Geography Methodolgy

METHODOLOGY On Thursday May 26, 2011, an investigation into the features found at the Swift River, Portland, Jamaica, was conducted. Three stops were visited namely rely utter, cashew tree Ridge and Swift River District. Velocity was measured at cashew tree Ridge and Swift River District. The process used to measure the f number was by dividing the time taken by a fuck up to travel a set standoffishness by the distance which was 15m. The guide conducted a test known as a sediment analysis at Hope Bay and cashew Ridge. The test was done by walking around the cranial orbit of the river, and picking up random sediments. The guide determined the characteristics of the examined sediments. Sketches and photographs were drawn and taken at all stops. These were of the river and its features, both the sketches and photographs will be used to help identify features at each stop. reconditeness of the river was checked at every meter across the width of the river. Data Presentation At stop one (Hope Bay) Characteristics: Gradient of cipher degrees The lower stage of the river (rivers mouth) Width of 1.5 km Length of 2.

2 km River flowing from southernmost to north Left bank was steep and covered in vegetation proper(a) bank was a gentle slope also with vegetation ascendant rock case was sedimentary Dominant sediment shape was wholesome rounded Plate 1- Sketch viewing banks of Swift River at Hope Bay Source: Field Study 2011 Figure 1- diagram showing banks of Swift River at Hope Bay[pic] Source: Hugh Jones Pie Chart presentation results of sediment analysis done at Hope Bay [pic] Source: Jevaugn Williams Chart showing dominant rock type see at Hope Bay [pic] Source: Jevaugn Williams Figure 2- Diagram showing sediments... If you want to get a full essay, position it on our website: Orderessay

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