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What is a region
concept referring to a segment of the Earth surface; it can be any size
Regional Geo
physical and human geography
Physical geo
natural environment (glaciers, geology)
Why are regions used
Simplify the study of large portions of the Earth's surface by breaking them up into manageable pieces which, because of their uniformity, allow for generalizations to be made about their geographical character
Intended to capture the personality of particular areas
How are regions defined
On the basis of features that allow us to differentiate a given region from other regions. Regions can be conceptualized based on size and on criteria
Regions based on size
Mega-regions (world regions)
Meso-regions (segments of countries)
Micro-regions (areas within a locale)
What do all regions have
Location, area, boundaries, and hierarchy
Regional Criteria
- Functional – A central place that serves the surrounding area. (Example: Pearson Airport connects people from nearby regions.)
- Formal – A region defined by shared physical or cultural characteristics. (Examples: climate, language, religion.)
- Perceptual / Vernacular – A region based on people's opinions, feelings, or how they see a place. (Example: thinking of Southern Ontario as a particular region.)
- Administrative / Political – A region defined by government boundaries. (Examples: cities, provinces, countries.)
6 Candian Regions and criteria
Atlantic Canada – fishing, economically depressed,
Quebec – language
Ontario – manufacturing
Western Canada – resource base similar, oil and pot ash, agricultural
British Columbia – physically, mountains, 10 different chains of mountains, forestry
Territorial North – climate similar, cool short summers, sparsely populated, mega-projects, economy similar
What factors cause Canada and its regions to change over time?
Culture, demography, economy, immigration, politics, and technology.
What is Canadian regionalism?
Differences between regions caused by geography, history, economy, and social, cultural, and racial makeup.
Four major faultlines (tensions) that change national unity
Centralist/Decentralist
English-speaking and french-speaking
Aboriginal and non-aboriginal
Newcomers and old-timers
Centralist/Decentralist Faultline
Conflict over how much power the federal government versus provinces should have, especially over natural resources, national interests, and provincial disputes.
English-Speaking/French-Speaking
Quebec seeks to protect its French language and culture. Conflicts include language laws, Quebec independence (1980 and 1995 referendums), Bill 21, and debates over Quebec’s future within Canada.
Aboriginal/Non-Aboriginal
Indigenous peoples have faced land and resource loss, discrimination, and limited opportunities due to colonialism. Changes to the Indian Act, the end of residential schools, and political activism led to greater opportunities and a shift toward reconciliation rather than assimilation.
Newcomers/Old-timers
Immigration brings population growth, cultural diversity, and economic benefits, but can create concerns about cultural identity, accommodating different traditions, settlement costs, and Canada's ability to support newcomers.
When was the division of power between the federal and provincial government established
British North American Act (1867)
Federal Power
defense; external affairs; criminal law; banking; trade; citizenship and Indian affairs
Provincial Power
education; health; welfare; highways; civil law; local government; natural resources.
What powers are shared between provincial and federal government
agriculture, immigration and taxation.
Sense of place
refers to two distinct but related ideas about the nature of particular locations on the Earth surface
First “Place”
The unique characteristics of a particular location (its character), which give meaning to people, even if they have never been there
Second “place”
refers to the attachments which people have to a particular location as a result of their direst experiences, memory and interaction (home)
What is nordicity, and how is it measured?
Nordicity measures how “northern” a place is. Louis-Edmond Hamelin created the Global Nordicity Index using 10 factors, including latitude, temperature, ice, precipitation, vegetation, accessibility, air service, population, and economic activity.
What is the Core-Periphery Model?
The economically powerful core (heartland) dominates the less powerful periphery (hinterland). The model explains how economic power and human activities are distributed across a region.
A regional version of the Core-Periphery Model, Friedmann’s construct divided countries into:
1. The core region – the focus of economic, political, and social activity (Ontario, Quebec)
2. The upward transitional region – a growing economy and a transition from primary to secondary and tertiary industries (BC, Western Canada)
3. The downward transitional region – characterized by a declining economy and dwindling population (Atlantic Canada)
4. The resource frontier – sparsely populated with little development (Territories)
Landforms that actively shaped and reshaped by various processes
Denudation: Wearing down the Earth's surface.
Weathering: Breaking rocks into smaller pieces.
Erosion: Moving broken-down rock and material.
Deposition: Dropping and settling transported material, often in oceans.
How are the rock cycle and plate tectonics related?
Plate tectonics moves Earth's plates, causing processes like melting, pressure, and volcanic activity that create and change rocks. These processes help drive the rock cycle, which transforms rocks between igneous, sedimentary, and metamorphic types.
Tectonic (Igneous Rocks)
No plants grow, toxic for them
Table lands – NFL
How can mountains form?
Through faulting, folding, tectonic forces, and volcanism.
What are orogenies?
Processes that build mountains through tectonic forces and rock deformation.
What processes are associated with mountain building?
Mass wasting (landslides), glaciers, and running water.
What shapes and carves mountain peaks?
Erosion wears away rock and shapes mountain peaks.
How does water contribute to rock breakdown on mountains?
Water enters cracks, freezes and expands, breaking pieces of rock off. The fallen rock fragments can form talus at the base of a slope.
physiographic region
A large area of the Earth’s crust that has three characteristics:
It extends over a large, contiguous area with similar relief features
Its landform has been shaped by a common set of geomorphic processes
It possesses a common geological structure and history
How does geology shape Canada's regions?
Different geological structures, topography, and mineral and energy resources shape regional economies and create different opportunities and challenges for human activity. Glaciation has shaped nearly all of Canada's topography.
7 physiographic regions of Canada
The Canadian Shield
The Cordillera
Mountains in the west, BC
The Interior Plains
Arctic to USA to gulf of mexico
The Hudson Bay lowlands
Upper Ontario, little bit of Quebec
Newer, from the last ice age, icesheets 2-3KM thick, all weight pushed down crust; when ice melted, water rushed in, sediments trickled down, ice rebound,
The Arctic lands
No vegitation
The Appalachian uplands
From NFL to about Georgia, same rocks on the other side of the Atlantic, worn-down rock
The Great lakes – St. Lawrence Lowlands
We are here: limestone, use to be above the ocean
The Canadian Shield
Canada's largest physiographic region, covering nearly half the country. It has ancient, rugged granite rock shaped by glaciers, which created lakes, scratches, and landforms like drumlins and eskers. It has poor agricultural potential but is rich in minerals such as nickel, copper, zinc, and gold.
The Cordillera
A region covering over 16% of Canada, stretching from southern BC to Yukon and including the Rocky Mountains. Plate tectonics formed its mountains, while glaciers shaped the landscape, creating cirques, horns, and tarns. It contains sedimentary, metamorphic, and igneous rocks and has earthquake and tsunami risks.
The Appalachian Uplands
An ancient region extending into the United States, weathered over about 500 million years. It has varied geological structures and topography, including folded and flat-lying rocks, igneous intrusions, and rocks also found in North Africa.
The Arctic Lands
Covers over 20% of Canada and includes coastal plains, plateaus, and mountains. It has permanently frozen ground (permafrost), patterned ground from freeze-thaw cycles, and pingos formed by underground ice.
The Interior Plains
A stable sedimentary plain covering nearly 20% of Canada, lying over the Canadian Shield. It was partly covered by glacial lakes, including Lake Agassiz, about 12,000 years ago. Rivers have exposed older rock layers, and sedimentary basins contain major oil and gas deposits. During the Late Cretaceous, the Western Interior Seaway covered the region, and today bedrock is covered by glacial deposits.
The Hudson Bay Lowlands
Canada's youngest physiographic region, covering about 3.5% of the country. It formed around 10,000 years ago from marine sediments exposed by isostatic rebound after the Laurentide Ice Sheet melted. It has widespread permafrost, muskeg (peat), and small human settlements.
Great Lakes — St. Lawrence Lowlands
Canada's smallest physiographic region, with surface materials from marine, river, and glacial deposits. Its favourable location makes it home to Canada's main ecumene (area of permanent human settlement) and manufacturing core. It has more varied topography than the Great Lakes Lowlands.
Climate
Describes average weather conditions for a specific place or region based on past weather over a very long period of time
Weather
The current state of the atmosphere with a focus on weather conditions that affect people living in a particular place for a relatively short period of time
Two climatic types of Canadas territory
the Arctic and Subarctic zones
Extremely long and cold winters
Climatic zone
An area of the Earth’s surface where similar weather conditions occur
Extent determined by long-term data of annual, seasonal, and daily temperatures and precipitation
4 dominat factors of Canadas climate
1. Solar energy/latitude
2. Global circulation system: winds, air masses, and ocean currents
3. Marine and continental air masses
4. “Continental effect”: air masses change temperature quickly over continental expanses
Solar energy/Latitude
The amount of radiation entering the atmosphere is a function of latitude
Low latitudes have a net surplus of energy
High latitudes have a net deficit of energy
Since Canada occupies a lot of territory, it experiences great variations in the amount of solar radiation received
Polar Ice Melting
Loss of more than 2 million square kilometers (800,000 square miles) of Arctic sea ice in last decade
Loss of ice = enhanced warming due to lower albedo (positive feedback)
Five air masses
Pacific, Atlantic, Gulf of Mexico, Southwest US, and Arctic
Global Circulation System
Redistributes heat energy from low to high latitudes through air circulation and ocean currents
Winds, air masses, and ocean currents
Warm Japan current warms the Pacific coastal waters
The cold Labrador current cools Atlantic Canada’s summer weather
Marine air masses bring mild and moist weather to adjacent land areas
Continental air masses are quite dry and vary in temperature according to the season
Precipitation
As an air mass rises, its temperature drops
Triggers condensation of water vapour within the air masses
Three types of precipitation
Convectional precipitation results when moist air is forced to rise because the ground has become particularly warm (associated with thunderstorms)
Frontal precipitation occurs when a warm air mass is forced to rise over a colder (and denser) air mass
Orographic precipitation results when an air mass is forced to rise over high mountains
As the same air mass descends along the leeward slopes of those mountains, the temp rises and precipitation is less likely to occur (rain shadow effect)
Permafrost
Relic from Pleistocene climate
Permanently frozen ground with temps at below 0 for at least 2y
Permafrost has been retreating from global warming
Exists in the arctic, subarctic climatic zones and occurs at higher elevations in the Cordillera zone
Found in over two-thirds of Canada’s land mass
Warming of permafrost changing northern landscape
Four types of Permafrost
Alpine permafrost is found in mountainous areas and taken on a vertical pattern as elevations of a mountain increase
Continuous permafrost occurs in higher latitudes of the Arctic climatic zone, where at least 80% of the ground is permanently frozen
Associated with low mean annual temperatures of -15C or less
Discontinuous permafrost occurs when 30-80% of the ground is permanently frozen
Subarctic climates where temp is -5C to -15C
Sporadic permafrost is mainly in the northern parts of the provinces, where less than 30% of the area is permanently frozen
0 to -5C
Melting of permafrost has caused:
roads to cave in, airport runways to fracture, railroad tracks to buckle, and buildings to crack, tilt, or collapse.
Broadleaf forest
Extends into Canada only in the southernmost Ontario
Temperature is a major factor in limiting the northward: 8°C (46°F) isotherm
Located in southern Ontario contributes to its warmer climate, but "lake effect" is even more important.
One of the largest natural areas lies within the boundaries of Point Pelee National Park
Mixed Forest
The northern needle- trees (conifers) extend south and the southern broad leaved (deciduous) trees extend north.
Contains 19% of Ontario's forests
Communities controlled by climate and soils
Boreal Forest
Canada contains about 30% of the world's boreal zone, which holds nearly three-quarters of Canada's forests and woodlands. Over 2.5 million people live there. Threats include fires, insects, disease, and industrial development, which damage habitats and threaten wildlife such as woodland caribou, wolverines, grizzly bears, and wolves. At least half the boreal forest should be protected, with the rest carefully managed.
Tundra
Tundra is located north of the treeline, where sub soils are permanently frozen. Tundra is a treeless area with dwarf shrubs and miniature wildflowers adapted to a short growing season.
Polar Desert
A prominent feature of the polar desert is the complete absence of sunlight over a period of nine to ten months.
In a polar desert the vegetation is scarce and well-spread
Grassland
At least 80% of our native prairie has been lost
Grasslands National Park contains over 70 different species of grass and over 50 different species of wildflowers
Costal Rain Forest
Rain, and lots of it (or other precipitation, i.e. snow, drizzle, mist, fog....). The area must receive a minimum of 250cm of moisture (100 inches) per year.
Moist maritime climate
The Sitka spruce commonly grows to 70 metres tall and 2 metres in diameter and may live 800 years.
What is a drainage basin
land that slopes towards the sea separated by topographic ridges
Four major drainage basins
1. The Atlantic Basin
3rd largest, 2nd greatest streamflow
2. The Hudson Bay Basin
Largest drainage basin in Canada
Precipitation varies greatly across this basin
3. The Arctic Basin
2nd largest basin
Largest coastline
4. The Pacific Basin
Smallest basin
3rd highest volume of water draining into sea
Ontario superlatives
Canada’s most populous Province
Over 93% of province’s population lives in Southern Ontario
Canada’s second-largest Province (over 1,000,000 sq. km)
Is the heart of Canada’s economy
The most politically influential Province
Ontario and the economic downturn of 2008
Manufacturing and the automobile industry are stalled
Whats required
Fresh directions and investments
Recovery of the US economy (on track)
US policies in trade
Considered a “have-not” province
Two sub-regions of Ontario
Northern Ontario
Southern Ontario
Northern Ontario
Candian shield and Hudson Bay Lowlands
Agricultural opportunities are severely limited by
Climate, soil, physiography
Southern Ontario
Consists of the Great Lakes— St. Lawrence Lowlands
Agricultural opportunities from
Long growing season
Ample precipitation
Fertile soils
Weather variety
Ontatio: Impacts of global economic turmoil
Decline of US market following 2008 economic crisis
Chinese manufactured goods displacing local manufacturers
Western provinces outpacing Ontario growth rates
No help from provincial government due to debt
Ontario: Decline of US market following 2008 economic crisis
US is Ontario’s principal market; recession has dented Ontario’s exports
Modest increase in exports in 2012
Ontario: Globalization of trade has resulted in the “China Syndrome”
Manufacturing shifts to low-cost countries (e.g., China) → developed countries cannot compete with production costs → manufacturing plants in developed countries forced to close
Ontario: Loss of low Canadian dollar
Low Canadian dollar kept price of exports to US at low levels
In 2010, CAD reached parity with USD; in 2013, CAD slightly below par (Cross- border manufacturing now more costly)
Ontario: Missed opportunity
Has Ontario missed economic boom in Western Canada and BC?
Foreign firms supply largest share of high-value manufacturing products in AB, SK, and BC
Ontarios physical geography: Physiographic regions
Great Lakes–St Lawrence Lowlands
Canadian Shield
Hudson Bay Lowlands
Ontarios physical geography: Climate Zones
Arctic
Subarctic
Great Lakes–St Lawrence
Climate of Southern Ontario
Long, warm summer (May to Sept)
Frigid winter (mid-Nov to March)
Three specialized agriculture zones of west of Toronto
Essex – Kent Vegetable Area
Norfolk Tobacco Belt
Niagara Fruit belt
Essex — Kent Vegteable Area
Formerly know as the ‘corn belt’
Currently Canada’s biggest producer of soy beans
Corn, wheat, and soybeans dominate production
Vegetables and fruits are important ‘high value’ alternative crops
Home to about ¼ of all vegetable processing
Leamington has the highest concentration of greenhouses in Canada
Tobacco was formerly of importance; vineyards are of growing importance
Windsor, Chatham and Leamington are the main service centers' in the region
Norfolk Tobacco Belt
Has sandy (deltaic and other lacustrine) soils
Has poor soil fertility relative to other areas
Farm failure and abandonment were common in the 19th Century
In the 1920s, demand for tobacco stimulated agricultural production
Farm prosperity has declined with the demand for tobacco
Five crops currently dominate: corn, soy beans, wheat, hay, and oats
No major service centre exists in the region; higher-order goods and services are obtained in London and Brantford
Niagara Fruit Belt
Fruit and vineyard production are concentrated on the Lake Ontario plain, north of the Niagara Escarpment
Grapes, cherries, peaches, plums, and pears dominate production in the north
The upland south of the escarpment is dominated by a hay-pasture-dairy economy
Soils vary: lacustrine soils dominate in the north, glacially deposited soils in the south
Lake Ontario moderates the climate of the area, particularly on the plain
Agricultural land in the region is under considerable population pressure
Farming operations in Southern Ontario vs Western Canada
Ontario
Avg. size of farms: 244 acres
Diversified crops such as grain corn, barley, winter wheat, soybeans, grapes, vegetables, and tobacco
Western Canada
Avg. size of farms: 1,668 acres (SK)
Dominated by grain farming and cattle ranching
Ontario: Concerns regarding urban sprawl
Farmland now part of urban landscape
Price of farmland well below that of urban land
Mismatch between value of farmland and other commercial uses
e.g. Highland Companies seeking to convert Class I soil into a quarry for high-quality Amabel dolostone bedrock
Urban Sprawl
Southern Ontario has over half of the highest quality agricultural land
Urban sprawl – between 1976 to 2006, nearly 200,000 acres have been lost.
land for growing vegetables or raising cattle might fetch $2,000 an acre, developers are ready to offer farmers $40,000 an acre, knowing they can flip it for twice that when the property becomes part of a new subdivision.
Ontario: Lake Effect Snow
As that air moves across the warm water of the Great Lakes, heat and moisture from the lake rises up into that air mass. That moisture eventually condenses out into snowflakes.
Ontario: Air Pollution
Caused by automobile dependency
More efficient engines reduce exhaust fumes, but this is not enough
Number of electric vehicles increasing yet still small
Ontario is behind BC and Quebec with the amount of electric vehicles
In 2018, the Ontario government removed consumer subsidy to purchase electric vehicles
In 2014, Ontario ceased to produce electricity from coal
The Ontario government’s decision to move away from fossil fuels and into higher-cost energy has pushed some Ontarians into “energy poverty”
It has also increased the cost of doing business in Ontario
Ontario: Water Pollution
Highlighted by Walkerton incident and pollution of Great Lakes
Caused by industrial effluents, farm chemicals, and livestock waste
Great Lakes Water Quality Agreement between Canada and US is commitment to restore and maintain integrity of Great Lakes Basin
A serious problem in Indigenous communities across Canada
Drinking water on reserves falls under the federal government
Boil-water advisories are common
Ontario: Other problems facing Great Lakes Basin
Declining water levels due to global warming lead to retreating shorelines and threat of water erosion
Introduction of exotic species(e.g. sea lampreys, zebra mussels) push out native species and have negative impact on domestic fisheries
Southern Ontario: Energy and Power
Prior to 1940, Southern Ontario was generally lacking in electrical capacity.
This became particularly problematic during the 1950s, when rapid industrial expansion outstripped power supplies.
The demand for electricity is increasing each year.
The energy consumed in Ontario (electrical and otherwise) is currently from five sources:
Hydroelectricity
Coal-based thermal power
Petroleum and Natural Gas from the Interior Plains
Nuclear Energy
Renerable Resources
Ontario: Hydroelectricity
Internal water power
Power dams constructed along the Niagara River, and rapids in the St. Lawrence Seaway at Cornwall
Canadian Shield Water Power
Dams built along the Ottawa River during the 1950s
Damming of the tributaries of the Moose River
Ontario: Coal based thermal power
Use of thermal sources increased after 1950
Power plants were built along the shores of the Great Lakes
Plants use mostly imported American coal
The Liberals (Provincial) passed the Green Energy Act (2009) to turn the province in a new direction of clean, renewable energy sources.
Coal plants produced 25 per cent of Ontario’s power in 2003.
Significant health and environmental benefits -
Ontario is replacing coal with a mix of emission-free energy sources like nuclear and renewables, along with lower-emission energy sources like natural gas.
Ontario: Petroleum and Natural Gas from the Interior Plains
Prior to the 1950s, most of the petroleum products consumed in Ontario were refined at Sarnia using American oil
The opening of the oil fields on the prairies allowed oil (and natural gas) to be transported to the Ontario market via pipeline
Ontario: Natural Gas
Natural gas emits nearly 70 per cent less particulate matter than coal and virtually eliminates mercury and sulphur dioxide emissions.
The Liberals pulled the plug on the plants in the Toronto suburbs of Mississauga and Oakville in what was widely seen as a political play to save the party’s local candidates from defeat in the 2011 election
Cancellation of these plants - $1 billion
Ontario: Nuclear Energy
Energy requirements in the growing industrial and residential markets could not be met through the increases in capacity resulting from other methods of generation
Nuclear power appeared to offer an ‘unlimited’ source of electrical energy
Number one energy source
Generating plants initially utilized uranium mined from the Canadian Shield
Nuclear power meets more than 50 per cent of Ontario's electricity needs. Produces no emissions that lead to smog, acid rain or global warming.
Ontario plans to deal with tonnes of nuclear waste: Bury the problem
Radioactive material leaked into Lake Ontario from the Pickering nuclear plant in 2011.
Aging infrastructure.
This thermal pollution forms a barrier which alters the aquatic balance, changes the habitat for fish, plants, and parasites, and causes fatal heat shock in billions of passing fish.
Even heat is considered pollution
Ontario: Renewable Resources — Wind and Solar
Ontario is moving away from fossil-fuel based, non-renewable energy sources, and toward natural sources that generate less pollution and will help improve Ontario's air quality.
Renewable resources account for only ~ 6% on Ontario’s energy output.
Opposition against wind turbines (?)
Disadvantages: bird mortalities (EU, pain one wing a different colour, 70% better), aesthetic value (people don't like it), might have water issues (they go down deep and disturb rock and water table)
Ontarios Automobile Industry
Heart of Ontario’s manufacturing economy
Expansion is highly unlikely as new plants in North America move to low-wage countries, such as Mexico
The automobile industry in Ontario has dwindled
New investment into the industry will slow but not reverse the trend
Experts do not see a bright future
Robotics technology and government support have kept industry alive
Expansion is highly unlikely as new plants move to low-wage countries, such as Mexico
Expanded greatly following Canada—US Automotive Products Agreement (1965) which:
Guaranteed that Canadian auto plants would not close
Provided advantage of economic of scale
Reduced price of cars for Canadian customers
Resulted in higher wages and benefits for workers