Seaside Morphology | Colin Campbell

Table of Content 1 . Aim of examine.

2 . Position of analyze


3. Way of data collection


4. Demonstration, Analysis and Discussion of info


5. Remark of results


6. Summary


7. Bibliography


Aim of Study 1 ) To study the consequences of constructive and destructive influx processes about coastal landforms development installment payments on your To determine the affect of the local rock and structure on the development of coastal landforms.

one particular

Location of Study The data was accumulated at Robins Bay St . Mary, Discovery bay, jamaica.


Approach to Data Collection The Data Was Collected about March thirtieth 2011 in Robins Bay St . Jane. Tables, along with tagged diagrams, were used to present the data.


Presentation, Analysis and Exploration of Data Marine Well Landforms: y Give y Notch y Headland

Time(s) sixty 60 sixty

Wave Data Table you Number of surf 15 sixteen 14

Period(s) 2 one particular 1

Say Frequency 12-15 12 13

Waves Desk 2 Wave Height(ft. ) 1 . a couple of 1 . eight 2 . you

Wave Length(ft. ) 5. 2 a few. 8 six. 7


Wave Action The power of waves is one of the most important forces of coastal modify. Waves are manufactured by wind blowing over the surface from the sea. Because the wind produces over the marine, friction is created - creating a swell in the water. The energy of the blowing wind causes drinking water particles to rotate within the swell which moves the wave ahead. The size and energy of the wave can be influenced simply by: y con y the length of time the wind have been blowing the strength of the wind what lengths the influx has journeyed (the fetch)

Waves can be destructive or perhaps constructive. Each time a wave fails, water is definitely washed up the beach -- this is named the swash. Then the normal water runs down again the beach -- this is referred to as the backwash. With a positive wave, the swash can be stronger than the backwash. With a destructive influx, the backwash is more powerful than the swash.

Figure one particular showing Waves Action.


Destructive Surf Destructive Surf is a plunging wave, using a short wavelength, a high rate of recurrence (13- 12-15 per minute) a high crest. Backwash significantly exceeds swash. Destructive waves comb seaside material seawards.

Figure two showing Destructive waves. This wave was present at all locations.

Positive Waves A decreased frequency (6-8 per minute) spilling trend, with a very long wavelength and a low crest, running carefully up the beach front. Swash significantly exceeding the backwash (which is decreased by percolation), leading to deposition.

Figure three or more showing Positive waves. This kind of wave was present in Don Captain christopher Cove and Peytons Cove.



Caves occur when surf force their particular way into cracks in the cliff deal with. The water contains sand and other materials that grind aside at the mountain until the splits become a give. Hydraulic action is the predominant process.


Figure four showing Cave. This landform was present at Sea Well and Peytons Cove and Level.


Level A V-shaped cut or perhaps hole in the bottom or perhaps edge of your surface, normally a cliff. This is created after repeated beating of waves, damaging, on the side of any cliff.


Figure 5 showing a notch. This landform was present at Sea well only.



Headlands are shaped when the sea attacks an area of coast with switching bands of hard and soft mountain. The groups of smooth rock, including sand and clay, go more quickly than patients of more resistant mountain, such as chalk. This leaves a section of land jutting out in the sea called a headland.


Figure 6th showing Headland. This landform was present at Ocean Well, Wear Christopher Stage and Forced Point.


Robins Bay Landforms: sumado a Stacks

Time(s) 60 62 60

Wave Data Number of Waves 12 15 13

Period(s) 1 2 1

Wave Consistency 11 13 14

Dunes Wave Height(ft. ) 1 ) 2 installment payments on your 1 1 . 9

Trend Length(ft. ) 10 being unfaithful. 3 almost 8


Bunch A collection is a geological landform that includes a steep and sometimes vertical line or articles of rock in the marine near a coast,...

Bibliography: 26