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' outlook Name: Nathaniel J. Adiah Candidate turning: bow: Geography School: video display College Chaguanas Year of run: Teacher’s Name: coach: To identify, describe and beak for the features of eroding and affidavit on Las Cuevas quest. Candidate Name: Candidate Number: Subject: Geography School: Year of Exam: Teacher’s Name: Aim: To identify, describe and account for the features of erosion and deposition along Las Cuevas verbalize. Contents Aim:4 Methodology5Introduction:6 Description of the Bay7 Presentation of findings †depth psychology and Discussion8 Caves9 Arches10 Stumps11 Cliffs12 Blowholes13 Geos14 Headlands15 Coves16 Notches17 The coast18 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 9:00 am †1:30 pm How? : The class was demote into six groups and each group analyz e a specific site along the shore.Each group carried out a estimate of tests: wave height, using a thou stick; wave absolute frequency, using a stopwatch; width of the bound, using a measuring tape. Introduction: Las Cuevas Bay is a 2. 2 kilometer raise brim named after the caves that lie on the south end of the margin. Las Cuevas Bay is located just about 7 kilometers east of Maracas Bay along the North Coast Road. This beach is exceedingly popular for both bathing and camping. The beach was chosen because of the fact that it has a component 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 head beach with a horse shoe shape. At the time of the study rain was go and there was a gentle breeze. It was during ut about tide. The beach gradient was gentle and uniform. The waves were inferential (8 waves per minute). Presentation of findings †Analysis and Discussion demote graph 1: showing the numeral of each feature seen on the beach The bar graph above shows that the most prevalent feature on the beach was the cliffs. Most of the features observed were seen at the east end of the beach. CavesA cave is a inwrought underground hollow in the rock, normally large enough for a forgiving being to enter. The solution of carbonate rocks much(prenominal) as limestone takes place mostly on a lower floor the wet table in the district of saturation or the phreatic zone. The water table sinks as the rocks are fade out and caves are create. Arches Stumps Cliffs Sea cliffs are formed when waves strike vigorously against a center coast. Blowholes Geos Headlands Coves Notches The Beach The beach is the sole(prenominal) depositional feature. get out graph 1: wave frequency at different points along the beachErosional Features| Depositional Features| Caves| Beach| Cliffs| | Geos| | Headlands| | Coves| | Blowhole| | Notches| | Stumps| | Arches| | Conclusion A reck on of features were observed although the beach is now raised so present processes have no great effect on each features except the beach. Las Cuevas Beach is a electrostatic 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) heave Bibliography\r\n'