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Physical Geography of Canada (land form reagonds (canadian shiled…
Physical Geography of Canada
Geologic Time
cenozoic
quaternary
human beings develop
ice age ends
continents move to todays position
tertiay
early forms of mammals dominate
mountians form
mesozoic
cretaceous
first feathered bird
formation of western cordillera begins
jurassic
most gas and oil deposit form
great variety of fish and reptiles
trassic
shallow seas cover north amarica
reptiles dominate and age of the degings
Paleozoic
permian
most coal deparits form
first reptiles appear, abunant fish
carboninferous
many spiders insects ferns
devonian
first amphibians appear
silurain
life on land apears
armoured fish and large coral reefs dominate the seas
ordovician
collision of north America and Europe results in formation of Appalachian mountains
first vertebrates appear in the seas
cambrian
sedimentary rocks form
many invertebrates develop
percambrian
sponges and jellyfish appear
canadian shiled forms
aquatic plants appear
bacteria may have existed
Volcanoes
Intrusive
Batholith
– Stock
– Lopolith
– Laccolith
– Volcanic
neck
– Sill
– Dike
Extrusive
– Lava flow
or plateau
– Volcano
(many
types)
– Crater
– Caldera
– Fissure
Pyroclastic Flow
Can move up to 700 km/h and can be 1,000 °C
hot
Normally hug the ground and travel downhill,
or spread laterally under gravity.
They are a common and devastating result of
certain explosive volcanic eruptions.
Ex. Pompeii and Mount St. Helens
Earths Crust
crust
upper layer
solid
very thin
0.1% of earths volume
two parts
sima
crust under oceans
sial
continental crust
lithosphere
made of rocks and mineralsu
inclubes
serface crust and below earths crust
solid
asthenosphere
plastic layer of upper mantle
thought 2 provide base witch crustle plates float
ozzy layer
couses
platectonics
mountians building
molten rock that comes out of volcanos
mantle
80% of earths volume
2 parts
made of iron, silica and magnesium
uppermantle (liquid)
lower mantle (solid)
the core
located center of earth
1/3 of earths total mass
2 parts
outer core
liquid, iron, multinmegma
innercore
solidiron, niccle
earth orbet
seasons
not elliptical
winter to cold
almost circuler
pangea
Evedence
Puzzle Pices
continents fit together like a puzzle
fossil types
Similar fossils found across the ocean across each other
Mountain Ranges
similar mountain ranges and ocean apart
Alfred Wegner
Discovered the idea of Pangea
Earth was initially one mass
Continental Drift
theory of continental drift
200,000,000 years ago
continents began to break apart
Continents have ben drifting ever since
Earth's Beginnings
theorys
creation theory
earth
created by higher power
god or gods
took place over thousands of years
evelution theory
univerce began with big bang
15-20 billion years ago
earth is 4,600,000,000 years old
tutle theory
the big bang theory
unviverce began to form 15 - 20 billion years ago
following a huge explosion
dust and gas was created as result
drawn together by gravitational attraction
formed a huge clowed
debrease in clowed
gathered together in circuler movments
eddies
land form reagonds
artic and hutsinsbay lowlands
extreme landscape
really cold
no trees
far from other things
left over glasiures
pollerbears
carabue
artic fox
inuet people
no roads
home built above grounds
live more in the south
northern canada
interior plain
praries
richest dinosour fossles
man made lakes
good soil
bisen, ducks
lots of farms
great lakes and saint loranse low lands
along saint loranse
niagara falls
lots of egercoulture
rocks and minurals
birds and fox
most people living in this reagon
canadian shiled
surrounds lower hatstands bay
lots of forests
largest of canadas reagons
lots of bodeys of water
oldest bedrock
meny fish/insects
not alot of peole live here
small cumunites
apalacion
east cost
highest tides
huge bolders
good soil
jeged mountins
rolling hills
wild hours' sea birds
small towns
western cordilia
between interier plains
rivers
contenental devide
tallest trees and mountian ranges
lots of rain
mountian lians
fishing comunitys
erosion
by water
rain erosion
wave erosion
sandy beach = old
rocky beah = young
river erosion
earodes setement and transports away
ice erosion
freezing and thoughing = cracked rock
by wind
physical processes
geologic time
The end of an era is when genetics change.
le. taking a car, rather then running everywhere
le. grocery store v.s. hunting or gathering food
glaciation
the last ice age was 10 000 years ago (every 10-50 000 years) ice ages are a "reset button"
plate boundaries
folding happends when soft rock layers experience heat and pressure from the mantle forcing it upwords
faulting - happens when hard rock is forced upward with heat and pressure from the mantle
faulting
strike slip - two plates slide past = earthquake (california)
extension fault - two plates pulling away = rift valley
faulting types
collision faut - two continental plates = mountain building
subduction - one continental plate and one ocean plate
precipitation (3 types)
conventionalu prisipitation
in canada usually occurs in the summer
sun heats the ground then as warm air rises cool air rushes to replace warm air