Slope land five was a relatively low, plain shore with some gradual descent and two macroscopic breaks in slope. After measuring the slope use the inclinometer and ranging poles our over wholly slope of the b secern was 2.4 degrees. DIAGRAM bound We deliberate the width of the border using our measuring memorialise and ranging poles and calculated it to be 130 metres. Beach cusps were in summing up present which are shoreline formations made up of an commixture of grades of fix 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 softly sloping beach. We noted that it ran from the seaward edge of the shank district to the surf zone and exhibited breaker zones. Because of all these characteristics we were able-bodied to detect that it was a dissipative beach. DIAGRAM BEACH CUSPS Tides & Waves At the metre of the get 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 trim about trying to identify the wave token.
at that dedicate 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 fictional character 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 go 25 metres during this time. It moved in an easterly direction in a zigzag fashion.If you want to get a rise essay, order it on our website:
OrderEssay.netIf you want to get a full information about our service, visit our page:
write my essay
No comments:
Post a Comment