Year 8 pathway
Year 8 geography, stage by stage
Five stages covering every Year 8 geography objective: tectonic hazards, weather and climate, biomes, rivers and coasts, population and regional comparison, and the map skills examiners test every year.
Year 8
Your progress
0 of 10 lessons finished · 0 of 10 Year 8 objectives secure
Every lesson has prior knowledge, key words, two learning parts, common mix-ups, marked checks and an exit quiz. All case studies and figures are written for these lessons.
Stage 1
The restless Earth
Plate boundaries, earthquakes and volcanoes — and the exam favourite: why people choose to live with the risk.
- Plates, boundaries and earthquakesUnderstand tectonic processes and hazards, including earthquakes and volcanic activityFilm4 marked checks30 min
- Volcanoes, and why people stayUnderstand how geographical processes interact to create distinctive human and physical landscapes that change over timeFilm4 marked checks30 min
Investigation: Which building shape survives the shaking?Does a wider base make a tower more likely to survive an earthquake?30 minFieldwork
What you need
- A baking tray
- A tea towel
- Building blocks, LEGO or sugar cubes
- A ruler
- Paper and pen
Fair test plan
- Change: Width of the tower's base
- Measure: Whether the tower collapses (out of three runs)
- Keep the same: Tower height, number of shakes, how hard and fast you shake
What to do
- Put the tea towel on a table and stand the baking tray on it: this is your shake table.
- Build a tower ten blocks high with a base one block wide. Measure its height.
- Slide the tray sharply side to side ten times at a steady speed, and record whether the tower fell.
- Rebuild to the same height with a base two blocks wide, then three, and repeat the same shaking each time.
- Do three runs for each base width and record how many collapsed.
What should happen: Wider bases survive more often. Spreading the load lowers the centre of mass, which is why real buildings in hazard zones use deep, wide foundations and cross-bracing.
Think about: Your shaking is never identical twice. Name one thing you did to keep it fair, and one thing you could not control.
Investigation: Runny lava or sticky lava?Does a thicker liquid flow further, or build a steeper cone?25 minFieldwork
What you need
- A tray
- A book to prop the tray
- Water
- Cooking oil
- Golden syrup or honey
- A ruler
- A timer
Fair test plan
- Change: How thick (viscous) the liquid is
- Measure: Time to reach the bottom and sideways spread in cm
- Keep the same: Slope angle, amount poured, pouring point, tray wiped clean between runs
What to do
- Prop one end of the tray on the book so it sits at a gentle, fixed slope.
- Pour one tablespoon of water at the top and time how long it takes to reach the bottom. Measure how far it spread sideways.
- Wipe the tray, then repeat with oil, then with syrup, using exactly one tablespoon each time.
- Repeat each liquid twice more and work out the mean time and mean spread.
What should happen: Runny liquids travel fast and spread wide, like the basaltic lava that builds gently sloping shield volcanoes. Thick liquids barely move, like the sticky magma that builds steep composite cones and traps gas.
Think about: Trapped gas is what makes eruptions explosive. Which of your three liquids models the more dangerous volcano?
Quiz
Stage 1 quiz: The restless Earth
4 questions from the lessons in this stage. No timer, and you can try again as many times as you like.
Stage 2
Weather, climate and living things
Weather against climate, climate graphs, change since the Ice Age, then biomes, adaptations and nutrient cycles.
- Weather, climate and the change since the Ice AgeUnderstand weather and climate, including the change in climate from the Ice Age to the presentFilm4 marked checks30 min
- Biomes, vegetation belts and ecosystemsUnderstand the key processes in biology relating to biomes, vegetation belts and ecosystemsFilm4 marked checks30 min
Investigation: Run your own weather station for a weekHow much does the weather change in one place across seven days?20 minFieldwork
What you need
- An outdoor thermometer
- A straight-sided jar or bottle as a rain gauge
- A ruler with millimetres
- A scrap of ribbon on a stick for wind direction
- A notebook
Fair test plan
- Change: The day of the week
- Measure: Temperature in °C and rainfall in mm
- Keep the same: Same time of day, same spot, thermometer always in shade
What to do
- Stand the jar in an open spot away from walls and trees, and put the thermometer in shade at the same height each day.
- At the same time every day, record the temperature, the rainfall in millimetres, the wind direction and the cloud cover in eighths.
- Empty the rain gauge after every reading.
- After seven days, draw a climate-style graph: bars for rainfall and a line for temperature on the same axes.
- Write two sentences comparing your week with the usual average for the month where you live.
What should happen: Readings jump around day to day. That is weather. Climate is the average of thousands of days like these, which is why one cold week proves nothing about climate change.
Think about: If your thermometer sat in direct sun, would your temperatures be too high or too low, and why?
Investigation: Hunting microclimates around your homeIs one side of a building really warmer than the other?35 minFieldwork
What you need
- A thermometer
- A phone timer
- A sketch map of your garden or street
- Paper and pen
Fair test plan
- Change: Where on the site you measure
- Measure: Air temperature in °C
- Keep the same: Same height, same two-minute wait, same route order every round
What to do
- Choose six spots: a sunny wall, a shaded wall, open grass, under a tree, a paved area and a sheltered corner.
- Mark all six on your sketch map.
- At each spot, hold the thermometer at waist height, wait two minutes for the reading to settle, then record it.
- Walk the same route again an hour later, and a third time in the afternoon.
- Shade your map by temperature to make a simple choropleth of your own microclimates.
What should happen: Sunny, paved and sheltered spots read warmest; shaded and vegetated spots read coolest. That is the urban heat island in miniature — dark surfaces absorb heat, plants cool the air by transpiring.
Think about: How would your map change on a cloudy day, and what does that tell you about relying on one day's fieldwork?
Quiz
Stage 2 quiz: Weather, climate and living things
4 questions from the lessons in this stage. No timer, and you can try again as many times as you like.
Stage 3
Rivers and coasts
River and coastal processes, the landforms they leave, and the winners and losers of coastal management.
- Rivers: processes and landformsUnderstand rivers, coasts and glaciation and the physical processes that give rise to landscapes, and how they change over timeFilm4 marked checks30 min
- Coasts: erosion, deposition and a changing landscapeUnderstand how geographical processes interact to create distinctive human and physical landscapes that change over timeFilm4 marked checks30 min
Investigation: Where does the rain actually go?Does water soak into grass faster than into bare soil or paving?30 minFieldwork
What you need
- A large plastic bottle with the base cut off, or an empty tin can with both ends removed
- A measuring jug
- 500 ml of water per test
- A timer
- A trowel or old spoon
Fair test plan
- Change: The surface being tested
- Measure: Time in seconds for 500 ml to soak in
- Keep the same: Same volume of water, same tube depth, tests done on the same day
What to do
- Push the open tube about 3 cm into a patch of grass so no water can escape at the sides.
- Pour in 500 ml of water and start the timer.
- Record how long it takes for the water to disappear, or the depth left after five minutes.
- Repeat on bare soil, on compacted soil you have trodden on twenty times, and on a paved slab with a tray to catch the run-off.
- Do each surface three times and work out a mean infiltration time.
What should happen: Grass drinks water fastest, compacted soil much slower, and paving not at all — it all becomes surface run-off. More impermeable surface means a shorter lag time and a higher flood peak.
Think about: Use your results to argue for one flood-management scheme a town could pay for.
Stay safe: Test away from doorsteps and drains, and dry any slippery paving afterwards.
Investigation: Rounding pebbles: attrition in a jarDoes shaking wear rock fragments rounder and smaller?25 minFieldwork
What you need
- A jar with a tight lid
- Six sugar cubes or chalk pieces (as soft 'rocks')
- Water
- Kitchen scales or a ruler
- A sieve or kitchen paper
Fair test plan
- Change: Total shaking time in minutes
- Measure: Mass or longest length of the fragments
- Keep the same: Same jar, same water volume, same shaking speed, control fragments untouched
What to do
- Weigh or measure your six fragments and sketch their shape.
- Put three in the jar with 200 ml of water. Keep the other three dry and untouched as your control.
- Shake steadily for one minute, then drain, dry, re-measure and sketch again.
- Repeat for two, four and eight minutes of total shaking, measuring after each stage.
- Plot total shaking time against mass, and describe the shape change in words.
What should happen: Fragments get smaller and noticeably rounder. This is attrition, which is why pebbles far downstream and along a beach are rounder and smaller than the angular rock upstream.
Think about: Sugar dissolves as well as breaking. Which of your two processes — solution or attrition — is doing the work?
Quiz
Stage 3 quiz: Rivers and coasts
4 questions from the lessons in this stage. No timer, and you can try again as many times as you like.
Stage 4
Population, cities and movement
Population, urbanisation and development, then a fair comparison of a region in Africa with a region in Asia.
- Population, cities and developmentUnderstand population and urbanisation, including international development and the causes and effects of migrationFilm4 marked checks30 min
- Comparing regions: Kenya's Rift Valley and India's Ganges plainUnderstand geographical similarities, differences and links between places through the study of human and physical geography of a region in Africa and a region in AsiaFilm4 marked checks35 min
Investigation: A land-use survey of your own streetHow is land used where you live, and who is it used by?40 minFieldwork
What you need
- A printed or hand-drawn street map
- A tally sheet
- Coloured pencils
- A phone for the time
Fair test plan
- Change: Location along the street (and time of day for the footfall counts)
- Measure: Number of plots in each land-use category, and people per five minutes
- Keep the same: Same categories, one category per plot, same counting points and count length
What to do
- Draw a tally sheet with categories: housing, shops, services, green space, industry, transport and empty or derelict.
- Walk one side of a chosen street with an adult, recording every building or plot in one category only.
- Walk the other side back and finish the tally.
- At two fixed points, count how many people pass in five minutes, once in the morning and once in the late afternoon.
- Colour your map by category and write a paragraph on which land use dominates and why.
What should happen: Land use is zoned rather than mixed at random, and footfall follows the shops and services rather than the housing.
Think about: Your categories forced some hard choices. Which plot was hardest to classify, and how does that affect your data?
Stay safe: Do this with an adult, stay on the pavement, and never photograph people or private homes.
Investigation: Where does your dinner come from?Which regions of the world feed your kitchen?30 minFieldwork
What you need
- Ten to fifteen food packets or fruit labels
- A world outline map
- A ruler
- Coloured pencils
Fair test plan
- Change: The food item
- Measure: Country of origin and approximate distance in km
- Keep the same: One kitchen, one day, origin taken only from the label
What to do
- Read the country of origin on every item you can find, and list them in a table.
- Mark each country on your world map and join it to the UK with a straight line.
- Use an online map's distance tool, or a scale bar, to estimate each distance in kilometres.
- Group the items by continent and work out what share came from beyond Europe.
- Write two sentences on why one item travels so far: climate, growing season, cost of labour or all three.
What should happen: Fresh produce out of season comes from a long way away. Trade links your kitchen to climates and economies across several continents.
Think about: Long distance does not always mean higher emissions. What else would you need to know to judge fairly?
Quiz
Stage 4 quiz: Population, cities and movement
4 questions from the lessons in this stage. No timer, and you can try again as many times as you like.
Stage 5
Reading the map like a geographer
Grid references, scale and relief on Ordnance Survey maps, then GIS layers and a UK–world comparison.
- Ordnance Survey maps: grid references, scale and reliefInterpret Ordnance Survey maps, including using grid references, scale, topographical and other thematic mapping, and aerial and satellite photographsFilm4 marked checks30 min
- GIS and comparing a UK area with a wider world regionUse geographical information systems (GIS) to view, analyse and interpret places and dataFilm4 marked checks30 min
Investigation: Draw a relief transect from a mapWhat does the land actually look like between two grid references?30 minFieldwork
What you need
- An Ordnance Survey map or a free online OS-style map
- A strip of paper
- A ruler
- Squared paper
- A sharp pencil
Fair test plan
- Change: Distance along the transect line
- Measure: Height above sea level in metres
- Keep the same: Same map, same scale, contour interval read consistently
What to do
- Pick two points about 4 km apart and write down each six-figure grid reference.
- Lay the paper strip between them and tick every contour line it crosses, labelling the height.
- Transfer the ticks onto squared paper: distance along the bottom, height up the side.
- Join the points to draw your cross-section, and mark on any river, road or settlement it crosses.
- Describe the relief in geographical language: steep, gentle, valley, ridge, plateau.
What should happen: Contours bunched close together become a steep slope on your section; widely spaced contours become gentle ground. Rivers sit in the low points.
Think about: Vertical scale is usually exaggerated. How does that make hills look, and why do geographers accept it?
Investigation: Ask a question with GIS layersDoes your area have enough green space within a ten-minute walk?35 minFieldwork
What you need
- A computer or tablet with a free online map
- Paper and pen
- A ruler for the scale bar
Fair test plan
- Change: The area being compared
- Measure: Number of green spaces within an 800 m radius
- Keep the same: Same radius, same definition of green space, same mapping site and zoom
What to do
- Open a free mapping site and centre it on your postcode. Note the scale bar.
- Switch between the map layer, the satellite layer and a terrain layer, and write down one thing each layer shows that the others hide.
- Use the scale bar to draw a circle roughly 800 m across your home: about a ten-minute walk.
- Count parks, playing fields and accessible woodland inside the circle, then repeat for a second area a few kilometres away.
- Present both counts in a table and write a conclusion with evidence from your map.
What should happen: Access to green space varies sharply over short distances, and layering data on one map is what makes that pattern visible.
Think about: Counting spaces ignores their size and quality. How would you improve the measure?
Quiz
Stage 5 quiz: Reading the map like a geographer
4 questions from the lessons in this stage. No timer, and you can try again as many times as you like.
Where this leads
These stages build straight into GCSE geography: tectonic and weather hazards, ecosystems, rivers and coasts, urban change and the fieldwork and skills papers.

