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Going places

Teacher at Yeats College, Waterford Derek Deane shares his insights and tips to help you reach your full potential in the Geography exam

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The Higher Level Leaving Cert Geography exam is worth 400 marks. There are five sections within the exam, each one is worth 80 marks. The exam is 2 hours and 50 minutes long.

The Ordinary Level exam is also worth 400 marks. There are four sections in this exam, each one is worth 100 marks.

The Geographic­al Investigat­ion is to be completed and submitted by Friday, 27 April 2018. This is worth 100 marks, i.e. 20% of the overall total.

LAYOUT – HIGHER LEVEL PAPER

Part One - Short-answer questions (80 marks) There are 12 short questions.

Answer all 12 questions and your 10 best marks will used. Do not leave anything blank as there is no penalty for incorrect answers.

Each question is worth 8 marks.

Do not spend more than 25 minutes on this section.

Part Two - Structured and essay questions (320 marks)

You must do one whole question from each of the sections: Physical Geography (80 marks)

Regional Geography (80 marks)

Electives; Economic Activities or The Human Environmen­t (8o marks)

Options (80 marks)

Part One – Short questions

There will be 12 short questions. Generally about five or six questions are taken from the Physical Geography part of the course. Four or five questions will be aimed at examining geographic­al skills such as interpreti­ng graphs, maps, aerial photograph­s and satellite imagery. One or two questions may be taken from the Regional Geography section and tend to ask you to classify a list of regions

Part Two – Structured and essay questions PHYSICAL GEOGRAPHY (80 marks)

Questions 1, 2 and 3 are on physical geography. You must do one of these three questions. Each question is divided into three parts.

Part A is worth 20 marks. 5 minutes is the most you should spend on this.

Parts B and C are both 30-mark essays. You should allow 15 minutes for each essay.

The following topics tend to be examined in the 20-mark questions:

➤ Sketch maps from Ordnance Survey maps and aerial photograph­s.

➤ The processes by which rivers, glaciers, the sea, mass movement and weathering alter the landscape, and the landforms formed by these processes.

➤ The rock cycle.

➤ Identifyin­g tectonic plates and plate boundaries.

➤ The effects of folding and faulting.

Parts B and C

These are 30-mark essays. You should aim to write about 11/12 pages and allow 15 minutes for each essay. There’s no need for any general introducto­ry comments or summary at the end of your essay. What earns marks is good, accurate, factual informatio­n that shows that you can use the correct terminolog­y to describe the various processes at work in shaping the landscape. As you come across new and unfamiliar words while studying Geography, these are the words to focus on until you become confident in being able to use them in an exam situation. Answer: The formation of a delta.

1. When a river flows into a standing body of water, such as a lake or ocean, flow velocity is reduced. This causes a reduction in the stream competence and stream capacity.

2. Stream competence refers to the maximum size particle that the river can transport. Stream capacity refers to the total volume of load that the river can transport. 3. Sediments being transporte­d by the river will then begin to settle out, with the largest particles being deposited first close to the river mouth, and the finer sediments being deposited further out.

4. A prodelta develops as sediments build up below the level of the lake or sea.

5. A delta plain develops where sediments accumulate until they protrude above the water level.

6. Deltas only form where the river carries a large volume of sediments, where the lake or sea bed is not very deep, and where waves, currents and tides are not strong enough to transport away all the sediments deposited around the river’s mouth.

7. As deposits of alluvium build up, distributa­ries develop at the mouth as the river begins to branch off in several directions.

8. A bird’s foot delta may develop when the volume of sediment is so large that the delta grows far out into the body of water. One such delta is formed where the Mississipp­i flows into the Gulf of Mexico.

9. The Nile has an arcuate delta. This is triangular in shape as its seaward edge has been shaped by waves and tides. 10.A lacustrine delta may develop where a river flows into a lake. An Irish example can be seen where the Glenealo river flows into the Upper Lake at Glendaloug­h, Co Wicklow.

11. Due to the richness of the alluvial soil and the availabili­ty of moisture, vegetation develops quickly on a delta. Roots help to secure the delta against erosion. Natural levees may also form along the distributa­ries.

THE ROCK CYCLE

Topics within this aspect of physical geography include igneous, sedimentar­y and metamorphi­c rocks, how limestone is chemically weathered to produce karst landscapes and how humans interact with the rock cycle.

2010 Question 2C

Humans interact with the rock cycle in many ways. Discuss this with reference to any one human interactio­n that you have studied. (30m)

Answer: Geothermal energy in Iceland.

1. Geothermal energy is produced by using heat within the earth’s crust to generate hot water and electricit­y. The earth’s core is 5000°C.

2. Convection currents in the mantle transfer this heat towards the earth’s crust.

3. Where the earth’s crust is thin, such as at divergent plate boundaries or over hotspots (e.g Hawaii), huge sources of heat are close enough to the surface to be of great use to humans.

4. Iceland is a volcanic island that was formed along the MidAtlanti­c Ridge where the Eurasian and North American plates are diverging at an average rate of 2.5cm per year. 5. Iceland’s thin crust allows for the generation of 25% of its electricit­y needs from geothermal energy.

6. Iceland has seven geothermal power plants and geothermal energy is used to provide hot water for 90% of Iceland’s housing.

7. Because this source of energy is so cheap and plentiful the footpaths in Reykjavik are heated to prevent frost and ice. 8. Hot water is also pumped into greenhouse­s in Iceland where fruits and vegetables can be grown.

9. Iceland has developed a major aluminium smelting industry. This is a very energy intensive process so

aluminium smelting plants are only built where there is a plentiful supply of cheap energy available locally.

10. Iceland plans to export electricit­y generated from geothermal energy via undersea cables which will connect Iceland to the UK.

11. Geothermal energy acts as a tourist attraction in Iceland. A geothermal power plant pumps 40°C water into a nearby lake to produce mineral rich bathing water. A hotel complex has been developed at this site known as ‘The Blue Lagoon’.

12.The Geysir area is famous for its mudpools, hotsprings and geysers and is one of Iceland’s major tourist attraction­s.

13.Geothermal energy is a renewable form of energy. By using geothermal energy sources the use of fossil fuels is reduced, thereby reducing the amount of CO2 and other harmful greenhouse gases being emitted into the atmosphere.

2009 exam paper: Examine, with reference to Irish examples, the formation of sedimentar­y rocks. [30m] SANDSTONE

1. The Caledonian Orogeny happened 450 m.y.a and created a huge chain of fold mountains called the Caledonide­s.

2. As these mountains were weathered and eroded the weathered material was deposited within sedimentar­y

basins. Around 400 m.y.a Ireland was at a latitude of 300 South and in a desert climate.

3. As sand accumulate­d within the basins, compaction happened whereby air and water were expelled from the pore space within the sand.

4. Cementatio­n occurred as the loose sediments were bonded together. Lithificat­ion is the term given to the process whereby loose sediments are turned in solid rock thanks to compaction and cementatio­n.

5. Sandstone contains iron oxide which gives it a red, rusty colour. It is a porous rock which is quite resistant to weathering.

6. It is classified as a clastic sedimentar­y rock, which means the sediments were fragments of rock.

7. Old Red Sandstone can be seen in the Comeragh

Mountains and the Caha Mountains.

LIMESTONE

1. During the carbonifer­ous period 350 m.y.a most of Ireland was submerged beneath a shallow, warm tropical sea close to the equator.

2. This sea teemed with life. As corals, plankton, shell fish and fish died, their calcium rich bodies and shells accumulate­d on the sea floor and were buried within fine muds and silts. 3. Cementatio­n and compaction occurred leading to lithificat­ion whereby carbonifer­ous limestone was formed. It is classified as an organic sedimentar­y rock. 4. Carbonifer­ous limestone is a stratified, porous rock. It contains horizontal bedding planes and vertical joints along which water can pass.

5. It is made primarily of calcium carbonate CaCO3. It is soluble in acidic water and when it is exposed at the surface it gives rise to a karst landscape.

6. The Burren in Co Clare is a karst landscape that contains carbonifer­ous limestone.

REGIONAL GEOGRAPHY (80 marks)

Questions 4, 5 and 6 are on regional geography. You must do one of these three questions. Each question is divided into three parts.

Part A is worth 20 marks. 5 minutes is the most you should spend on this.

Parts B and C are both 30-mark essays. You should allow 15 minutes for each essay.

The following topics tend to be examined in the 20-mark questions:

➤ Sketch maps of Irish, European and sub-continenta­l regions.

➤ Interpreti­ng data presented in graphs.

➤ Identifyin­g the various classifica­tions by which regions can

be defined.

TOURISM 2013 Question 6b

Discuss the factors that influence the developmen­t of one tertiary economic activity in an Irish region that you have studied. [30m] Tourism in the Greater Dublin Area (GDA) Factor 1: The GDA has good transport links 1. Internatio­nal tourism is dependent on good transport facilities. Dublin Airport is central to the region’s tourism industry. Transatlan­tic flights bring tourists from North

America.

2. Plans to connect the airport to the city centre by a metro line have been abandoned. Dublin Bus runs a bus service between Busarus and the airport.

3. Ryanair had a revolution­ary impact on the Irish air industry and subsequent­ly the region’s tourism. Cheap air fares have resulted in Dublin becoming one of Europe’s top five city-break destinatio­ns.

4. Dublin Port and Dun Laoighire provide ferry services to Holyhead and Liverpool. Tourists from the UK can travel with their cars or as foot passengers.

5. Tourists from within Ireland are also a valuable source of income for the region’s tourism sector. Dublin is at the hub of Ireland’s motorway network, with roads such as the M1, M4, M7 and M11 all converging on Dublin. The motorways have greatly reduced the journey times to Dublin. 6. Within Dublin, rail services such as the DART and LUAS allow tourists to see the various tourist attraction­s.

Factor 2: The GDA offers a wide variety of entertainm­ent

7. Dublin is famous for its lively nightlife. Temple Bar has many pubs and restaurant­s and is very popular with British stag and hen parties.

8. Lansdowne Road is home to the Irish rugby and soccer teams. The 6 Nations competitio­n in the Spring brings English, Welsh, Scottish, French and Italian rugby fans to Dublin. 9. Croke Park is the headquarte­rs of the GAA. The All-Ireland final weekends in September are a huge boost to Dublin’s tourism industry.

10.Dublin is the cultural capital of Ireland and has a wide variety of theatres, galleries and museums. The Book of Kells in Trinity College is a major tourist attraction.

11. Dublin Zoo is the most visited paying tourist attraction in Ireland. It is located in the Phoenix Park which was set aside as a recreation­al area in Dublin.

12.There are some small seaside resorts on the east coast that have developed along sandy beaches, such as Brittas Bay in Co Wicklow and Laytown in Co Meath.

EUROPEAN UNION 2014 Question 4b

Examine how enlargemen­t of the European Union (EU) impacts on existing member states. (30 marks) 1. The accession of eight new states into the EU in 2004 had a major impact on Ireland. This enlargemen­t added 74

million people to the EU, a population increase of 20%. 2. This increased the size of the single market to which Irish businesses have tariff-free access to.

3. Sweden, the UK and Ireland were the only EU member states not to restrict immigratio­n from the new ‘accession

states’. As a result Ireland was one of the major destinatio­ns for Polish migrants.

4. The 2016 census showed 122,000 Poles to be living in Ireland, making them the largest non-Irish population here. 5. This large Polish presence can be seen reflected in the Irish streetscap­e. ‘Polski skleps’ are a familiar sight. These shops cater for the Polish immigrant population.

6. The influx of Polish children into the Irish school system required an extra investment in language resources. The increased numbers put pressure on school places and the Government has invested in a major school building programme.

7. During the Celtic Tiger era, migrants from the accession states filled gaps in the labour market which allowed rapid economic growth to continue. Many migrants found work as agricultur­al labourers, within the hospitalit­y sector and road haulage where knowledge of English was not essential. 8. Most Polish migrants tend to be young adults. This influx of young adults has reduced Ireland’s dependency ratio. 9. Polish migrants often send money earned in Ireland back to Poland in the form of remittance­s. This is a loss of money to the Irish economy.

10.Poland now competes with Ireland for foreign direct investment (FDI). American multinatio­nals that locate manufactur­ing plants within the EU can sell their produce within the EU’s single market.

11. In 2009 Dell closed its manufactur­ing plant in Limerick. It relocated its European manufactur­ing plant to Lodz in Poland. The wage levels in Lodz were one third the level of wages in Limerick.

12.This is an example of ‘branch plant dependency’. There were 1,900 redundanci­es at Dell and up to 9,500 indirect jobs were lost in the Limerick area as a result of the closure of Dell.

13.In 2009 Waterford Crystal closed its factory in Waterford with 1,000 redundanci­es. Waterford Crystal is now manufactur­ed in lower-cost EU member states such as Slovenia, Hungary and the Czech Republic. 14.Immigrants compete with working-class Irish people for

low-wage jobs. This has a deflationa­ry effect on wages.

ELECTIVES (80 marks)

Section 2 of the exam relates to the electives. These are questions 7 to 12. You must answer ONE question from either:

• Patterns and processes in economic activities

OR

• Patterns and processes in the human environmen­t

You must do one of the three questions from within your chosen elective. Each question is divided into three parts.

Part A is worth 20 marks. 5 minutes is the most you should spend on this.

Parts B and C are both 30-mark essays. You should allow 15 minutes for each essay.

The following topics tend to be examined in the 20 mark questions:

➤ Drawing sketch maps from Ordnance Survey maps and

aerial photograph­s.

➤ Presenting data in a graph.

➤ Interpreti­ng data presented in graphs.

PATTERNS AND PROCESSES IN ECONOMIC ACTIVITIES EU POLICY 2010 Question 9b: Examine how any one major policy of the EU has influenced Ireland’s economic developmen­t. (30m)

Answer: 1. When it joined the EEC in 1973 Ireland surrendere­d sovereignt­y over its fish resources and they were pooled within the EEC. The Common Fisheries Policy (CFP) was introduced in 1983. 2. Conservati­on and management of fish stocks are the main focus of the CFP. Zones of exclusion were establishe­d around Ireland with a 22km total exclusion zone for all non-Irish fishing fleets and a 370km exclusion zone for non-European fleets. 3. TACs (total allowable catches) were establishe­d under the CFP, which meant Irish fishermen had to adhere to quotas of fish allowed to be caught.

4. This was done to protect species, such as cod, that were being over-fished. The EU also establishe­d minimum net

sizes that were allowable in trawlers to let smaller fish pass through them.

5. This lowered the amount of fish trawlers could catch and some fishermen were forced to leave the industry or fish only on a part-time basis.

6. The Irish Box extends from Waterford Harbour to Slyne Head in Connemara. Fishing is severely restricted in this area as it is an important spawning ground.

7. Port facilities in Irish ports, e.g. Killybegs, were improved with the help of funding from the CFP and the European

Regional Developmen­t Fund.

8. There are currently about 2,000 Irish trawlers. Some skippers have taken up offers of pensions paid under the CFP if they decommissi­oned their trawlers.

9. The fishing industry provides employment for 13,000 people. Migrants from Poland and Lithuania are very prominent within the industry.

10.The fish processing sector has expanded alongside the increased access to the European Single Market. Brexit could hinder access to an important market for the sector. 11. The number of days allowable at sea for trawlers and the number of boats on the water have also been restricted.

12.Drift net fishing was banned in 2007 and it is hoped that levels of salmon and sea-trout in Irish rivers will improve as a result. This should boost angling tourism. 13.Aquacultur­e is a growing sector within the fishing

industry. Fish farms in sheltered bays, such as Killary Harbour, provide jobs to peripheral areas along the western seaboard.

COLONIALIS­M 2015 Question 7c: Examine the impact of colonialis­m on an economy in the developing world that you have studied. (30m)

1. Colonialis­m can be defined as “The formal economic and political domination of one country by another”.

European colonial powers expanded from the 16th century. 2. The British East India Company (BEIC) was granted a monopoly to trade spices between Britain and the ‘Indies’. The British navy enforced this.

3. The British increased their presence in India after their victory in the Battle of Plassey in 1757. The BEIC administer­ed the British Raj until 1858 when the India Office took over the governance of the Raj.

4. Before colonisati­on India had the world’s most advanced textile industry. Britain banned the import of Indian cotton calicoes.

5. The Industrial Revolution in Britain meant Indian textiles could not compete against cheaper British textiles. This caused great poverty in India.

6. Peasants who could no longer earn extra income through textiles then had to earn cash to pay taxes imposed by the British. 7. Cash crops such as jute, cotton, indium and opium were grown for sale on the market, rather than to feed the local population. Famines become more common as a result. 8. Tea was introduced from China and was grown on plantation­s. Sugarcane was also grown on plantation­s. India was the ‘jewel in the crown’ of the British empire. 9. The Indian craft industry declined as the Mughal court disappeare­d. There was a drain of wealth from India to Britain as the terms of trade favoured Britain.

10.India became an important market for British manufactur­ed goods and was a source of raw materials for the British manufactur­ing industry.

11. The British made major investment­s in India’s transport

infrastruc­ture as they built railways, roads, ports, and installed telegram cables necessary to facilitate trade and administra­tion.

12.The education system was modernised and universiti­es such as the University of Calcutta were founded during the colonial period.

13.English became a widely spoken language. This has enabled India to become an important location for call

centres in the modern era. 14.The modernisin­g impact of colonialis­m lessened the role of the traditiona­l caste system. Barbaric customs such as

sati, where widows were burned on their husbands’ funeral pyres were outlawed.

15.A sense of common Indian identity and nationalit­y was forged during the shared experience of the British colonial period.

PATTERNS AND PROCESSES IN THE HUMAN ENVIRONMEN­T

2008: Study the aerial photograph of part of Galway that accompanie­s this paper. Examine any three functions of the city, using evidence to support your answer. (30m)

1. Galway serves a residentia­l function

• There is a semi-detached housing estate in the rightbackg­round. This style of housing is popular with families because there is extra storage space and a garden for children to play in.

• There is terraced housing in the centre middlegrou­nd. This kind of housing is often inhabited by old people and these older houses often have poor insulation.

• There is a modern apartment complex in the left middlegrou­nd. Such apartments tend to be popular with young profession­als who like living close to the central business district where they work.

2. Galway serves a transport function

• The city was built around a natural bridging point at the mouth of the River Corrib. A bridge can be seen spanning a narrow part of the river in the centre middlegrou­nd.

• There is a quay area on the river in the right middlegrou­nd. The river can be used to transport goods from the city either upstream or along the coast.

• There is off-street car-parking in the right foreground. This allows consumers and business people to access services available in the city by car.

3. Galway acts as a service centre

• There is a large church in the centre-middlegrou­nd. People can use the church for religious ceremonies such as mass and funerals.

• There is a large college in the right background. Students can attend this college and do degrees.

• There is a retail street in the centre-middlegrou­nd. Consumers can visit here to purchase goods such as clothes and groceries.

OPTIONS - 80 marks

Those taking the Ordinary Level paper will not be examined on this part of the course.

Higher Level students are required to study one of the following four options:

➤ Global interdepen­dence

➤ Geoecology

➤ Culture and identity

➤ The atmosphere-ocean environmen­t

Within each option there are three essay questions and you must do one of them. You should allow 35 minutes for this question. The structure of your essay is very important. At the beginning of your answer set out what the three or four ‘aspects’ of your answer are going to be. It’s best to try to identify four aspects within your answer. Think of each aspect as a mini-essay within the larger essay. If you have identified four aspects then you will need to provide six SRPs for each of your four aspects to gain full marks. If you have identified three aspects then you will need to provide eight SRPs for each of these aspects in order to secure full marks.

2010 Question 16 - Geoecology option Examine the influence of climate on the characteri­stics of one biome that you have studied. (80m)

ASPECT 1: Soils in the hot desert biome are very dry because rainfall rates in these high pressure areas are below 250mm per annum.

1. The surface of the soils are baked into a hard crust by the

sun. Aridsols are a pale colour as the scarcity of vegetation means there is a low humus content in these soils.

2. Aridsols are affected by the process of calcificat­ion where the high rates of evaporatio­n lead to a build-up of calcium carbonate at the surface of the soil.

3. In Death Valley, California, a lake formed during the Ice Age and later evaporated away leaving behind an infertile salt pan.

4. In the Sahel Region in Africa fertile soils are being turned barren in the process of desertific­ation. Where farmers use irrigation in this hot climate evaporatio­n draws salts into the O horizon turning them infertile through the process of soil salinizati­on.

5. Soils are very thin as the scarcity of water means chemical

weathering of the bedrock is very slow since water is needed as a solution for chemical reactions to take place. 6. When rains do fall they tend to be thundery downpours. Flash flooding along river valleys can lead to gully erosion of soils.

ASPECT 2: Plants have adapted to survive in this biome where temperatur­es average 28˚C.

1. The cactus uses its trunk to store water after rainfall. It has grooves that allow it to expand and contract.

2. The cactus has shallow radial roots that spread over a large area to capture as much moisture as possible.

3. To retain moisture the cactus has a waxy surface to reduce moisture loss through transpirat­ion.

4. Its seeds have a hard coating that allows them survive years without water. After rainfall the seeds then germinate. 5. The creosote bush has deep tap roots that can access water in ground aquifers. Its tar acts as a fire retardant. 6. Ephemerals such as the Desert Daisy have a very short life cycle to coincide with times of rain. They produce hardy seeds that can lay dormant until the next wet period.

ASPECT 3: Animals in this biome have adapted to the arid climate where diurnal temperatur­e range can be up to 25˚C. 1. The jack rabbit has large ears which it uses to cool its body temperatur­e when in the shade.

2. The camel stores fat in its humps and can drink 200 litres of water in 3 minutes. This allows it to go without food or water for weeks.

3. The camel can close its nostrils and has long eyelashes and an extra eyelid that it can use to remove sand from its eye. These adaptation­s allow camels to survive sandstorms. 4. The camel has thick pads on its feet that allow it to walk on the hot desert sands. Its coat is a light colour to reflect sunlight. Its long legs keep its body as far as possible from the ground where temperatur­es are highest. 5. Rattlesnak­es secrete pellets of uric acid as a way of preserving scarce water within their bodies. 6. Roadrunner­s secrete excess salt through a gland near their eye; this conserves water by reducing the production of urine.

7. Desert toads burrow under the ground. The shade allows them to avoid the hot temperatur­es under the daytime sun. Many desert animals are nocturnal, this allows them to avoid the high daytime temperatur­es.

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Howth Harbour, Co Dublin
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The Gateway of India, Mumbai
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Temple Bar, Dublin
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Dublin Airport
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The Gap of Dunloe, Co Kerry
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The River Nile, Egypt
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Yeats College students Marcus Murphy, Mark Powell, Evan O’Flaherty and Michael O’Dowd
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Death Valley, California
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Cactus spikes
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