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Intro to Physical Geography
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The study of rocks and the physical history of the earth.
Geology The study of rocks and the physical history of the earth.
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Continental Drift 1915 German Scientist Alfred Wegener suggested the theory of Continental Drift Believed that 300 million years ago, all Earth’s land masses collided to form land mass he called Pangaea (“all land”) 200 million years ago, Pangaea broke into pieces, slowly drifting to the positions of the continents today
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Pangaea
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Wegener’s Four Proofs Video About the 4 Proofs Of Continental Drift
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Evidence of Continental Drift
South America & Africa seem to fit together
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Evidence of Continental Drift
Fossils of the same plants and animals on different continents E.g. the Mesosaurus, a reptile which lived in fresh waters - it could not have traveled across the sea.
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Evidence of Continental Drift
There are mountains and rocks of similar age and structure on both sides of the Atlantic Ocean E.g. The Appalachians (eastern US and Canada) and the Caledonian Mountains in Northern British Isles and Europe
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Evidence of Continental Drift
Ice sheets covered parts of southern Africa, India, Australia, and South America approx. 250 million years ago but these places are warm today! Coral reefs around Antarctica
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An Unbelievable Theory ?
Wegener died in 1930 before there was acceptance of his theory He could not explain HOW the continents moved – suggested tidal forces but did not make sense 1960s, Canadian J. Tuzo Wilson helped to bring up theory again Newer technology able to help explain…
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What Will the Earth Look Like
Vide of what the Earth used to look like – and what it will look like in the far future
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Pangaea Ultima The world may look like this in another 250 million years
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Plate Tectonics Theory
Helps to explain most geologic processes States that Earth’s outer shell consists of plates that move causing earthquakes, volcanoes, mountains and the formation of new crust
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Plate Tectonics Earth’s outer shell consists of about 20 plates
most have both continental & oceanic crust
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Plate Tectonics Plates are floating on layer of hot rock - the mantle
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Tectonic Video Video About Tectonic Plates
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Plate Tectonics Don’t entirely understand what makes the plates move
Think that unequal distribution of heat within the core of the earths causes convection currents in the mantle that push the plates around
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Plate Tectonics When plates are pushed together you could get:
A mountain range A volcano New crust An earthquake
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The 3 Kinds of Plates Boundaries
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1) Divergent Boundaries
The plates are moving away from each other Ex: Mid-Atlantic Ridge Explains the hot springs that run through Iceland
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2) Convergent Boundaries
The plates are pushing toward each other Ex: the boundary between the Eurasian and the Indian plates under the Himalayas
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3) Transform Boundary The 2 plates slide past each other
Ex: the boundary between the North American plate and the Pacific plate in California
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Plate Tectonics Earthquakes, volcanoes and mountain ranges usually follow plate boundaries Earthquake map below
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Plate Tectonics Volcanic activity surrounding the Pacific Plate has been labeled the “Pacific Ring of Fire”
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Volcanoes Volcanoes can occur when one plate is pushed under another (oceanic plates are heavier and will push up the lighter continental plates)
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Volcanoes Canada’s west coast has currently dormant (sleeping) but not extinct (dead) volcanoes
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Mountain Ranges Mountains are created when plates push against each other and fold the crust Mountain ranges can also be volcanic in nature
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Watching the Himalayas Form
How the Himalayas Were Formed
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Canada’s Mountains New West Coast Mountains The Rockies
Old East Coast Mountains The Appalachians
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Earthquakes Earthquakes happen when 2 plates rub against each other, causing friction
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Earthquakes The San Andreas fault is a large crack in the earth's surface where two gigantic plates are sliding past one another (California)
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Tsunamis Tsunamis, like the one that hit Japan in March 2011, are caused by underwater earthquakes
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Tsunami March, 2011
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Tsunami December, 2004
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Tsunamis City of Banda Aceh, Indonesia before and after the tsunami in 2004
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Tsunamis and Canada Location: West coast of British Columbia Date: March 27, 1964 Description: The strongest North American earthquake of the century, measuring 8.5 on the Richter scale, struck off Anchorage, Alaska. It sent a tsunami travelling at over 700 km an hour hurtling toward the BC coast. The 4.3 m wave destroyed houses and flooded basements in Hot Springs Cove and Bamfield on the coast of Vancouver Island. The wave travelled up Alberni Inlet and flooded town of Port Alberni. Luckily, no one was killed, but damages caused by the wave totaled over $8 million.
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