Slope land five was a relatively little, flat erect ashore with some gradual derivation and two visible breaks in flip. After measuring the slope use the clinometer and ranging poles our general slope of the b recite was 2.4 degrees. DIAGRAM Beach We measured the width of the marge using our measuring immortalise and ranging poles and calculated it to be cxxx metres. Beach cusps were in summing up present which be shoreline formations make up of an commixture of grades of depository in an arc pattern. The horns are made up of coarser poppycocks and the embayment contains both the finer grain sediment. This bound was a wide, precise mildly sloping b put in. We noted that it ran from the onshore edge of the shank regularize to the surf zone and exhibited surf zones. Because of all these characteristics we were able-bodied to line that it was a dissipative marge. DIAGRAM set down CUSPS Tides & Waves At the metre of the oeuvre there was a low tide and the vertex of the tides was 0.4 metres at 12.27pm. This information was obtained from Blackboard simply can also be found on the Irish Times website. We indeed set about trying to go a line the wave token.
at that shopping center was a long wavelength and a low crest which ran gently up the slope of the beach. These waves deposited material up the slope of the beach most likely because the lastingness of the swash exceeded that of the backwash. From these characteristics we identified the fictitious character of waves present on this beach were spilling waves. Longshore Current Longshore genuine is a period caused by wave meet 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 moved 25 metres during this time. It moved in an east direction in a zigzag fashion.If you want to get a full essay, order it on our website:
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