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- 1. 1 Geography School Based Assessment (SBA) (Tourism) Candidate Name: Shemar Cunningham School: Old Harbour High School Teacher: Center#: 100088 Candidate#:100088 Territory: Jamaica
- 2. 2 Table of Content Introduction ………………………………………………….……………………………… i Aim of study …………………………………………………………………………….…… 4 Location of study area ……………………………………………………………………….. 5 Methodology ……………………………………………………………………………........ 6 Presentation of data ……………………………………………………………………….. 7-15 Conclusion ………………………………………………………………………………….. 16-17 Bibliography …………………………………………………………………………….….. 18 Appendix …………………………………………………………………………………….19
- 3. 3 Introduction Tourism is travel for recreation, leisure, religious, family or business purposes, usually for a limited duration. Tourism is commonly associated with international travel, but may also refer to another place within the same country. Tourism has become a popular global leisure activity, it as both incoming and outgoing implications on a countries balance of payments. Today Tourism is a major source of income (foreign exchange) for many countries mainly in the Caribbean. St Ann is one of the largest parishes in Jamaica. It is situated on the north coast of the island, in the county of middleSex, St Ann is also known to be the Garden Parish of Jamaica, on a count of its natural beauty. The major economic activity in the parish is tourism. St. Ann is also one of the major tourist destinations given that it as popular beaches, numerous hotel and resorts (including Sandals), cruise ship dock (maritime) on the west shore of the Ocho Rios. Therefore in this research a survey was carried out so to collect statistical data that will state the necessary information on the major factors affecting the development of tourism in Ocho Rios St Ann.
- 4. 4 Aim of study What are the major factors that help to contribute to the development of tourism in Ochi Rios, St Ann? ``
- 5. 5 Location of study area The parish is located at latitude 18°12'N, longitude 77°28'W. It is bordered on the south by Clarendon and St Catherine in the east by Saint Mary, and Trelawney, in the west. Its north coast is washed by the Caribbean Sea. St. Ann covers an area of 1,212.6 km², making it the largest parish, before Saint Elizabeth's 1,212.4 km².
- 6. 6 Methodology This research was carried out using quantitative research which is research carried out by means issuing questionnaires to collect primary data. The location chosen to conduct the research was Ochi Rios which is located in the parish of St Ann. We were placed in groups of four (4) and diverted into different locations within the area, the questionnaires were issued to people randomly in order to achieve the different views and suggestions from tourists, store owners, vendors and locals. |Secondary information was retrieved from the internet and textbooks to support the primary data collected.
- 7. 7 Representation of data A total of 25 persons were questioned and only 22 were willing to answer. Therefore after data was collected, tallied and recorded it was presented and analyzed.
- 8. 8 0% 10% 20% 30% 40% 50% 60% Factors Location Physical Features Cultural Heritage Hospitality
- 9. 9 Question 1: What are some of the factors that led to Ochi Rios becoming a tourist resort area? Figure 1 shows the factors that help to contribute to Ochi Rios being a tourist resort. Fifty percent (50%) said that the location or accessibility contributed to them coming to Ocho Rios as Sangster’s International airport is relatively near. Also Sandals all inclusive hotels pull tourists there due to affordable packages. 20% say Physical features because of the exotic white sandy beaches, luxurious hotels and magnificent views as the parish is also known as the garden parish. 15% say cultural heritage so to learn more about the area’s history, food and tradition. Finally 15% say hospitality which is offered by hotels and other attractions.
- 10. 10 45% 14% 21% 20% Strongly Agree Strongly Disagree Agree Disagree 0% 5% 10% 15% 20% 25% 30% 35% 40% 45% 50% PIE CHART PIE CHART Figure #2
- 11. 11 Question # 4: There is a high level of tourist harassment in the area. Figure #2 In the bar graph shown above, tourist harassment has been prevalent, however 45% of tourists including residents strongly agree and 21% agree to this matter because residents in and around the area who are jobless try to make a living by forcefully selling food, clothes, their bodies even drugs, to tourists. There are reports from the largest cruise ship company in the world (Carnival cruise) that tourists has been harassed, however to avoid losing their customers they will be relocating the business from Ochi Rios to Falmouth. The tourism minister Dr. Wykehm McNeil states in parliament that while the country aggressively competes for tourists to help grow the economy and create jobs, harassment is threatening to drive them away. “If our visitors don’ t enjoy the Jamaica harass free as they want then very soon there will be a decline in business and arrivals at our ports, however all evidence indicate that control of harassment will lead to an increase in arrivals and businesses.”
- 12. 12 No 36% Yes 64% Does Physical Environment contribute to the growth of torism? Question #8: Does the physical environment contribute to the growth of tourism in the area? Figure #3
- 13. 13 Figure #3 shows the responses on question 8 does the physical environment contribute to the growth of tourism. In the pie chart above it shows that 64% of the respondent that say that the physical environment contribute to the growth of tourism in the the area because the physical environment (beaches, rives, Mountains) is considered to be the pull factors (features that drives people to a location). While 36% of the people said NO due to the poor maintenance of roads, and water which is the most critical natural resource. The tourism industry generally overuses water resources for hotels, swimming pools, golf courses and personal use of water by tourists. This can result in water shortages and degradation of water supplies generating a greater volume of waste water.
- 14. 14 Question 11.Does the local population contributes to the development of tourism in the area? Figure #4 39% 61% Does the population contribute to tourism development?
- 15. 15 Figure #4 shows whether or not does the population in Ocho Rios contribute to tourism development in the area. 61% of the persons who were questioned agreed mainly because not all people in and around the area is qualified, due to a poor family background, where academics is concerned, so in order to make a living they organize their own businesses big or small and sell items that will attract people especially tourists. While 39% said no, because people like those try to persuade or force tourist to buy their goods causing majority of them to refrain from touring the area and stay in there hotels within the vicinity or on cruise ship. If this act becomes prevalent it will eventually cause a decrease in in economic growth and also fewer tourists would want to visit the area due to fear.
- 16. 16 Conclusion What are the major factors that help to contribute to the development of tourism in Ochi Rios, St Ann? Ocho Rios back in the days was once a fishing village, it was also known to be a small town before it became a resort area, now Ochi Rios is known as a developing area due to the fact that its location is made accessible to tourists because the airport (Sir Donald Sangster International Airport) is in close proximity to the town, which is approximately 30 minutes’ drive, While on the way to the town of Ochi you first have to go through Fern Gully where a number of wildlife features (Eco-system) such as: animals, insects, birds are indigenous to Jamaica. The physical environment has a lot to do with the development and growth of the area because of the wonderful hotels, the major cruise ship dock located in the area (which most tourists use as a means of traveling to the island e.g.: Carnival Cruise) its coast line which is made attractive due to its beautiful corals, Beaches (formed by constructive waves that build up features) due to Long Shore Drift, Head Lands and Bays, mountains which consists of dense Mangrove Forests and also majestic Sand Spits. The population also contributes to the development of tourism in the area because not all of the residents is academically qualified, so in order to make a living they organize and develop their own businesses namely: shopping malls (this provides shoppers with various different kinds of out fits based on our Jamaican culture), art galleries (which show cases Jamaican historical Features), and food (Restaurants which provide luscious Jamaican dishes).
- 17. 17 The island reached an historic milestone when it welcomed its 2 million stopover visitors in December, surpassing the 1.986 million arrivals recorded in 2012. This represents more than a 0.7 per cent increase in arrivals for the year. Figures on the industry’s overall performance during 2013, indicate that Jamaica is recorded close to US $2 billion in earnings that year. Jamaica’s tourism industry recorded several landmark achievements during 2013, in terms of earnings, visitor arrivals, new markets tapped, and linkages and partnerships forged with new cruise and airlines, making the year one of the most successful in recent times.
- 18. 18 Bibliography Books: Bleasdell S. et al.: CSEC New Integrated Geography. Caribbean educational, published, 2008 Guinness, P.et al.: Geography for CSEC Nelson Thornes Ltb, 2008. Websites: https://www.google.com.jm/search?q=development+of+tourism+in+ocho+rios&spell=1&sa Date: 1/03/2015 http://google.www.pollution.com Date: 14/02/2015 http://google.www.jamaica-observer-tourism.com Date: 17/02/2015
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GEOGRAPHY SBA GUIDELINES. EACH ITEM 1 2 3 etc. TO BEGIN ON A NEW PAGE 1. COVER PAGE – with your own design and the title of your project You may include.
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What Processes Have Affected the Features on the Stretch of Coastline at Archer’s Bay, St. Lucy, Barbados? Name: Shawana Harris School: Harrison College Candidate Number: 00300141645 Table of Contents Page * Aim of Study......................................................................3 * Location of Study .............................................................4 * Methodology ...................................................................6 * Presentation of Data and Analysis...................................7 * Conclusion...................................................................... 16 * Bibliography ...................................................................17 * Appendix ........................................................................18 Aim of Study This study aims to examine what processes have affected the features on the stretch of the coastline at Archer’s Bay, St. Lucy, Barbados. Location of Study Fig 1 A Sketch Map of Barbados Fig 1.2 A Sketch Map of Archer’s Bay St. Lucy Fig 2 A Sketch Map of Archer’s Bay St. Lucy Barbados Methodology: Methodology On Wednesday, 5th November, 2014, a group of geography students from Harrison College visited Archer’s Bay, St. Lucy Barbados to study the influence of wave action on the visited coastal landforms. The data was collected between 10:00 am and1:30pm.The used equipment were : a ruler, a compass, a protractor, a stopwatch, a camera, tape measure, clinometers, ranging poles pencils, a sketchpad and sample bags. To begin with, field sketch maps were drawn using a sketch pad and pencil and photographs were taken of Archer’s Bay using a camera. Next, data was collected to construct a beach profile. Using the ruler, ranging pole, protractor and compass, information for a beach cross section was collected. Using two one-metre poles, a compass and a measuring tool of over 50 feet a beach cross-section was done. The two poles were stuck into the sand parallel to each other and eight feet apart. The compass measurement of the second pole from the first pole was taken. Next, sediment analysis was done. Sand samples were collected and observed in sample bags along the transect, to establish the most common grain size and composition .The angularity of pebbles were also measured by sampling along the beach profile. After which the coastal features surrounding Archer’s Bay were observed and described. Next the waves were observed and the wave data was collected. A particular section in sea was observed and the amount of waves that passed by that section were counted with the time which began at 11: 34 am and ended at 11:44 with intervals of every two minutes. Finally weather conditions were taken. Presentation of Data and Analysis Archer’s Bay is a bay and is located in Saint Lucy, Barbados. The estimate terrain elevation above sea level is 41 metres. Its Latitude is said to be 13°19'0.01 and its Longitude: -59°37'59.99. A bay is a body of water partially enclosed by land but with a wide mouth, affording access to the sea. Waves contain energy which may cause material to erode, transport it to a different place and deposit it there to build a new landform. Waves alter landforms through transport, deposition and erosion. Wave action describes the behaviour of waves. Waves can either be construction or destructive. Constructive waves act to build up the beach, this occurs when more sediment sand is deposited on the beach and less of it is removed with the receding waves. Destructive waves are the opposite of constructive wave. This is when more sediment is removed than is deposited onto the beach. Also, there is the wave frequency which describes the number of waves that pass a fixed place in a given amount of time and is one way to define how fast a wave moves. The waves at Archer’s Bay St. Lucy were moderately choppy are fairly ordered. When the bay waves are compared to headland waves, headland waves are more destructive than bay waves. The bay waves are bunched closer together and higher while the headland waves are further apart. Time | Number of Waves | 11:34am | 9 | 11: 36 am | 7 | 11:38 am | 7 | 11:40 am | 7 | 11:42am | 6 | Average 10 mins | 7 | Fig 3 A Table Showing the Wave Frequency –Number of Waves every 2 Min The wave height is estimated to be 1- 1 ½ m above the surface of the sea. Constructive waves were found to be in the bay and destructive waves beyond by the headlands. Additionally, when waves break at frequencies less than 10 per minute they are considered constructive and these waves are also able to break without interference from oncoming waves, so the swash is able to deposit material and build the beach. The weather conditions for Wednesday, 5th November 2014 were mostly sunny. Sunrise was at 6:15 am and sunset was 5:30 pm. The barometer readings were 9-1027 Mb and 3- 1009mb. The wind were said to be blowing at 26km/h while the maximum temperature was 30.4 ℃ and minimum temperature was 25.6 ℃. Hide tide occurred at 2:27 am & 2:27 pm and Low tide was at 8:12 am & 8:53 pm. Breeze was light and gentle. The Beaufort scale number was 2-3 (4-12km/hr). Beach Profile Fig 4 A Graph Showing the Characteristics of the Cross Section The sand is coarse. Most of sediment is eroded limestone. Pebbles were found to be small and well rounded. A high energy wave action seems to be present as suggested by high attrition level in the sea. Sediment Fig 5 Showing students doing sediment analysis Landforms The Bay The areas where soft rock is eroded away, next to the headland are called bays. The bay on Archer’s bay has a v-shape and is located between two headlands-East and West. Due to deposition of the sand, a beach can be found in the middle. Though Archer’s bay is small area, many landforms can be found at this site. These are: a bay, a stack, a cliff, a notch, a wave-cut platform, miniature arch, a headland, a beach and a cave. Fig 6 Showing the Bay area at Archer’s Bay A Stack Stacks (tall rock columns) are formed by the erosion of an arch. When the arch becomes so big that it can support its top it will collapse leaving a headland on one side and a stack on the other. Three stacks may be found at the Archer’s Bay St.Lucy Barbados site. Two on the East with wave cut platforms and one on the west with 2 stomps. Fig 7 Showing a Stack in the Water at Archer’s Bay A Cliff- Cliffs are formed by erosion and weathering. There is a vertical cliff to the East with a notch at its base due to the erosion (hydraulic action) which is approximate 20 m tall. A horizontal cliff is located to the West. It appeared to be once a cave which formed a cliff as a result of the roof falling in. In figure 8 the cliff is shown. Fig 8 Showing a nearby Cliff at Archer’s Bay Miniature Arch A sea arch is a natural opening eroded out of a cliff face by marine processes. If a cave is formed in a headland, it may eventually break through forming an arch. A miniature arch is located on Westside of the bay on the headland. Little erosion has occurred. Fig 9 Showing the miniature cliff at Archer’s Bay Headland Headlands are formed when sea attacks a section of coast with alternating bands of hard and soft rock. Soft bands erode more quickly than more resistant rock leaving a section of land jutting out into the sea i.e. a headland. Three headlands may be found at Archer’s Bay St.Lucy Barbados. There they are formed on either side of the water course. Fig 10 Showing the Headland at Archer’s Bay St.Lucy Barbados in the distance Beach The beach at Archer’s bay is a sandy one. From the appearance of the beach it can be determined that carbonation has affected the soft limestone from the back due to the water course. The deposition and waves are also found to be constructive. Fig 11 Showing the Beach at Archer’s Bay St.Lucy Cave Caves are formed by the dissolution of limestone as well as weathering and erosion. Hydraulic action is a predominant process. Caves occur when waves force their way into cracks in the cliff face. The cave at Archers Bay St.Lucy has collapsed off the headland. It was initially a cave but has eroded and the ceiling collapsed, now forming a cliff. A Notch A notch is located at the bottom of the cliff. This could be a possible result of hydraulic action and abrasion. Hydraulic action is the force of the water itself acting on the bed and banks where as abrasion is the process by which stones, sand and other particles are carried and thrown against the bed and bank to help erode them. Wave-Cut Platform This is formed when destructive waves crash against the cliff face cause undercutting high and low water marks mainly as a result of corrosion and hydraulic power. As seen in figure 12, a small wave cut platform on the East side of the bay. It is located at the bottom of the notch. Fig 12 Showing the Wave Cut Platform at Archer’s Bay Weathering Action Weathering is the break down but not the removal of rocks. Carbonation is seen at the Archer’s Bay St.Lucy Barbados. When carbon dioxide in the atmosphere is combined with rain water, it makes a weak acid called carbonic acid which infiltrates the soil then carbonic acid reacts with the limestone to form calcium bicarbonate which is insoluble and is then washed away. Evidence of Biotic Weathering is also evident at archer’s bay. Biotic weathering is caused by molluscs and plant roots extend downward deep into rock cracks in search of water and nutrients. When the rocks were observed, roots can be seen in the cracks and joints. This widens the joints creating a water path allowing carbonation. In addition hermit crabs and mollusc’ were found on the rocks. Such creatures may cause damage to the rock surfaces. Plants roots penetrating rocks Fig 13 Showing biotic weathering at the Archer’s Bay site Relief and Drainage The presence of limestone proves that uplift has occurred because limestone is formed underwater. Therefore in order for it to be seen it has to be lifted out of the sea. Uplift causes a change in sea level and this may influence the relief in the St.Lucy area. The water course flows downward toward the bay and drains toward the North. Mass Wasting: Rock fall Mass wasting is the movement down slope of rock fragments and soil under the influence of gravity. Evidence of mass wasting on the St. Lucy site was evident in the cliff. Mass wasting occurred destroying the slope and thus causing the retreat of the cliff backward. Human Activity Man’s impact rate on the Little Bay area proved to be quite low. At the Archer’s Bay St.Lucy Barbados site a stair case was built for easier access to the beach. Littering levels were very low. In addition the bay may be used for recreational purposes such as picnicking .Trees were possibly planted for shade and Bricks were found in the watercourse. A plastic bottle Fig 14 showing an example of litter found on the beach Conclusion From careful observation of Archer’s Bay St.Lucy Barbados, many processes such as carbonation, weathering and mass wasting have affected the features on the stretch of the coastline. The cliff eroded, forming caves, arches and other landforms. The formation process of the landforms commences, when the sea water attacks minute cracks in a headland and widen them. The cracks gradually become larger and transform into a small cave. An arch is formed when the cave wears through the headland. Further erosion results in the arch collapsing, leaving a stack which is a pillar of hard rock standing away from the coast. Eventually the stack will collapse due to further erosion leaving a stump. There was still a constructive type environment. Additionally, the waves in the bay were constructive. Destructive waves occur during storms. There was also hardly any human activity and man’s impact was rated to be moderate because though there was no litter a staircase was built for easier access and trees were planted. Sand particles were coarse but round. Alot of attrition occurred in the sea suggesting a high wave energy action in the area. The weather was mostly sunny and there was a light breeze. All in all, we discovered that there are many different processes which have affected the features on the stretch of the Archer’s Bay coastline and they all play a very important part in the formation of beaches, bays and the many different coastal landforms. Bibliography Books Bunnett B.R., Physical Geography in Diagrams, Carlong Publishers (Caribbean) Limitied, 1965 - Thursday, 13th November, 2014 Wilson M., The Caribbean Environment for CXC Geography, Oxford University Press, 1997 - Monday, 17th November, 2014 Internet Sources Google Maps, https://www.google.com/maps/@37.0625,-95.677068,4z –Wednesday, 12th November, 2014
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