- A.They travel quickly through the Earth's interior, compressing and expanding the crust in the direction of travel.
- B.They are surface waves that cause horizontal, side-to-side displacement, often causing severe damage to building foundations.
- C.They are longitudinal body waves that propagate through both the solid mantle and the liquid outer core.
- D.They are surface waves that roll along the ground like an ocean wave, moving the ground primarily up and down.
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Thinka Jun 2022 Pearson Edexcel AS Level-Style Mock — Geography (8GE0)
Paper 1 Section A (Tectonic Processes and Hazards)
An extinct volcanic seamount is located \(360\text{ km}\) from the active hotspot. Radiometric dating indicates the seamount is \(4.5\text{ million years}\) old.
Calculate the average rate of movement of the Pacific Plate in centimeters per year (\text{cm/yr}). Show your working.
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\(360 \text{ km} \times 1,000 \text{ m/km} \times 100 \text{ cm/m} = 36,000,000 \text{ cm}\)
Step 2: Convert the age of the seamount into years.
\(4.5 \text{ million years} = 4,500,000 \text{ years}\)
Step 3: Calculate the rate of movement.
\(\text{Rate} = \frac{\text{Distance}}{\text{Time}} = \frac{36,000,000 \text{ cm}}{4,500,000 \text{ years}} = 8 \text{ cm/yr}\)
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- e.g., converting \(360 \text{ km}\) to \(36,000,000 \text{ cm}\) OR setting up \(\frac{360 \times 10^5}{4.5 \times 10^6}\).
Award 1 mark for the correct final answer:
- \(8\) (or \(8 \text{ cm/yr}\)).
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- **Speed of Onset:** If a profile shows an extremely rapid onset (such as a major earthquake), early warning is rarely viable. Governments will therefore focus preparation on long-term structural resilience, such as enforcing strict seismic building regulations, to prevent building collapse.
- **Spatial Predictability:** Highly predictable hazards (like volcanic eruptions at known plate margins) allow governments to implement precise land-use zoning, keeping permanent settlements out of high-risk valleys.
- **Areal Extent:** A hazard with a very large areal extent (like a major tsunami) alerts governments that regional or national coordination will be necessary, helping them plan evacuation routes and scale emergency relief supplies appropriately.
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Award 1 mark for explaining a specific preparation strategy linked to this characteristic (1).
Award 1 mark for linking this preparation strategy directly to improved hazard management or reduced vulnerability (1).
**Example 3-mark response:**
If a hazard profile indicates high spatial predictability (1), governments can create precise hazard maps to establish land-use zoning laws (1), which prevents critical infrastructure from being built in high-risk zones and reduces economic losses (1).
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1. **Seabed Detection**: A bottom pressure recorder (BPR) anchored to the ocean floor continuously monitors water pressure. As a tsunami wave passes over, the increased mass of the water column causes a distinct pressure spike that is detected by the BPR.
2. **Acoustic Transmission**: The seabed recorder transmits this pressure data using acoustic telemetry (sound waves) through the water to a moored surface buoy.
3. **Satellite Relay**: The surface buoy receives the acoustic signals and immediately relays this real-time data via communication satellites to national and international monitoring stations (such as the Pacific Tsunami Warning Center).
4. **Public Warning**: Experts at warning centers analyze the real-time data to verify the tsunami, forecast its arrival times and wave heights, and issue evacuation warnings to at-risk coastal populations before the waves make landfall.
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- Award 1 mark for explaining that seabed sensors (bottom pressure recorders) detect changes in water column pressure caused by the passing tsunami wave (1).
- Award 1 mark for explaining that the pressure data is transmitted acoustically (using sound waves) from the seafloor up to a surface buoy (1).
- Award 1 mark for explaining that the surface buoy relays this real-time data via satellite to monitoring/warning centers (1).
- Award 1 mark for explaining that warning centers use the data to model the tsunami and issue timely evacuation warnings to coastal communities (1).
Do not credit responses that only mention earthquake seismographs without explaining the water-column detection process.
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1. **Introduction**:
- Define key terms: vulnerability (the susceptibility of a community to the impacts of a hazard) and development (economic, social, and political progress, often measured by HDI or GDP per capita).
- Outline the thesis: While a country's level of development is a primary determinant of vulnerability (by shaping capacity to cope, quality of governance, and infrastructure resilience), physical characteristics of the tectonic event (magnitude, location, and depth) can occasionally override human preparation.
2. **Arguments supporting the role of development (Human Factors)**:
- **Infrastructure and Mitigation**: Developed countries can invest in earthquake-resistant engineering (e.g., base isolators and dampers in Tokyo, Japan) and strict building codes, which minimize structural collapse. Developing countries often suffer from rapid, unregulated urbanization (e.g., Port-au-Prince, Haiti, in 2010) where substandard housing leads to high mortality.
- **Governance and Planning**: Wealthier nations have robust disaster management agencies (e.g., FEMA in the USA, or Japan's early warning systems). In contrast, poor governance, corruption, and lack of resources in developing nations mean emergency services are ill-equipped and search-and-rescue is delayed.
- **Social and Economic Recovery**: High-income countries have insurance penetration and financial reserves to rebuild quickly, whereas low-income countries face long-term economic regression and dependency on international aid.
3. **Arguments highlighting other factors (Physical Factors / Hazard Profile)**:
- **Magnitude and Intensity**: Extremely high-magnitude events can overwhelm even the most prepared, highly developed nations. For example, the 2011 Tohoku earthquake and tsunami in Japan ( M_w 9.0 ) caused over 15,000 deaths and led to the Fukushima nuclear crisis despite Japan's world-class defense systems.
- **Type of Hazard**: Secondary hazards such as tsunamis, lahars, and landslides are difficult to mitigate completely. A coastal location near a subduction zone inherently increases vulnerability regardless of wealth.
- **Location and Depth**: Shallow-focus earthquakes occurring directly beneath densely populated developed cities (e.g., Christchurch, New Zealand, in 2011) can cause disproportionately high localized damage compared to deep-focus events in rural developing regions.
4. **Conclusion**:
- Summarize the main points. Conclude that while physical factors determine the raw hazard potential, a country's level of development is the critical filter that determines whether a tectonic event becomes a manageable disaster or a catastrophic humanitarian crisis. Thus, development determines vulnerability to a very large extent, but nature's extremes can occasionally bypass human defenses.
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**Level 1 (1-4 marks)**:
- Demonstrates isolated or limited knowledge of tectonic hazards, vulnerability, and development (AO1).
- Offers a superficial assessment with little or no connection between development levels and vulnerability. Assertions are unsupported by case study evidence (AO2).
- Communication is basic with frequent geographical or grammatical errors.
**Level 2 (5-8 marks)**:
- Demonstrates good geographical knowledge and understanding of how development (infrastructure, governance) and physical hazard profiles influence vulnerability (AO1).
- Applies this knowledge to assess the extent to which development determines vulnerability, using some relevant case studies (e.g., comparing Haiti 2010 and Japan 2011/Christchurch 2011) to show contrasting impacts. The argument is balanced but may overemphasize one side (AO2).
- Structure is logical, and geographical terminology is used appropriately.
**Level 3 (9-12 marks)**:
- Demonstrates detailed, comprehensive, and precise knowledge of tectonic hazards, vulnerability concepts (e.g., the pressure and release model), and development indicators (AO1).
- Provides a sophisticated, balanced, and evaluative assessment of the extent to which development determines vulnerability compared to physical factors (magnitude, depth, secondary hazards). Fully supported with detailed, well-integrated case study evidence (AO2).
- Formulates a clear, logical, and substantiated conclusion. Writing is highly structured, fluent, and uses precise geographical terminology.
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1. **Introduction**:
- Define key terms: vulnerability (the susceptibility of a community to the impacts of a hazard) and development (economic, social, and political progress, often measured by HDI or GDP per capita).
- Outline the thesis: While a country's level of development is a primary determinant of vulnerability (by shaping capacity to cope, quality of governance, and infrastructure resilience), physical characteristics of the tectonic event (magnitude, location, and depth) can occasionally override human preparation.
2. **Arguments supporting the role of development (Human Factors)**:
- **Infrastructure and Mitigation**: Developed countries can invest in earthquake-resistant engineering (e.g., base isolators and dampers in Tokyo, Japan) and strict building codes, which minimize structural collapse. Developing countries often suffer from rapid, unregulated urbanization (e.g., Port-au-Prince, Haiti, in 2010) where substandard housing leads to high mortality.
- **Governance and Planning**: Wealthier nations have robust disaster management agencies (e.g., FEMA in the USA, or Japan's early warning systems). In contrast, poor governance, corruption, and lack of resources in developing nations mean emergency services are ill-equipped and search-and-rescue is delayed.
- **Social and Economic Recovery**: High-income countries have insurance penetration and financial reserves to rebuild quickly, whereas low-income countries face long-term economic regression and dependency on international aid.
3. **Arguments highlighting other factors (Physical Factors / Hazard Profile)**:
- **Magnitude and Intensity**: Extremely high-magnitude events can overwhelm even the most prepared, highly developed nations. For example, the 2011 Tohoku earthquake and tsunami in Japan (magnitude 9.0) caused over 15,000 deaths and led to the Fukushima nuclear crisis despite Japan's world-class defense systems.
- **Type of Hazard**: Secondary hazards such as tsunamis, lahars, and landslides are difficult to mitigate completely. A coastal location near a subduction zone inherently increases vulnerability regardless of wealth.
- **Location and Depth**: Shallow-focus earthquakes occurring directly beneath densely populated developed cities (e.g., Christchurch, New Zealand, in 2011) can cause disproportionately high localized damage compared to deep-focus events in rural developing regions.
4. **Conclusion**:
- Summarize the main points. Conclude that while physical factors determine the raw hazard potential, a country's level of development is the critical filter that determines whether a tectonic event becomes a manageable disaster or a catastrophic humanitarian crisis. Thus, development determines vulnerability to a very large extent, but nature's extremes can occasionally bypass human defenses.
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**Level 1 (1-4 marks)**:
- Demonstrates isolated or limited knowledge of tectonic hazards, vulnerability, and development (AO1).
- Offers a superficial assessment with little or no connection between development levels and vulnerability. Assertions are unsupported by case study evidence (AO2).
- Communication is basic with frequent geographical or grammatical errors.
**Level 2 (5-8 marks)**:
- Demonstrates good geographical knowledge and understanding of how development (infrastructure, governance) and physical hazard profiles influence vulnerability (AO1).
- Applies this knowledge to assess the extent to which development determines vulnerability, using some relevant case studies (e.g., comparing Haiti 2010 and Japan 2011/Christchurch 2011) to show contrasting impacts. The argument is balanced but may overemphasize one side (AO2).
- Structure is logical, and geographical terminology is used appropriately.
**Level 3 (9-12 marks)**:
- Demonstrates detailed, comprehensive, and precise knowledge of tectonic hazards, vulnerability concepts (e.g., the pressure and release model), and development indicators (AO1).
- Provides a sophisticated, balanced, and evaluative assessment of the extent to which development determines vulnerability compared to physical factors (magnitude, depth, secondary hazards). Fully supported with detailed, well-integrated case study evidence (AO2).
- Formulates a clear, logical, and substantiated conclusion. Writing is highly structured, fluent, and uses precise geographical terminology.
Paper 1 Section C (Coastal Landscapes and Change)
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- Concordant
- Concordant coastline
- Concordant coast
- Pacific-type coast / Pacific type
Reject 'discordant' or 'Atlantic-type'.
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**Figure 1**
* **Location A**: Boulder clay (unconsolidated glacial till) | Mean Cliff Recession Rate: 1.8 m/yr
* **Location B**: Limestone (jointed sedimentary rock) | Mean Cliff Recession Rate: 0.1 m/yr
* **Location C**: Granite (crystalline igneous rock) | Mean Cliff Recession Rate: 0.01 m/yr
Describe the relationship between rock type (lithology) and the rate of cliff recession shown in Figure 1.
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* **Relationship identified:** Unconsolidated/weaker rock types experience significantly higher rates of recession compared to consolidated sedimentary or crystalline igneous rocks.
* **Data support:** Boulder clay (unconsolidated) has a recession rate of 1.8 m/yr, which is much higher than limestone (0.1 m/yr) and granite (0.01 m/yr).
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* Unconsolidated rock types experience higher/faster rates of cliff recession than crystalline/jointed rocks (or vice versa) (1).
Award 1 mark for supporting the trend with relevant data from Figure 1:
* For example, boulder clay has the highest rate of recession at 1.8 m/yr, while granite has the lowest rate at 0.01 m/yr (1).
**Reject:** Answers that explain *why* the relationship exists (e.g. referencing wave action or specific sub-aerial processes) as the command word is 'Describe'.
Suggest one way in which building a dam upstream on the river could affect the equilibrium of this sediment cell.
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- Award 1 mark for identifying the disruption or reduction to sediment input (e.g., sediment starvation / trapping of sand behind the dam).
- Award 1 mark for explaining the impact on the sediment budget (e.g., negative budget, outputs exceeding inputs, beach starvation).
- Award 1 mark for linking this to coastal equilibrium or landform changes (e.g., shift to dynamic disequilibrium, increased erosion, shoreline retreat).
Accept alternative valid coastal feedback loops (e.g., reduced beach width leading to increased cliff erosion as a natural response to try and re-establish sediment equilibrium).
Reject responses focusing solely on fluvial hydrology (e.g., changes to river discharge) without explicit connection to the coastal sediment cell.
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However, this hard engineering directly interfered with the regional sediment cell. The groynes trapped beach material transported by longshore drift, starving beaches further south of sediment. Consequently, at Great Cowden (further down-drift), where the policy is 'No Active Intervention' (Do Nothing), the cliffs became highly vulnerable to wave attack due to the lack of a protective beach.
This physical link led to direct socio-economic conflict. Local farmers and residents in Great Cowden witnessed accelerated erosion rates (up to 10 metres per year), resulting in the loss of agricultural land, farm buildings, and homes. This created severe conflict between the affected residents of Great Cowden and the East Riding of Yorkshire Council (the local authority), with residents demanding compensation or defense schemes and accusing the council of sacrificing their livelihoods to protect Mappleton.
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- Demonstrates isolated knowledge of coastal management or conflict.
- Lacks a specific named location or uses it purely as a label.
- Explanations are generic, descriptive, and do not connect policies to physical impacts or stakeholder tension.
Level 2 (3–4 marks):
- Demonstrates geographical knowledge and understanding of coastal management policies (AO1).
- Applies knowledge to explain how a policy in one area affects another (e.g., sediment starvation / terminal groyne syndrome) (AO2).
- Mentions a named location with some accurate details, identifying at least two conflicting stakeholders (e.g., residents vs. council).
Level 3 (5–6 marks):
- Demonstrates detailed, accurate geographical knowledge of contrasting coastal management policies in a fully integrated, named case study (AO1).
- Provides a well-structured, logical explanation of how the physical consequences of one policy (e.g., trapping sediment) directly cause negative externalities elsewhere, driving conflict between specific, well-defined stakeholders (AO2).
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Introduction
Geological structure refers to the arrangement, lithology, and structural features of rock strata (e.g., jointing, faulting, folding, and dip). It plays a crucial role in shaping the coastal morphology (the shape and form of the landscape). Concordant (parallel) and discordant (perpendicular) alignments represent the primary structural templates. However, while geology establishes the framework, marine processes (wave energy, refraction) and sub-aerial weathering are essential in executing and modifying these coastal forms.
The Influence of Geological Structure
- Discordant Coasts: Where alternating bands of hard and soft rock run perpendicular to the coastline (e.g., East Dorset/Swanage Bay). This structure directly dictates the formation of headlands and bays. The differential erosion rates of resistant lithologies (such as Portland Limestone or Chalk) versus less resistant ones (such as Wealden Clay) lead to the distinct indented morphology of discordant margins.
- Concordant Coasts: Where rock bands run parallel to the coast (e.g., the south coast of the Isle of Purbeck/Lulworth Cove). The outer barrier of resistant rock (Portland Limestone) prevents the sea from easily penetrating inland. However, where weaknesses like faults or joints are breached, the sea rapidly erodes the weaker clays behind, creating circular coves or elongated dalmatian-style concordant structures. Here, structure dictates a linear, less indented macro-morphology, broken only by specific structural weaknesses.
The Role of Marine Processes (Counter-Argument/Evaluation)
- While geological structure determines the locations of headlands and bays, marine processes actively shape them. Wave refraction is a critical dynamic process: as waves approach an irregular discordant coast, they refract (bend) around headlands, concentrating high wave energy and causing rapid erosion (forming caves, arches, stacks, and stumps). Conversely, wave energy is dissipated in bays, leading to deposition and beach formation.
- The energy of the environment (macro-tidal vs. micro-tidal, high-energy destructive vs. low-energy constructive waves) determines the rate at which geological structures are exposed and modified.
The Role of Sub-aerial Processes and Dip
- The dip of the rock strata (part of geological structure) strongly controls cliff profiles (seaward-dipping strata create loose, unstable slopes prone to mass movement, whereas landward-dipping strata produce steep, stable cliff profiles).
- Sub-aerial weathering (e.g., freeze-thaw, salt crystallization) and mass movement (e.g., rockfalls, slumping) continually alter the micro-morphology of the cliffs, independent of whether the coast is concordant or discordant.
Conclusion
In conclusion, geological structure is highly significant as it acts as the primary first-order control or 'template' for coastal morphology, creating the initial blueprint of headlands, bays, and coves. However, it cannot be considered in isolation. The actual physical shape of the coast is a dynamic, ongoing product of marine processes (particularly wave refraction) and sub-aerial weathering working upon this structural template. Therefore, geological structure is the primary structural factor, but morphology is ultimately co-determined by active geomorphological processes.
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Marking Scheme & Assessment Objectives
This question assesses both AO1 (Knowledge and understanding of geographical concepts - 4 marks) and AO2 (Application of knowledge and understanding to analyze and evaluate - 8 marks).
Level Descriptors
- Level 1 (1–3 marks): Demonstrates isolated or limited knowledge of concordant/discordant coastlines. Lacks depth in explaining geological structure or processes. Evaluation is subjective or absent.
- Level 2 (4–8 marks): Demonstrates good geographical knowledge of geological structures (lithology, alignment) and marine processes. Applies this to explain concordant (e.g., Lulworth) and discordant (e.g., Swanage) morphologies. Outlines other factors (wave refraction, sub-aerial weathering) but the assessment of 'extent' may be unbalanced or lack a firm conclusion.
- Level 3 (9–12 marks): Demonstrates detailed, accurate, and systematic geographical knowledge of structural controls (lithology, alignment, dip, faults) and dynamic processes (wave refraction, marine erosion, mass movement). Offers a balanced, well-structured assessment of the extent to which geology is the primary driver, concluding logically that geology provides the structural template while marine/sub-aerial processes act as the dynamic sculptors.
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Structure of a Strong Response:
Introduction: Define sustainable coastal management and Shoreline Management Plans (SMPs), outlining the four key strategies: Hold the Line, Advance the Line, Managed Realignment, and No Active Intervention (Do Nothing). Introduce the premise that these strategies create 'winners' and 'losers', which often breeds conflict, but state the thesis that conflict can be mitigated through proactive planning and governance.
Paragraph 1: Why conflict occurs (Socioeconomic vs. Environmental priorities): Discuss how decisions like 'Managed Realignment' or 'No Active Intervention' directly threaten residential properties, agricultural land, and local businesses (e.g., Happisburgh on the Holderness Coast or similar eroding shorelines). Highlight that local homeowners experience severe financial loss (as properties lose value and are not covered by standard insurance), causing deep frustration and conflict with local authorities and environmental bodies (e.g., the Environment Agency) who prioritize cost-benefit ratios and natural sediment cells over individual properties.
Paragraph 2: The role of Cost-Benefit Analysis (CBA) and Environmental Impact Assessments (EIA): Explain that engineering decisions are heavily guided by CBA and EIA. Areas with high economic value (large towns, critical infrastructure like gas terminals at Easington) are protected ('Hold the Line'), while sparsely populated rural areas are often abandoned ('No Active Intervention'). This disparity creates a sense of social injustice and inequality among rural communities, escalating conflict as rural stakeholders feel marginalized compared to urban ones.
Paragraph 3: Instances where conflict is minimized / Alternative viewpoints: Evaluate how sustainable schemes can reduce conflict if managed transparently. When stakeholders are integrated into the decision-making process early on, or when transitional financial support and 'roll-back' schemes are provided (such as pathfinder projects helping residents relocate), resentment is reduced. Additionally, some environmental groups (e.g., National Trust, RSPB) actively champion managed realignment because it creates valuable intertidal saltmarsh habitats, aligning their interests with sustainable governance, meaning conflict is not universal among all non-governmental organizations.
Conclusion: Summarize that while conflict is highly likely due to the zero-sum nature of coastal erosion (where protecting one area can starve another downdrift via interrupted longshore drift), it is not completely inevitable. The degree of conflict depends heavily on the governance style, the availability of compensation or relocation schemes, and the transparency of the decision-making process.
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- AO1 (6 marks): Demonstrate knowledge and understanding of coastal processes, management strategies (SMPs), and their impacts.
- AO2 (10 marks): Apply knowledge to evaluate and analyse the extent to which these policies lead to stakeholder conflict.
Level Descriptors:
- Level 1 (1–4 marks): Simple or descriptive recall of coastal protection. Lacks evaluation of conflict or stakeholders. Structure is basic.
- Level 2 (5–8 marks): Shows some understanding of SMP strategies (e.g., hold the line). Identifies some stakeholders (residents, councils) but the evaluation of 'inevitability' of conflict is superficial or one-sided.
- Level 3 (9–12 marks): Good geographical understanding of physical processes and human management decisions. Applies concepts well, showing why different options (like managed realignment) lead to conflict due to winners and losers. Well-structured argument.
- Level 4 (13–16 marks): Clear, balanced, and sophisticated evaluation of the 'inevitable' nature of conflict. Explores nuances (such as mitigation through community consultation and compensation). Reaches a logical, supported conclusion using precise geographical terminology.
Paper 2 Section A (Globalisation)
- A.The adaptation of a global product or service to fit the unique cultural, economic, or legal requirements of a local market.
- B.The process by which local cultures become dominant globally, replacing multinational corporate structures.
- C.The concentration of economic activity in major global hub cities, leading to regional disparities.
- D.The removal of trade barriers by national governments to encourage foreign direct investment from transnational corporations Ready to invest in domestic industries, lowering production costs globally..
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1. **Free-market liberalisation (deregulation):** By removing restrictive regulations on financial markets and foreign ownership (such as allowing foreign banks to operate freely), governments encourage foreign capital flows. For example, the UK's deregulation of financial markets in 1986 ('Big Bang') made London a global hub for international finance.
2. **Privatisation:** Selling state-owned assets (such as energy, water, or telecommunications companies) to private investors, often foreign TNCs. This brings in massive Foreign Direct Investment (FDI) and integrates domestic infrastructure into global corporate networks.
3. **Creation of Special Economic Zones (SEZs):** Governments can designate specific regions (like Shenzhen in China) that offer tax incentives, low tariffs, and simplified planning regulations. This attracts global manufacturing and service firms, embedding the country into international trade networks and global supply chains.
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- **Point 1 (2 marks):** 1 mark for identifying free-market liberalisation/deregulation, and 1 mark for explaining how this facilitates globalisation (e.g., by removing barriers to foreign investment and increasing capital flows).
- **Point 2 (2 marks):** 1 mark for identifying privatisation, and 1 mark for explaining how it drives globalisation (e.g., by allowing foreign TNCs to acquire public services, expanding their global footprint and investment).
- **Point 3 (2 marks):** 1 mark for identifying Special Economic Zones (SEZs) or tax incentives, and 1 mark for explaining how this connects the country to globalisation (e.g., by attracting manufacturing TNCs to set up export hubs, boosting trade flows).
*Accept other valid government policies, such as investing in transport/communications infrastructure (e.g., container ports) or joining free trade blocs, provided they are clearly linked to promoting globalisation.*
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Globalisation has accelerated rapidly since the late 20th century, driven by a combination of global financial institutions (IFIs) and national government policies. While IFIs establish the global rules and structures of trade, national governments hold the ultimate sovereign power to choose how, when, and to what extent they integrate into the global economy. This essay will assess the relative influence of both, arguing that while IFIs create the enabling environment, national government policies are the primary catalyst for local acceleration.
**The Role of Global Financial Institutions (IFIs)**
International organizations such as the World Trade Organization (WTO), the International Monetary Fund (IMF), and the World Bank have been instrumental in establishing a neo-liberal global economic model.
- The **WTO** promotes free trade by reducing barriers, tariffs, and quotas, facilitating global trade flows.
- The **IMF and World Bank** provide financial assistance to countries in economic distress, often attaching strict Structural Adjustment Programmes (SAPs). These SAPs mandate policies like privatization, deregulation of financial markets, and the opening up to foreign direct investment (FDI).
- For many developing nations in the late 20th century, these forced policy changes accelerated their integration into global networks. However, the influence of these organizations is often structural and passive; they set the conditions, but they do not actively manage local implementation.
**The Role of National Government Policies**
In contrast, national government policies are active, deliberate drivers of globalisation. Sovereignty means that national governments must ultimately decide to engage with the global economy.
- **The Open Door Policy and SEZs:** China’s 1978 'Open Door Policy' is a prime example. The national government decided to embrace globalization by establishing Special Economic Zones (SEZs) like Shenzhen, offering tax incentives and cheap labor to attract transnational corporations (TNCs). This single national decision fundamentally shifted global manufacturing networks.
- **Deregulation and Privatisation:** In the UK during the 1980s, the Thatcher government implemented financial deregulation (such as the 'Big Bang' of 1986) and privatised state industries. This transformed London into a global financial hub, accelerating financial globalisation.
- **Trade Blocs:** Governments also choose to join trade blocs (e.g., the EU or USMCA), which reduces trade friction and allows free movement of goods, services, and sometimes people, directly accelerating regional globalisation.
**Evaluation & Conclusion**
In conclusion, national government policies are more influential than global financial institutions. Although IFIs created the neo-liberal architecture that made global integration possible, it was the sovereign decisions of national governments to adopt 'open' economic policies—such as China's 1978 reforms or India's 1991 economic liberalisation—that actually triggered the rapid acceleration of globalisation. Without national willingness and targeted policies like SEZs, the structural frameworks of the IMF and WTO would remain underutilised. Therefore, national governments act as the primary engines and gatekeepers of globalisation.
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- **AO1 (4 Marks):** Demonstrate knowledge and understanding of the roles of national governments (deregulation, privatisation, SEZs, trade blocs) and global financial institutions (IMF, World Bank, WTO) in globalisation.
- **AO2 (8 Marks):** Apply knowledge and understanding to write an analytical, balanced essay assessing the relative influence of national policies versus global institutions.
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### Level Descriptors:
* **Level 1 (1–4 marks):**
* **AO1:** Demonstrates isolated or basic knowledge of globalisation drivers. Likely to name institutions or policies without detail.
* **AO2:** Assessment is generic, subjective, or heavily unbalanced. Lacks clear structure or a supported conclusion.
* **Level 2 (5–8 marks):**
* **AO1:** Demonstrates good, accurate knowledge of both national policies (e.g., China's open-door policy, SEZs, UK deregulation) and global financial institutions (WTO, IMF, World Bank).
* **AO2:** Offers a logical, structured assessment of both factors. Begins to weigh which is more influential, supported by some case study evidence. A conclusion is present but may lack depth.
* **Level 3 (9–12 marks):**
* **AO1:** Demonstrates precise, detailed, and comprehensive knowledge of the mechanisms used by both national governments and global financial institutions to accelerate globalisation.
* **AO2:** Provides a highly coherent, balanced, and sophisticated assessment. Clearly evaluates the relationship between the two (e.g., national governments as active gatekeepers vs. global institutions as structural enablers). Reaches a logical, well-supported final judgment.
Paper 2 Section C (Diverse Places)
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**Table 2: Demographic data for Ward A and Ward B**
| Ward | UK-born population | Non-UK born population | Total population | Percentage (%) of non-UK born population |
| :--- | :--- | :--- | :--- | :--- |
| **Ward A** | 12,400 | 3,600 | 16,000 | (i) .................... |
| **Ward B** | 8,550 | 5,950 | 14,500 | (ii) .................... |
Complete Table 2 by calculating the percentage of non-UK born residents for both Ward A and Ward B. State your answers to **one decimal place**. Show your working.
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\(\text{Percentage} = \left( \frac{\text{Non-UK born population}}{\text{Total population}} \right) \times 100\)
For Ward A (i):
\(\text{Percentage} = \left( \frac{3,600}{16,000} \right) \times 100 = 22.5\%\)
For Ward B (ii):
\(\text{Percentage} = \left( \frac{5,950}{14,500} \right) \times 100 = 41.034...\% \approx 41.0\%\)
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- (i) Ward A = 22.5% (Accept 22.5) (1 mark)
- (ii) Ward B = 41.0% (Accept 41% or 41.0) (1 mark)
* **Aged 18–30:** 82% feel 'safe or very safe' walking alone in the neighborhood after dark.
* **Aged over 65:** 34% feel 'safe or very safe' walking alone in the neighborhood after dark.
Suggest one reason for the difference in perception of safety between the two age groups shown in Figure 3.
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To secure all 3 marks, the answer must provide a clear chain of reasoning:
1. Identify a valid source of differing perception (e.g., physical vulnerability, media influence, or lived experience of the area).
2. Develop the point by explaining how this factor specifically impacts the older generation's daily life or psychological state (e.g., fear of falling, lack of physical defense, or high consumption of local crime news).
3. Link this back to why this creates a contrast with the younger demographic group (who have higher physical resilience, different lifestyle habits, or greater confidence walking alone at night).
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**Example response:**
Older residents may experience higher levels of physical frailty or mobility issues (1 mark). This means they feel less able to defend themselves or escape quickly if a threatening situation arises at night (1 mark). Consequently, this vulnerability amplifies their fear of crime, leading to a much lower perception of safety compared to younger adults who are generally more confident in their physical resilience (1 mark).
**Alternative response:**
Older residents may spend more time consuming local news media or community social media alerts that focus heavily on local crime and anti-social behaviour (1 mark). This can disproportionately distort their view of actual threat levels, leading to heightened anxiety about being outdoors after dark (1 mark). In contrast, younger residents may be less engaged with these local media channels or have a larger network of peers active in the area, leading to a more secure perception of the same environment (1 mark).
* **Aged 18–30:** 82% feel 'safe or very safe' walking alone in the neighborhood after dark.
* **Aged over 65:** 34% feel 'safe or very safe' walking alone in the neighborhood after dark.
Suggest one reason for the difference in perception of safety between the two age groups shown in Figure 3.
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PastPaper.workedSolution
To secure all 3 marks, the answer must provide a clear chain of reasoning:
1. Identify a valid source of differing perception (e.g., physical vulnerability, media influence, or lived experience of the area).
2. Develop the point by explaining how this factor specifically impacts the older generation's daily life or psychological state (e.g., fear of falling, lack of physical defense, or high consumption of local crime news).
3. Link this back to why this creates a contrast with the younger demographic group (who have higher physical resilience, different lifestyle habits, or greater confidence walking alone at night).
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**Example response:**
Older residents may experience higher levels of physical frailty or mobility issues (1 mark). This means they feel less able to defend themselves or escape quickly if a threatening situation arises at night (1 mark). Consequently, this vulnerability amplifies their fear of crime, leading to a much lower perception of safety compared to younger adults who are generally more confident in their physical resilience (1 mark).
**Alternative response:**
Older residents may spend more time consuming local news media or community social media alerts that focus heavily on local crime and anti-social behaviour (1 mark). This can disproportionately distort their view of actual threat levels, leading to heightened anxiety about being outdoors after dark (1 mark). In contrast, younger residents may be less engaged with these local media channels or have a larger network of peers active in the area, leading to a more secure perception of the same environment (1 mark).
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1. **Income and Employment Measures**: Direct measures of economic wealth, such as average household income, salary distribution, or the percentage of the population claiming out-of-work benefits, highlight wealth gaps. Areas with high proportions of low-income or zero-hours contract workers show clear socio-economic division compared to affluent pockets.
2. **Health and Life Expectancy**: Variations in physical health, such as infant mortality rates, obesity levels, or overall life expectancy at birth, reflect differences in living standards, diet, and access to healthcare services. Significant spatial variations in life expectancy across a city (often termed the 'subway gap') demonstrate deep structural inequality.
3. **Composite Indices (e.g., Index of Multiple Deprivation - IMD)**: Rather than relying on a single metric, composite indices combine multiple domains—such as education, crime, barriers to housing, and the living environment—to calculate relative deprivation. This provides a holistic spatial view of how different neighbourhoods within a diverse place compare nationally and locally.
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- **Income/Employment (1+1 marks)**: e.g., Identifying household income/unemployment rates (1 mark) and explaining how it shows variations in purchasing power, disposable income, or job security between different groups within the place (1 mark).
- **Health/Education outcomes (1+1 marks)**: e.g., Identifying life expectancy/educational achievement levels (1 mark) and explaining how this reflects disparities in social opportunities, lifestyle, or quality of local services (1 mark).
- **Composite Indices like IMD (1+1 marks)**: e.g., Identifying the Index of Multiple Deprivation (1 mark) and explaining how combining domains like housing, crime, and environment helps map complex, multi-dimensional deprivation across small local areas (1 mark).
*Accept other valid indicators of socio-economic inequality such as housing tenure (renting vs ownership) or fuel poverty.*
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Paper 2 Section D (Unfamiliar Fieldwork - Diverse Places)
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Calculate the percentage of retail units that were classified as 'Global/International Food Outlets'. Give your answer to one decimal place.
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1. Divide the number of 'Global/International Food Outlets' by the total number of retail units surveyed:
\[\frac{18}{80} = 0.225\]
2. Multiply by 100 to convert the decimal into a percentage:
\[0.225 \times 100 = 22.5\%\]
Since the value is already at one decimal place, no further rounding is required.
Final Answer: \(22.5\%\) (or \(22.5\))
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- \(22.5\%\) (accept \(22.5\))
Reject any rounded answers such as \(23\%\).
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Explain two ways the students could improve their sampling methodology to ensure a more representative and valid set of results.
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1. **Spatial and Temporal Diversification (2 marks)**: Standing outside a specialized international supermarket on a Tuesday morning restricts the sample to specific shoppers and excludes people who work standard weekday hours. By expanding the locations to multiple neutral sites (e.g., public squares, transit stations) and varying the times (e.g., Saturday afternoon, weekday evening), they would capture a more representative cross-section of the local community.
2. **Alternative Sampling Strategy (2 marks)**: The current method relies on convenience/opportunity sampling, which introduces researcher bias (selecting friendly-looking people) and self-selection bias. Implementing a systematic sampling strategy (e.g., approaching every nth person passing a line) or stratified sampling (targeting specific age, gender, or ethnic subgroups reflecting local census data) would ensure a more balanced and statistically valid sample.
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**Improvement 1 (Max 2 marks):**
- **Identification (1 mark):** Vary the timing (e.g., weekends/evenings) or locations (e.g., high street, parks) of the survey.
- **Explanation (1 mark):** This avoids bias towards specific shopper types (international supermarket) and ensures people who are employed or at school during the day are included, making the sample more representative.
**Improvement 2 (Max 2 marks):**
- **Identification (1 mark):** Implement a systematic (e.g., every 5th person) or stratified sampling frame instead of convenience sampling.
- **Explanation (1 mark):** This minimizes researcher subjectivity when selecting participants and ensures the sample reflects the overall demographic profile of the neighborhood.
*Do not credit generic improvements that do not relate to the sampling methodology presented in the scenario (e.g., 'doing more secondary research first' or 'using a GIS mapping tool' unless tied explicitly to improving the sampling frame).*
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