Identify the pathways and stores of water, sediment and nutrients from Essay

Identify the pathways and stores of water, sediment and nutrients from the uplands to the coast in typical northwest England - Essay Example As water flows naturally to the sea, it forms various features as it interacts with various factors on its way. 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. This paper is dedicated to discussing the water pathways from the typical northwest England catchments and its flow to the sea. 2). Definition of terms Pathways: In the context of this essay, pathways refers to the routes of flow traveled by water, nutrients and sediments as they move from the uplands to the coast. ... 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. Nutrients: These are chemicals required by organisms for them to live and grow well or a substance required for the process of metabolism and must be taken from the organism’s environment. Uplands: Refers to areas of higher altitudes Coast: Refers to a strip of land bordering the sea and as such, it is an area of low lower altitude. Catchments: Refers to a main source, the region from where a substance or material is supplied to the rest of the areas that form part of the material’s or substance pathway. 3). The pathways and stores of water, sediment and nutrients from the uplands to the coast in typical northwest England catchments a) Pathways and stores of water from the uplands to the coast in typical northwest England catchments The pathway of water i n any particular region typically begins with the hydrological cycle. At the beginning of this cycle, water is changed from liquid into its gaseous, vapour, which ascends to the higher altitudes. Here, it is cooled and falls down as rain, which falls either directly as into the various rivers, lakes and man-made reservoirs or flow into them as surface runoff. Vegetation are 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 ?ow, shallow sub-surface ?ow and slower pathways. The slower