Counterurbanisation

Slope land five was a relatively low, at once shore with some gradual descent and two manifest breaks in slope. After measuring the slope use the dip circle and ranging poles our over solely slope of the b secern was 2.4 degrees. DIAGRAM strand We metric the width of the brim using our measuring magnetic tape and ranging poles and calculated it to be 130 metres. Beach cusps were in step-up present which are shoreline formations made up of an commixture of grades of sedimentation 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 mildly sloping beach. We noted that it ran from the seaward edge of the shank order to the surf zone and exhibited breaker zones. Because of all these characteristics we were able-bodied to order that it was a dissipative beach. DIAGRAM BEACH CUSPS Tides & Waves At the metre of the hire there was a low tide and the vertex 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 limit about trying to identify the wave token.

at that move 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 strength of the swash exceeded that of the backwash. From these characteristics we identified the example 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 sh ore. We measured this by throwing an orange ! into the sea. We watched this for 3 minutes and measured that it go 25 metres during this time. It moved in an easterly direction in a zigzag fashion.If you want to get a expert essay, order it on our website: BestEssayCheap.com

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