Inappropriate……………………………………………………………10 Earthquakes………………………………………………………………………11 Mass Wasting (1)………………………………………………………………...12 Mass Wasting (2)………………………………………………………………...13 Stream Process…………………………………………………………………...14 Coastal Process – Headland……………………………………………………...15 Coastal Process – Sea Stack……………………………………………………...16 Free Choice –Marsh...……………………………………………………………17 Lifting Condinsation Level Topic: Atmospheric Moisture Chapter 6 Page: 147 Date:
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combination of these processes working in conjunction with each other in the vanity of the Otakamiro point headland in the Muriwai coastal environment‚ consequently resulting in the current headland morphology of a cave and arch within the headland and an offshore stack‚ Motutara island. Waver refraction is the process where waves bend around relief and cause the erosion of the headland/relief resulting in the forming and shaping of other landforms Refraction occurs when the part of a wave crest
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Presentation College Chaguanas Year of Exam: Teacher’s Name: Aim: To identify‚ describe and account for the features of erosion and deposition along Las Cuevas Bay. 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 Bay. Contents Aim: 4 Methodology 5 Introduction: 6 Description of the Bay 7
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Maracas bay. It is considered a building or constructive beach which makes it an excellent beach for bathing and nesting by the turtles. For our school based assessment‚ we choose Las Cuevas Bay (area of study) due to the dominant coastal processes (erosion‚ deposition) and the prominent coastal features (caves‚ arches‚ blowholes‚ cliffs) which seems to be changing overtime. Map of Trinidad and Tobago showing cities and coastal areas Map of study area Methodology A field trip
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Geography School Based Assessment ( S.B.A) Topic: What Are The Effects Of Wave Processes On The Coastline Of Robin’s Bay St Mary. Centre Number: 100013 Candidate Name: ********* Registration Number: Year of Examination: 2012 School: Calabar High School Teacher: ********** Territory: Jamaica Contents Topic ……………………………………………………………………………………………………………………………………………………3 Aim ………………………………………………………………………………………………………………………………………………………3 Methodology ……………………………………………………….……………………………………………………………………………
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TITLE PAGE Candidate Name: Nasia Pierre-Alexander Candidate Number: School Centre Number: 160527 Year: 2014 Subject: Geography Title: How do wave processes affect the formation of coastal features along Las Cuevas Bay‚ North Trinidad? Teacher’s Name: Mr. Deosaran Seelal Score: Table of Contents Aim/Purpose of study Location of study Map one Trinidad showing study area Map two showing Map three showing a map of Las Cuevas Bay Methodology Presentation of Data/Analysis and Discussion Discussion
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occurring at the Terrigal beach area are: * Erosion‚ which is effecting: * The Skillion‚ mainly the headland and rock platform‚ which is part of a preserved area of land known as “the Haven” which also contains the rugby oval. The man type of erosion that affects this is from the sea. * The sand dunes on the beaches. This area is affected by wind erosion as well as the tides if adequate vegetative cover is not present. The main type of erosion‚ from the sea‚ takes the sand from the sand dunes
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Waves ‚ Tides and Sediment Cells L.O. = to compare and contrast constructive & destructive waves‚ to understand wave refraction‚ to understand the difference between spring and neap tides and to identify the UK’s sediment cells. Wave Characteristics Wavelength = the distance between the crest of two adjacent waves. Wave Amplitude = the distance between sea level and the crest. Wave Crest =the highest point of the wave. Wave Trough = the lowest point of the wave. Wave Height = the distance
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many different designs; it can be used to protect a cliff from wave attack and improve slope stability and it can also dissipate wave energy on sandy coasts. Challenges /Limitations /Disadvantages However‚ a seawall may not protect a coast from erosion in the long run. As waves break against the seawall‚ the curved sea walls reflect the energy of the waves which is redirected downwards‚ to the base of the seawall‚ resulting in a strong backwash. The backwash wears away the base of the seawall‚ causing
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Spurn Point in the south‚ a distance of 61 km. The Holderness Coast is famous due to its history of being one of Europe’s fastest eroding coastlines. Essentially erosion is the process by which coastline rocks are broken up by the action of the sea and transported out to sea or along the coast by waves and the wind. Coastal erosion can occur in numerous forms: Seawater can compress air into cracks in rocks. When the air escapes it does so under pressure and shatters the rock (hydraulic action)
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