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nominee Name Nathaniel J. Adiah prospect Number Subject Geography School initiation College Chaguanas Year of Exam teachers Name Aim To identify, follow and account for the propertys of erosion and sediment on Las Cuevas alcove. Candidate Name Candidate Number Subject Geography School Year of Exam Teachers Name Aim To identify, describe and account for the features of erosion and deposition along Las Cuevas Bay. Contents Aim4 Methodology5Introduction6 Description of the Bay7 unveiling of findings Analysis and Discussion8 Caves9 Arches10 Stumps11 Cliffs12 Blowholes13 Geos14 Headlands15 Coves16 Notches17 The Beach18 Conclusion20 Limitations21 Bibliography22 Aim To identify, describe and account for the features of erosion and deposition along Las Cuevas Bay. Methodology Where? Las Cuevas Bay When? Monday 11th June, 2012. From 900 am 130 pm How? The class was split into six groups and each group force field a specific site along the bank.Each group carried out a number o f tests fluctuate height, using a metre stick wave frequency, using a stopwatch width of the brim, using a touchstone tape. Introduction Las Cuevas Bay is a 2. 2 kilometer raised bank named after the caves that lie on the southwestern ratiocination of the beach. Las Cuevas Bay is locate approximately 7 kilometers east of Maracas Bay along the North sliding board Road. This beach is extremely popular for both bathing and camping. The beach was elect because of the fact that it has a lot of observable features. Description of the Bay Las Cuevas Bay is approximately 2. kilometers long and its width is 74 feet. It is a bay corpus beach with a horse shoe shape. At the time of the study rain was falling and there was a gentle breeze. It was during high tide. The beach gradient was gentle and uniform. The waves were constructive (8 waves per minute). Presentation of findings Analysis and Discussion avert graph 1 showing the number of each feature seen on the beach The bar graph ab ove shows that the most prevalent feature on the beach was the cliffs. Most of the features observed were seen at the eastern end of the beach. CavesA cave is a natural underground hollow in the rock, usually large enough for a human being to enter. The solution of carbonate rocks such as limestone takes place mostly below the water put off in the zone of saturation or the phreatic zone. The water postpone sinks as the rocks are dissolved and caves are make. Arches Stumps Cliffs Sea cliffs are formed when waves strike vigorously against a steep coast. Blowholes Geos Headlands Coves Notches The Beach The beach is the whole depositional feature. Line graph 1 wave frequency at dissimilar points along the beachErosional Features Depositional Features Caves Beach Cliffs Geos Headlands Coves Blowhole Notches Stumps Arches Conclusion A number of features were observed although the beach is now raised so present processes have no great effect on any features except the beach. Las Cuevas Beach is a stable beach system with several erosional features and only one depositional feature, which is the beach itself. Limitations Some limitations on this study are 1) The weather 2) Timeframe 3) Tide Bibliography