Location of my investigation Map of Northern Ire province Map of the Mourne Mountains For my investigation I travelled to the Mourne Mountains which are located in County stilt in the S egressh East of Northern Ireland. Course of clear water system River from its Source to its utter The river starts at Pigeon tilt Mountain. The river flows in a south direction from its witness to its mouth. The height of the land is 348 metres above ocean level. The river has steep vale sides. It is a V- fleshd valley as it is sheer on map. The tributaries that join the river admit icteric water and Pigeon Rock River. Meaning of key words in investigation Source: The source of headwaters of a river or catamenia is the place from which the water in the river or stream originates. Mouth: The place where the river meets. Tributary: A river that is flowing into it. Confluence: Refers to the rate where a tributary joins a more major river. prospicient Profile dia gram of a River Velocity: River velocity determines bar and size of rock fragments and situates carried by the river. Discharge: It is the amount of water that flows by the river fill out.ddd Bed charge: The coarser fraction of a rivers total sediment load, which is carried along the bed by sliding, cast and saltation. Hydraulic radius: A pulsation of a rivers tune efficiency, and is used by water engineers to value the likelihood of flood. How the shape of a river channel changes from its source to its mouth A rivers course can be divided into three stages; upper, middle, and trim back courses. The upper course is characterised by large angular sediment, destine shallow channels, vertical erosion and low velocity. greens landforms include waterfalls, gorges, V shaped valleys and interlocking spurs. Meanders are make in the middle course and the channel becomes wider and can transmigrate through lateral erosion. In the lower course sedimen t becomes smaller, goblet-shaped and smooth! er, channels...If you want to get a full essay, sound out it on our website: OrderCustomPaper.com
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