IB Geography SL study materials
IB Geography SL study resources

IB Geography SL cheat sheet

IB Geography SL · Keep the key ideas within reach.

Quick reference

Geographic Themes and Concepts

  • Space = the areal extent and distribution of phenomena; place = space given meaning by human experience, identity, or attachment (e.g., a sacred site, a home village).

  • Scale is a relational concept: a process visible at local scale (a farm) may be driven by global scale (commodity prices); analysis must state the scale of observation.

  • The seven concepts are interlinked: change in one (e.g., processes) alters others (place, sustainability); exam answers should name at least two concepts and show their linkage.

  • Systems have inputs, outputs, stores (reservoirs) and flows (fluxes); open systems exchange matter/energy across boundaries, closed systems exchange only energy (Earth as a whole is effectively closed for matter).

  • Positive feedback amplifies change (permafrost thaw releases methane, raising temperature); negative feedback dampens change (increased cloud albedo reducing insolation) and promotes equilibrium.

  • Sustainability has three interacting pillars (environmental, social, economic); a project is sustainable only if it meets present needs without reducing the capacity of future generations to meet theirs.

  • Spatial concepts for describing distribution: density, concentration, dispersion, pattern (clustered, linear, uniform) and gradient (e.g., distance decay from a city centre).

  • Change is measured as rate (amount per unit time) or as magnitude; distinguishing short-term fluctuation from long-term trend is required when interpreting any time-series graph.

Quick reference

Core: Population and Economic Development Patterns

  • Population density = total population / total land area (km²); physiological density = population / arable land area, which better indicates pressure on food-producing land.

  • The Demographic Transition Model has five stages: high stationary (high CBR and CDR), early expanding (CDR falls), late expanding (CBR falls), low stationary (both low), and declining (CBR below CDR).

  • Natural increase rate = CBR − CDR per 1,000; doubling time is approximately 70 / annual percentage growth rate (rule of 70).

  • Development is multidimensional: economic (GNI per capita, PPP), social (life expectancy, literacy, HDI), and demographic (fertility, infant mortality); HDI combines life expectancy, mean/expected years of schooling and GNI per capita.

  • Rostow's model of five stages (traditional society, preconditions for take-off, take-off, drive to maturity, high mass consumption) is a linear model criticised for assuming all countries follow the same path.

  • Core–periphery model: core regions accumulate capital and skilled labour; periphery supplies raw materials and cheap labour; the dependency school argues this relationship perpetuates inequality.

  • The Brandt line divides a wealthier 'North' from a poorer 'South', but it is a simplification: newly industrialised countries (e.g., South Korea) and oil-rich states now sit in the 'South' with high GNI per capita.

  • Population pyramids indicate stage of development: broad base and concave sides = high fertility and high mortality (stage 2); narrow base and bulging middle = ageing population (stage 4–5).

Quick reference

Core: Changing Populations

  • Push factors drive migration away (conflict, unemployment, drought); pull factors attract (jobs, safety, services); intervening obstacles (borders, cost, distance) filter the flow.

  • Ravenstein's laws: most migrants move short distances, migration is stepwise, long-distance migrants favour cities, and every migration stream produces a counter-stream.

  • Net migration = immigration − emigration; population change = natural increase + net migration.

  • Forced migration includes refugees (cross a border, protected under the 1951 Refugee Convention) and internally displaced persons (IDPs), who remain inside their own state and lack that protection.

  • Ageing populations raise the old-age dependency ratio = (population aged 65+) / (population aged 15–64) × 100, increasing pressure on pensions and health budgets.

  • Youthful populations (youth bulge) create demand for schools and jobs; if job creation lags, high unemployment can drive emigration or instability.

  • Pro-natalist policies (e.g., France's family allowances, Singapore's baby bonuses) aim to raise fertility; anti-natalist policies (e.g., China's former one-child policy, India's sterilisation campaigns) aim to reduce it.

  • Migration impacts are gendered and age-selective: sending areas lose working-age adults (brain drain) but gain remittances; receiving areas gain labour but may face housing and integration pressures.

Quick reference

Core: Global Climate Change and Its Impacts

  • The enhanced greenhouse effect: human emissions of CO₂, CH₄, N₂O and halocarbons trap outgoing long-wave radiation, adding to the natural greenhouse effect.

  • Major sources: CO₂ from fossil fuel combustion and deforestation; CH₄ from livestock, rice paddies and landfills; N₂O from fertilisers.

  • Impacts are uneven by latitude and by vulnerability: low-lying deltas and small island states face sea-level rise; the Sahel faces drought and rainfall variability; high latitudes face permafrost thaw.

  • Vulnerability = exposure + sensitivity − adaptive capacity; the same hazard produces different impacts in a wealthy and a poor region.

  • Mitigation reduces causes (renewable energy, afforestation, carbon pricing, energy efficiency); adaptation reduces harm (sea defences, drought-resistant crops, early warning systems).

  • Positive feedbacks amplify warming: ice–albedo feedback (melting ice exposes darker ocean/land, absorbing more heat) and permafrost methane release.

  • The Kyoto Protocol (1997) set binding targets for developed countries only; the Paris Agreement (2015) uses nationally determined contributions (NDCs) aiming to hold warming well below 2 °C, pursuing 1.5 °C.

  • Common but differentiated responsibilities (CBDR) is the principle that developed states should bear more of the mitigation burden, given their historical emissions.

Quick reference

Core: Resource Consumption and Security

  • Resource security exists when a reliable, affordable and environmentally acceptable supply of a resource meets demand; it has dimensions of availability, access, affordability and acceptability.

  • Energy mix = the proportion of total energy supply from each source (e.g., oil, coal, gas, nuclear, hydro, wind, solar); it differs sharply between countries.

  • The energy transition is the shift from high-carbon to low-carbon sources; it is constrained by cost, infrastructure, intermittency and political priorities.

  • Water stress occurs when demand exceeds 20% of available renewable supply; water scarcity is physical (insufficient supply) or economic (lack of infrastructure/funds to access supply).

  • Virtual water is the water embedded in a product (e.g., ~15,000 litres per kg of beef); trade in virtual water shifts pressure between regions.

  • Food security has four pillars: availability, access, utilisation (nutritional use) and stability over time; food insecurity can be chronic or transitory.

  • Malthus argued population growth outpaces food supply (geometric vs arithmetic growth); Boserup argued population pressure stimulates agricultural intensification; the Green Revolution (high-yield varieties, fertilisers, irrigation) supported the Boserup view.

  • The resource curse (paradox of plenty) describes states rich in a single resource (e.g., oil) that show slower growth, corruption or conflict due to dependence on volatile commodity prices.

Quick reference

Optional Themes: Freshwater and Oceans and Coastal Margins

  • The hydrological cycle: stores (oceans, ice, groundwater, atmosphere) and fluxes (precipitation, evaporation, transpiration, runoff, infiltration); a drainage basin is an open system.

  • A storm hydrograph shows discharge over time; a short lag time and high peak flow indicate impermeable rock, steep slopes, urbanisation or sparse vegetation; a long lag time indicates permeable rock and dense vegetation.

  • River processes: erosion (hydraulic action, abrasion, attrition, solution), transport (traction, saltation, suspension, solution), and deposition when velocity falls.

  • The long profile shows a concave-up curve from steep upper course to gentle lower course; the cross-profile changes from narrow V-shaped to wide and flat with a floodplain.

  • Coastal sediment cells are self-contained units of sediment movement bounded by headlands; a change in one part of the cell (e.g., a groyne) affects the whole cell.

  • Waves of high energy and long fetch cause destructive (plunging) waves and erosion; constructive (spilling) waves build beaches with a gentle swash and strong backwash.

  • Coastal landforms: erosional (cliffs, wave-cut platforms, headlands and bays, caves–arches–stacks) and depositional (beaches, spits, bars, tombolo, salt marsh).

  • Hard engineering (sea walls, groynes, riprap) is costly and can shift erosion downdrift; soft engineering (beach nourishment, dune stabilisation, managed retreat) works with natural processes but needs maintenance.

Quick reference

Optional Themes: Extreme Environments and Geophysical Hazards

  • Glacial systems: accumulation (snowfall) vs ablation (melting, sublimation, calving); the equilibrium line separates net accumulation from net ablation; a positive mass balance means glacier advance.

  • Glacial erosion processes: plucking (meltwater freezes around rock and pulls it away) and abrasion (rock carried in ice scours the bed); landforms include cirques, arêtes, U-shaped valleys, hanging valleys and truncated spurs.

  • Periglacial environments have permafrost and active layers; processes include freeze–thaw weathering, solifluction and patterned ground; thawing permafrost releases methane and destabilises infrastructure.

  • Deserts are defined by aridity (usually <250 mm precipitation per year); landforms include yardangs, zeugen, barchan and seif dunes, pediments and wadis.

  • Hazard risk = (hazard × vulnerability) / capacity to cope; risk is not the same as hazard magnitude.

  • Earthquake hazards: ground shaking, liquefaction (saturated sediment behaves like a fluid), landslides, tsunamis and fires; seismic risk is high where dense populations occupy unstable ground.

  • Volcanic hazards: lava flows, pyroclastic flows, ash fall, lahars (volcanic mudflows) and gases; the VEI (Volcanic Explosivity Index) rates magnitude from 0 to 8.

  • Hazard management cycle: mitigation, preparedness, response and recovery; prediction (e.g., seismic monitoring, tiltmeters, gas sampling) reduces risk but cannot prevent events.

Quick reference

Optional Themes: Leisure, Tourism and Sport and Food and Health

  • Butler's Tourism Area Life Cycle: exploration, involvement, development, consolidation, stagnation, then decline or rejuvenation.

  • Factors driving tourism growth: rising disposable income, increased leisure time, cheaper air travel (including low-cost carriers), and media/Internet promotion.

  • Mass tourism impacts: economic (foreign exchange, employment, leakage of profits abroad), sociocultural (commodification of culture, demonstration effect), environmental (footprint, water use, reef damage).

  • Ecotourism aims to minimise impact and benefit local communities; it can fail if it becomes 'greenwashing' or if visitor numbers exceed carrying capacity.

  • Sports and mega-events (Olympics, World Cup) bring infrastructure and image benefits but risk cost overruns, displacement and underused venues (white elephants).

  • The nutrition transition is the shift from traditional diets to energy-dense, processed foods, linked to rising obesity and diet-related disease (type 2 diabetes, cardiovascular disease).

  • Food security and health are linked: undernutrition (stunting, wasting) and overnutrition (obesity) can coexist in the same country (the double burden).

  • Health geography examines disease diffusion (contagious vs hierarchical), access to healthcare and the influence of environment on health outcomes (e.g., malaria in warm, wet lowlands).

Quick reference

Internal Assessment: Fieldwork and Report

  • The IA is an individual fieldwork report of about 2,500 words, structured as: fieldwork question, background/geographic context, methods, data presentation, analysis, conclusion and evaluation.

  • A good fieldwork question is specific, measurable and geographically located: it names a variable, a place and a spatial or temporal comparison (e.g., 'How does pedestrian flow vary along X street between 08:00 and 18:00?').

  • Sampling methods: random (unbiased but may miss patterns), systematic (every nth point along a transect), and stratified (sampling proportionally within subgroups); state the sample size and justification.

  • Primary data collection techniques include questionnaires, pedestrian/traffic counts, environmental quality surveys, field sketches, photographs and bipolar/rating scales; secondary data include census, GIS and meteorological records.

  • Data presentation must match data type: bar charts for discrete categories, scatter graphs for correlation, pie charts for proportions, choropleth or isoline maps for spatial distributions, and annotated field sketches.

  • Analysis should use appropriate techniques: mean, median, mode, interquartile range, Spearman's rank correlation coefficient or chi-squared; state significance and interpret the result geographically.

  • The conclusion must answer the fieldwork question directly and link findings to geographic concepts (space, place, scale, processes, change, systems, sustainability).

  • Evaluation must address limitations of methods (sampling bias, sample size, timing, weather, instrument error) and suggest specific improvements, not vague statements.