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Pathways and Stores of Water, Sediment and Nutrients in Northwest England Catchments - Coursework Example

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"Pathways and Stores of Water, Sediment and Nutrients in Northwest England Catchments" paper discusses the water pathways from typical northwest England catchments and its flow to the sea. Pathways refer to the routes of flow traveled by water, nutrients as they move from the uplands to the coast…
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Pathways and Stores of Water, Sediment and Nutrients in Northwest England Catchments
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Extract of sample "Pathways and Stores of Water, Sediment and Nutrients in Northwest England Catchments"

Download file to see previous pages In some cases, the water gets stored temporarily in reservoirs, most of the time moving at various speeds. Depending on the speed of movement, the water collects, transports, and deposits objects including soil, rocks, and wood. Using these objects, the water at high speed can create new features as the objects brush against other objects in the water path. Water also dissolves nutrients and minerals while suspending tiny particles which are later deposited as sediments at lower speeds. 

Pathways: In the context of this essay, pathways refer to the routes of flow traveled by water, nutrients, and sediments as they move from the uplands to the coast. It includes the various runoff and underground routes they follow for them to complete their cycles.

Sediments: These are materials broken down by the processes of erosion and weathering and are subsequently transported through the actions of wind and liquid water and glaziers. These materials are naturally occurring.

The pathway of water in any particular region typically begins with the hydrological cycle. At the beginning of this cycle, water is changed from liquid into its gaseous, vapor, which ascends to the higher altitudes. Here, it is cooled and falls down as rain, which falls either directly into the various rivers, lakes and man-made reservoirs or flows into them as surface runoff. Vegetation is important in making this water to sip into the ground from where they flow as underground water till they join rivers, lakes or man-made reservoirs.
In typical northwest England catchments, the water moves along various pathways. These include fast ways for example overland flow or drain flow, shallow sub-surface flow and slower pathways. The slower pathways include flows through the deeper strata of rock and regolith. Whichever the type of flow, all the water ends in the various North West England rivers, lakes, and man-made reservoirs, and these form the main stores of water. ...Download file to see next pagesRead More
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