Counterurbanisation

Slope land five was a relatively low, tight shore with some gradual descent and two gross breaks in slope. After measuring the slope use the clinometer and ranging poles our over all told slope of the b secern was 2.4 degrees. DIAGRAM marge We mensurable the width of the land using our measuring videotape and ranging poles and calculated it to be 130 metres. Beach cusps were in profit present which are shoreline formations made up of an commixture of grades of deposition in an arc pattern. The horns are made up of coarser materials and the embayment contains all the finer grain sediment. This beach was a wide, precise lightly sloping beach. We noted that it ran from the seaward edge of the shank regulate to the surf zone and exhibited breaker zones. Because of all these characteristics we were able-bodied to draw that it was a dissipative beach. DIAGRAM BEACH CUSPS Tides & Waves At the metre of the discover there was a low tide and the ver tex of the tides was 0.4 metres at 12.27pm. This information was obtained from Blackboard but can also be found on the Irish Times website. We indeed rear about trying to identify the wave token. at that name was a long wavelength and a low crest which ran light up the slope of the beach. These waves deposited material up the slope of the beach most likely because the strength of the swash exceeded that of the backwash. From these characteristics we identified the type of waves present on this beach were spilling waves. Longshore Current Longshore genuine is a current caused by wave action and sets parallel to the shore. We measured this by throwing an orange into the sea. We watched this for 3 minutes and measured that it move 25 metres during this time. It moved in an easterly direction in a zigzag fashion.If you want to get a encompassing essay, order it on our website: OrderEssay.net

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