, 1998) Soil loss is a huge factor and many different things can be done to help slow it,

There are six different types of water erosion: splash erosion, sheet erosion, rill erosion, gully erosion, valley or stream erosion, and bank erosion. Splash erosion is when raindrops hit soil and small soil particles are displaced. Sheet erosion is when raindrops remove soil in thin layers. During rill erosion, small concentrated flow paths are created. “These paths create a sediment source and delivery system for hillslope erosion. Areas where precipitation rates exceed soil infiltration rates are more prone to this type of erosion. During gully erosion, water flows in narrow channels during or after heavy rains or melting snow. The gullies can erode to considerable depths. Valley or stream erosion is created by water flowing alongside land. It extends downward, deepening a valley, and extending the valley into the hillside. This occurs more frequently

By identifying the sediment size at each station allows the amount of long shore drift happening at each stage of the beach to be assessed and evaluated. If the size of the rocks decrease in size closer to the harbour arm, it will help prove my hypothesis

Any rainfall increases fluvial erosion. When rain does fall, this creates ephemeral streams causing water erosion due to fast forces of water. Flash floods are possible as well creating even more erosion.

If you have ever lived in proximity to coastal areas you may have seen coastline erosion first hand. The beaches you frequent during the summer may seem to be getting smaller and smaller every year. Why does your favorite beach seem to be disappearing? Coastal erosion is to blame. The waves, wind, tides and currents all play a part in the mechanism that is coastal erosion. When water and wind batter the shoreline sediments are carried out to sea and deposited on the sea floor or at other points along the coastline. This is called an erosional coastline. This erosion may be very apparent or seem to have happened overnight when it happens due to a large storm or extremely high tide.

The aim is to identify and associate landforms, rock types and soils to the natural environment and its plants and animals and also to investigate the history of the local environment, comprising human impacts over the last 50 years. The impact of human alterations to the environment includes increased soil erosion and changes in river flows.

Extracted soil samples indicate simultaneous reduction of rainfall and occasional erosion. Both soil and sediment features show establishment of marked

Erosion is a global problem, as we have already seen (umich.edu). Globally, topsoil is eroding faster than it can be replaced over 1/3 of the world's croplands (umich.edu). In the U.S, the loss of topsoil has been estimated to cost $125B per year (umich.edu). As you might imagine, this is a very difficult calculation to perform, since topsoil production rates are so slow, the lost topsoil is essentially irreplaceable (american.edu). This has been increasing within the past for years and corporations are trying to lessen the amount of erosion but it does not seem to be working

Turbidity and nutrient levels occur within Australia’s river systems, generally coincide in Australia's river systems. A large proportion of the suspended sediment in Australian rivers results from vegetation removal, leading to gully and stream bank erosion and sheetwash. Phosphorus is overwhelmingly associated with such particulate loads (The National Land and Water Resources Audit, 2002).

This year I went on a field trip to the Conodoguinet Creek. This creek runs into the Susquehanna River and drains 500 square miles of diverse landscapes. Conodoguinet comes from an indian word meaning “a long way with many bends.” It begins near Carlisle at North Middleton Park and comes to an end in West Fairview, when it flows into the Susquehanna River. The Conodoguinet Creek is about 90 miles of bends and loops that meander throughout Cumberland Valley. When I went on this trip, I tested how fast the water was moving downstream. I also tested the creek for the acidity and eutrophication. Eutrophication is excessive richness of nutrients in a lake or other body of water, frequently due to fertilizer runoff from the

Within each zone, alterations in physical features of the landscape can blur zonation patterns (Graham & Wilcox, 2000; Stephenson & Stephenson, 1949; 1937; Lipkin, 1971; McQuaid & Branch, 1984). Additionally, between each zone there is a “fringe” zone where species from each zone can persist in small numbers before reaching their range limit (the “supralittoral fringe” and the “infralittoral fringe”) (Stephenson & Stephenson, 1949). Boulders, crevices, and tide pools all create microhabitats within the zones (Graham & Wilcox, 2000; Stephenson & Stephenson, 1949; Lartigue, 2003; Bolton & Anderson, 1990; Underwood, 2000). The presence of these features can alter the effects of abiotic factors such as light availability, salinity, and wave

Images were analyzed in GIS to identify and map features such as woody debris, rock outcroppings, shifting versus stable sand, and smooth limestone bottom.

The seepage of ground water and the overland flow of surface water runoff also contribute to the erosion of shorelines (http://www.epa.gov/OWOW/NPS/MMGI/Chapter6/ch6-4.html). The role of ground water is most important wherever permeable subsurface layers of sand are exposed in high bluffs along coastal bays. In these areas, the seepage of ground water into the waterway can cause erosion at the point of exit. The surface flow of upland runoff can also dislodge sediments through the creation of rills and gullies on the shoreline banks and bluffs (http://www.epa.gov/OWOW/NPS/MMGI/Chapter6/ch6-4.html).

The intertidal rocky shore of Caloundra Beach is inhabited by diverse range of biodiversity of animals and plants, many of which have developed high levels of adaptations throughout their existence. The very boundary of marine and terrestrial ecosystem, this environment is subjected to extremes of the physical environment such as temperature, desiccation, wave turbulence as well the ecological interactions that commonly occur in biotic communities (e.g. competition, predation). However Rocky intertidal shores are easily accessible by humans and provide an enjoyable opportunity for passive recreation and for science and environmental education as well.