Geography unit 2 quiz
Unit 2: Physical geography
Age of Earth: Around 4.54 billion years old
Precambrian (Earliest Life)
4.6 billion - 570 million years ago
Precambrian shield formations: Canadian Shield, Brazilian Shield, Africa Shield
First single and multi celled organisms
Paleozoic (Ancient Life)
570 - 245 million years ago
Formation of Appalachian Mountains
Large parts of North America are created
Age of amphibians and fish
First plants, animals and insects appear
Large swamps and shallow seas - coal formed from this vegetation
Mesozoic (Middle life “age of dinosaurs)
245 - 66 million years ago
Shallow seas in the interior of North America
First flowering plants, birds and mammals
Age of reptiles (dinosaurs)
Innuitian Mountains formed
Cenozoic (Recent Life “Age of Humans”)
66 million years ago - present
Ice sheets cover North America
Continents take present shape
Complete formation of Rocky Mountains
Humans, mammals and modern forms of life evolve
Continental drift
In 1912 German Scientist Alfred Wegener (meteorologist) created the Theory of Continental Drift
What is it?
Theory that all continents had once been joined together in a single landscape
This big combined continent was called Pangae
Geke apart over time and formed the landscapes that we have today
Evidence that supports Wegener’s theory:
Jigsaw puzzle: coastlines of the continents all fit together just like a puzzle.
Fossil correlation: similar fossil remains from the same period found on different continents
Geologic evidence: the mountains on the East coast of North America and northern Europe are made of the same type of rock
Past climate data: similar glacier deposits and striations exist in South America and Africa. This suggests that a glacier passed through this region.
Even though Wegener provided evidence of the continental drift, he couldn’t prove why this was happening.
Plate Tectonics
Plates move, collide, pull apart or scrape against each other
Tectonic - the deformation of the crust because of a plate interaction
Lithosphere - made up of the crust and upper part of the mantle
Global plates: North American plate, South American plate, Pacific plate, Antarctic plate, Indian plate, Australian plate, Indo-Australian plate, African plate and Eurasian plate
How Do Plates Move?
Due to heat in the asthenosphere - described as hot taffy or warm goo
Heat is being released from the center of Earth
It is hot and gooey because convection currents cause hot material to rise and expand
Allows plates to movet CD a
Key Terms
Boundaries - where different pieces of lithosphere meet at edges
Faults - breaks in the Earth’s crust
What Do They Create?
Volcanoes
Mountain Ranges
Deep Ocean Trenches
Plate Boundaries
Divergent Boundary
Two oceanic plates pull away from each other - seafloor spreading
As plates move, rising magma fills in the gap, resulting in volcanic activity
Convergent Boundary
Two plates crash towards each other
3 type
s: oceanic - oceanic, oceanic - continental, continental - continental
Oceanic - Oceanic: one plate is pushed under another allowing magma from the mantle to rise (volcanoes)
Oceanic - Continental: Ocean plate (thinner) slips under land plate (thicker) which creates trenches. This is known as subduction.
Continental - Continental: Collision causes crust to rise resulting in mountain ranges
Transform Boundary
Two plates move sideways against each other - known as lateral slipping
Friction builds pressure and released pressure causes Earthquakes
Earth Layers
Core
Sits at the center of the Earth and spins in a liquid containing iron and nickel
Mantle
Made up of magnesium and iron rich rocks
Sits in a thick liquid called magma
Rocks are in constant convection cycle
Heat from the core warms rocks and causes them to move away from the core
the rocks cool down and start to move back towards the core
Crust
Divided into massive plates that float on the mantle
Convection movement in the mantle causes tectonic plates to slowly shift
Natural Disasters
Earthquakes :
a movement of the Earth’s crust caused by stress build up within geological faults or volcanic activity.
Plate tectonics are another cause of earthquakes. Areas that are most likely to get earthquakes in Canada are the coast of BC, the St. Lawrence and Ottawa valleys, and parts of three northern territories.
Floods:
most common disaster in canada.
Occur when there is a heavy or steady rain for several hours or days, which oversaturates the ground.
Hurricanes, storms, ice jams, or breaking dams can also cause flooding
Wildfires
Usually occur from May to September
45% of all wildfires were caused by lightning and are responsible for 81% of area burned
Regions in canada that are most vulnerable to wildfires are Western Cordillera and Boreal Forest zone
Hurricanes
A storm with extremely high winds
The storm surge of a hurricane pushes water inland, causing serious flooding
Landslides
The downward movement of the rock or soil triggered by natural processes or human actions.
Most damaging landslides occur in the mountainous regions in BC
Tornadoes
A violent rotating column of air in a shape of a funnel cloud
Uproot trees, flip cars, and damage homes
Usually occur in SOuthern Prairies, southern Ontario, Quebes, the interior of BC, and western New Brunswick.
Winter storms
Can be sudden and last for days
They can bring heavy snowfalls, dangerously low temperatures, strong winds, and frozen rain
Most occurring winter storms in Canada are blizzards and ice storms.
A blizzard is a storm with very high winds and heavy snow lasting at least three hours
An ice storm is caused by the accumulation of freezing rain
Rock Cycle
3 Types of Rocks:
Igneous rock
Formed when magma cools and hardens
95% of Earth’s crust
Sedimentary
Forms when sediments compress into a rock overtime
Sediments are small particles of sand, mud and other material
Metamorphic
Rock that has been changed by heat and pressure
Other rocks can be changed into metamorphic rock
Full Cycle
Magma to igneous rock: cooling
Igneous, metamorphic or sedimentary gets turned to magma through melting
Igneous, metamorphic or sedimentary rock gets turned to a sediment through weathering, erosion and deposition
Igneous rock to metamorphic rock: heat and pressure
Sediments to sedimentary rock: compaction
Sedimentary rock to metamorphic rock: heat and pressure
Weathering
The process by which rocks and minerals break down into smaller pieces due to various natural forces
Natural forces: water, wind, temperature, plants and roots, oxygen and acid rain
Chemical weathering
Water: dissolves minerals in rocks over time, resulting in the rocks weakening and disintegrating
Oxygen: reacts with minerals (iron ) in a process called oxidation and forms rust like substances that weaken the rock
Acid rain: reacts with minerals in rocks and breaks them down over time
Physical weathering
Water: seeps into cracks in rocks. When water freezes, it expands, forcing the crack to widen and breaking the rock apart
Wind: carries small particles of sand and dust that are like sandpaper, wearing down rocks oliver time
Temperature: rocks expand when heated and contract when cooled. Repeated cycles of heating and cooling causes the outer layers of rock to crack and flake off
Weathering = breaking down of rocks, caused by natural forces.
Erosion = moving the broken up pieces of rock to a new location.
Deposition = broken up materials built up in a new location.
Glaciation
A glacier is made up of fallen snow that, over many years compresses into large masses of ice
The weight of the glacier pressing down causes the bottom layers of ice to melt, which makes the glacier move (slide)
During the last ice age 30% of the world was covered with glaciers, right now only 10% of the Earth’s surface is covered in ice
Types of Glaciers:
Alpine glaciers
Form on tops of mountains and slowly creep down
This process creates valleys
Ice sheets
Form broad domes and spread out is all directions
They cover their surroundings with a layer of ice
Examples: Antarctica and Greeland
Glaciers affect the land
Glaciers erode mountainsides and carve valleys
They dig rivers and lakes
They transport materials through large distances
200 000 km of Canada is covered in glaciers
Glaciers and Climate Change
When the temperature increases, the glaciers melt
This helps scientists to determine the rate of the climate change
Climate and Weather:
Weather makes up the climate of a location
Climate refers to weather conditions of a place averaged over a long period of time
The greenhouse effect causes the temperature to increase which causes many glaciers to melt
Freshwater from melted glaciers runs off in oceans
This causes sea levels to rise
The addition of freshwater to marine ecosystems harms multiple species
Increases the rate of the occurrence of natural disasters
LOWERN:
L - Latitude
The distance of place is located from the equator
Closer to equator = hotter
Farther from equator = colder
Earth’s curvature causes the sun’s energy to be spread out over large areas towards the poles
Ocean currents
Warm currents = warmer temperature of nearby area
Cold currents = cooler temperature of nearby area
Wind
Low pressure system = hot air rising, creates clouds and precipitation
High pressure system = cool air sinking, creates clear skies
Air masses: characterized based on their moisture content and temperature
Moisture:
Maritime - wet (formed over water)
Continental - dry (formed over land)
Temperature:
Tropical - hot (formed near the tropics)
Polar - cold
Arctic - very cold (formed over the arctic)
5 air masses
Continental arctic - bitterly cold and dry
Continental polar - cold and dry
Polar maritime - cold and moist
Continental tropic - hot and dry
Polar tropic - warm and moist
Elevation
Height about the Earth’s surface/altitude
As elevation increases, the average annual temperature decreases
Relief
Refers to the shape of the land; the shape affects the amount of precipitation in an area
Windward: the side of the mountain that faces the prevailing wind, gets the most rain
Cool and moist
Leeward: the side of the mountain facing away from the prevailing wind, drier side (rain shadow)
Warm and dry
Nearness to water
Wind carries moisture over nearby land, creating a moderating effect on climate
Summer: bodies of water remain cooler than the surrounding land
aLand is cooled is by the water
Winter: bodies of water retain their heat and are warmer than surrounding land
Land is warmed by the water
Carbon Tax
Carbon tax is when people are being charged tax for burning fossil fuels
Some fossil fuels are taxed more than others because they emit more greenhouse gasses when burned
The government hopes that carbon tax will influence people to reduce their use of dangerous carbon emissions in order to pay less tax
The price increases
The cost of the tax per 1 tonne of carbon released will increase by $15 each year
The increase in price will stop in 2030
The government created a flexible program
Some jurisdictions were offered to set their own carbon tax pricing system
3 jurisdictions (BC, Quebec, an the Northwest territories) have a separate plan for carbon taxing that meets the minimum standard
All Canadians receive rebate for the carbon taxes they pay
80% of all Canadian receive more rebate than the carbon taxes they pay
20% pay more tax than they receive because they drive gas-guzzling cars or live in very big houses
Liberals have called for a pause in the tax as it affects heating oil
Government is trying to give tax relief to lower-income families that have been hit the hardest by inflation, which are also the ones who mostly use heating oil
Some people say that this pause is unfair to to the tensions with the Atlantic provinces which mostly use heating oil and will greatly benefit from this decision
Physical Regions of Canada
The Canadian Shield
Biggest region in Canada by area
Oldest region
Flat (covered by sedimentary rocks) with round hills
Some of the oldest rocks in the World is found here
Lakes, thin layers of soil and rolling hills
Majority of the region is covered in boreal forests
Very cold climate (long winters and very short summers)
Pulp and paper factories due to a large amount of trees
Interior Plains
Big areas of low-lying lands
Has mineral-rich soil
Permafrost, spruce forests, streams, and treeless tundra
Rivers, flat, large, and shallow lakes, and islands
Bare plain
Extreme temperatures and little precipitation
Mixed deciduous and coniferous trees
Grasslands
St. Lawrence Lowlands
Where we live (South parts of Ontario and Quebec)
Smallest region in Canada
Flat plains with small hills and deep river valleys
Glacier activity resulted in multiple lakes and rivers
Humid climate
Vegetation consists of a mix of deciduous and coniferous trees
Most likely to be used for agriculture
Western Cordillera
Takes up the western part of Canada (BC, Yukon, etc.)
The newest and youngest region
Mountain ranges separated by plateaus and valleys
Maritime climate
Evergreens, grasses and even cacti
Hudson Bay Lowlands
Mostly consists of flat area covered by swampy forests or permafrost
Located between Canadian Shield and southwestern shores of hudson bay and James Bay
A subarctic climate
Wet and boggy landscape
Little vegetation due to constantly frozen soil
Most likely to be used as a fishing lodge
Appalachian Mountains
Located in Labrador, Newfoundland, Quebec, Nova Scotia and New Brunswick
Lower ranges, ridges, valleys, and forests
Oldest highland region/mountain ranges in canada
Erosion has rounded and shortened the mountains
Consists of sedimentary and volcanic rocks
Harsh climate but warm enough for trees to exist
Vegetation consist of a mix of deciduous and coniferous trees
Fertile soil
Arctic region
Nunavut, and the Northwest territories
Contain some igneous and metamorphic rock but mostly of sedimentary rock
Covered by ice and permanent snow
Cold, harsh climate
No vegetation
Has the second tallest mountain range and the longest river in Canada
Human Led Activities:
Agriculture - the science of cultivating soil, crops and livestock
As population increases, demand for agriculture increases
Farmers use intensive farming practices like fertilizers, pesticides and fuel
The importance of agriculture is it provides us with food and grows crops and plants
Mining - extracting natural resources from the ground
Open pit mining: mining that occurs ON THE SURFACE of the Earth in an open pit
Underground mining: tunnels that go through the Earth’s crust. Minerals and metals are extracted underground
Mining provides us with minerals that are the basis of our daily products
Deforestation -lumber is an important resource used for housing construction, paper and other industries
Forestry involves using forest resources for non forest activities
Clear cutting means to cut down all the trees in an area
Selective cutting: means selecting mature trees to cut down and leaving the rest
They release carbon dioxide
Forests provide habitats for animals