Grade by Grade
B. Physical Geography and Physical Processes in Canada · Canada's Physical Environment: Landforms, Climate, Hazards and People

Human Activities That Change Natural Processes

B2.2 A1.5 A2.3About 70 minutes
Learning goals
  • I can explain how urban development, wetland drainage, dams, agriculture, forestry and mining change physical processes in Canada.
  • I can read a storm hydrograph and explain why cities flood more quickly.
  • I can calculate how much more runoff a paved surface produces than a natural one.
  • I can describe examples from my local region and from elsewhere in Canada of people changing natural events and phenomena.

Words to know

impervious surface
A hard surface such as pavement or a roof that water cannot soak into.
storm hydrograph
A graph showing how a stream's flow changes after a rainstorm.
peak flow
The highest flow of a stream after a storm.
lag time
The time between the heaviest rain and the peak flow in the stream.
urban heat island
A city area that is warmer than the countryside around it because pavement and buildings absorb and hold heat.
wetland
Land covered by shallow water for at least part of the year, such as a marsh, swamp, bog or fen.
reservoir
An artificial lake created behind a dam.
channelization
Straightening, deepening or lining a stream with concrete to move water away faster.
eutrophication
Over-fertilization of a lake by nutrients such as phosphorus, causing large algae blooms.
green infrastructure
Natural or nature-like features (wetlands, rain gardens, green roofs, trees) used to manage water and heat.

A lake that came back

Until the 1920s, Sumas Lake lay in the Fraser Valley east of Vancouver, a large, shallow lake that rose and fell with the seasons and was central to the lives of the Semá:th (Sumas) First Nation. In the 1920s, the lake was drained with dikes, canals and pumps to create farmland. In November 2021, an atmospheric river brought days of heavy rain, a dike was breached, and water poured back into the old lake bed. For a while, the lake was back.

The story shows something important: people change natural processes, and nature often pushes back. Expectation B2.2 asks you to explain how human activities alter physical processes and affect natural events and phenomena in Canada, including in your local region.

1. Cities change the water cycle

When forests and fields are replaced by roofs, roads and parking lots, the land becomes impervious. Rain cannot soak in, so:

  • More water runs off, and it runs off faster, through gutters and storm sewers into streams.
  • Streams rise higher and sooner after storms, causing flash floods and erosion of stream banks.
  • Less water infiltrates, so groundwater is recharged less, and small streams may run low in dry weather.
  • Many city streams were buried in pipes or channelized with concrete. In Toronto, for example, Garrison Creek and many other creeks now flow in underground sewers.

Cities also change local climate: dark pavement and buildings absorb heat, creating urban heat islands that can be several degrees warmer than the countryside, especially at night. Severe rainstorms that overwhelm city drains, such as one that flooded roads, basements and parts of the subway system in Toronto in July 2013, show how urban design affects flood risk.

Natural ground coverevaporation and transpiration 40%infiltration 50%runoff 10%75–100% pavedevap. 30%infilt. 15%runoff 55%Where rain goes (approximate, from a widely used U.S. EPA diagram; real values vary).
Where rain goes on natural land and on heavily paved land (approximate values). Paving the ground turns much of the water that used to soak in into fast runoff.
rainstormcity (lots of pavement):higher, faster peakforest or farmland:lower, later peaktime after rain begins (hours) →stream flow →Storm hydrographs for two similar streams. Schematic shapes, not real data.
A storm hydrograph compares how two streams respond to the same storm (schematic shapes). The city stream peaks higher and sooner because water rushes off pavement; the forest stream rises slowly because rain soaks in first.
Worked example

Worked example: How much more runoff from a parking lot?

A storm drops 30 mm of rain on 1 hectare (10 000 m²) of land. Using the approximate values above (natural land: 10% runoff; heavily paved: 55% runoff), how much runoff comes from each? How many times more is it?

  1. Volume of rain: 30 mm = 0.03 m; 0.03 m × 10 000 m² = 300 m³ of water (300 000 litres).
  2. Natural land: 10% of 300 m³ = 30 m³ of runoff.
  3. Paved land: 55% of 300 m³ = 165 m³ of runoff.
  4. Compare: 165 ÷ 30 = 5.5.

The paved hectare sends about 165 m³ of water into the storm sewers, about 5.5 times as much as natural land (30 m³). Multiply that by a whole city and you can see why urban streams flood.

2. Draining and filling wetlands

Wetlands act like sponges: they store flood water, release it slowly, filter pollutants and provide habitat. In southern Ontario, more than 70% of the original wetlands have been drained or filled, mostly for farming and development. Losing them means faster runoff, bigger floods, more erosion and poorer water quality. Sumas Lake is a dramatic example of what can happen when the land's natural storage is removed.

3. Dams and reservoirs

Dams provide hydroelectricity, water supply and flood control, but they change rivers:

  • Upstream, a reservoir floods land, forests and sometimes communities and traditional territories.
  • Sediment settles in the reservoir, so the river downstream carries less sediment and can erode its bed and banks.
  • Flows are controlled, so natural spring floods become smaller. On the Peace River, after the W.A.C. Bennett Dam was built in B.C. in the 1960s, people downstream, including the Mikisew Cree First Nation and Athabasca Chipewyan First Nation, raised concerns that the Peace–Athabasca Delta was flooding less often and drying out.
  • Dams block fish migration unless fish ladders or other passages are built.
reservoir floods land upstreamsediment settles heredamdownstream: less sediment,controlled flow, smaller spring floodsEffects of a dam on a river (side view). Schematic, not to scale.
How a dam changes a river (schematic side view, not to scale). The reservoir traps sediment and floods land; downstream, flows are controlled and natural floods shrink.

4. Farming, forestry and mining

  • Farming: ploughing exposes soil to wind and water erosion. Tile drainage (pipes under fields) moves water off land faster. Fertilizer and manure can wash into lakes: excess phosphorus, much of it from farmland runoff, feeds large algae blooms in the western basin of Lake Erie (eutrophication).
  • Forestry: clear-cutting removes trees that intercept rain and hold soil, which can increase runoff, erosion and landslides on steep slopes. Decades of putting out nearly every forest fire allowed fuel to build up in some forests, which can make later fires more intense.
  • Mining and oil sands: removing rock, soil and forest reshapes the land; tailings ponds and waste rock must be managed so they do not pollute water. Companies are required to reclaim land, but restoring a working ecosystem takes a long time.

5. Changing the atmosphere

Burning fossil fuels adds greenhouse gases that are warming the climate, which changes almost every physical process in Canada: permafrost, sea ice, glaciers, wildfire seasons and heavy rain. That is the subject of the next lesson.

Your local region

In southern Ontario, look for: suburbs growing onto farmland and the Oak Ridges Moraine (which stores groundwater), streams in concrete channels, storm ponds in new subdivisions, and green infrastructure such as rain gardens, permeable pavement, green roofs and restored wetlands designed to slow water down again. Your local conservation authority tracks how land use changes affect your watershed.

Hands-on activity

The infiltration test

You need: a measuring cup, water, a timer, a notebook, and three outdoor surfaces near home (for example, lawn, garden soil, driveway or sidewalk). Ask a grown-up before pouring water on any surface.

  1. On each surface, pour 250 mL of water slowly from about 5 cm high in the same way.
  2. Time how long until the water disappears into the surface, or note where it runs off and how far it travels.
  3. Record your results in a table: surface, time to soak in, did it run off? how far?
  4. Rank the surfaces from most to least infiltration.
  5. Explain: If a developer paved all of the lawn and garden on your street, what would happen during a big storm? Suggest one green-infrastructure fix.

What to look for: soil and lawn soak up water (garden soil fastest if loose); pavement makes the water run off almost immediately. The fix could be a rain garden, a rain barrel on a downspout, permeable pavers or planting trees.

Just for fun

Pavement is the world's worst sponge. It has exactly one job in a rainstorm, and it flatly refuses to do it.

Your turn

1

What is an impervious surface? Give two examples.

2

On a storm hydrograph, how does an urban stream differ from a forest stream?

3

Why do wetlands reduce flooding?

4

Give two ways a dam changes a river.

5

What is causing large algae blooms in Lake Erie?

6

What is an urban heat island?

7

Explain how draining Sumas Lake connects to the 2021 flood.

More practice: warm-up

1

What is lag time on a hydrograph?

2

Roughly what share of southern Ontario's original wetlands has been lost?

3

What is a reservoir?

4

Name one example of green infrastructure.

5

What is channelization?

More practice: on your own

1

A 20 mm rainfall falls on a 2-hectare shopping plaza (55% runoff). How much runoff is produced in cubic metres?

2

Why can channelizing a stream reduce flooding in one place but increase it downstream?

3

Explain how decades of fire suppression can change the natural fire process in some forests.

4

Why might First Nations downstream from a large dam have a different perspective on it than people who use its electricity?

5

How can tile drainage on farms affect both floods and water quality?

Challenge

1

A town plans a new subdivision on 50 hectares of farmland. Using the 10% (natural) and 55% (paved) runoff values, how much extra runoff would a 40 mm storm produce? Suggest two ways to reduce it.

2

Explain why the 2021 Sumas Prairie flood can be seen as both a natural event and a human-influenced one.

3

Choose an example from your own local region of a human activity that alters a physical process. Describe the change, its effects and one response.

Check your understanding

Quiz

1.

Compared with a forest stream, an urban stream after a storm usually has:

2.

Which change would increase infiltration?

3.

Sumas Lake in B.C. was:

4.

Dams usually cause rivers downstream to carry:

5.

Large algae blooms in Lake Erie are mainly linked to:

6.

30 mm of rain falls on 1 hectare (10 000 m²). How much water is that?

For parents and teachers

Big idea: B2.2 asks students to explain how human activities alter physical processes and affect natural events in Canada, including their local region. This lesson covers urbanization, wetlands, dams, farming, forestry and mining, with calculations to make the effects concrete.

Common difficulties:

  • Unit conversions. Remind your teen that 1 ha = 10 000 m², 1 mm = 0.001 m, and 1 m³ = 1000 L.
  • Reading hydrographs. Higher peak = more water at once; earlier peak = water arrives faster.
  • Seeing only harm. Many changes bring real benefits (food, power, homes); geographers weigh benefits and costs.

How to help: Walk your neighbourhood after a rainstorm. Where does the water go? Find storm drains, ditches, storm ponds or rain gardens. Look up your local conservation authority's watershed report card together.