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Natural Forces that Shape the Earth
Physical Geography Natural Forces that Shape the Earth
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Planet Earth Geologic History Plate Tectonics Earth’s Interior
Rock Cycle Erosion and Weathering Glaciers
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Geologic History
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Geologic History Precambrian Era Vulcanism Fault Ancient Sea
Igneous Rock
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Geologic History Paleozoic Era Erosion Erosion Sediments Sediments
Igneous Rock
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Geologic History Mesozoic Era Erosion Sediments Sediments Igneous Rock
Mountains Forming
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Geologic History Cenozoic Era (Today) Cross Section of Canada 50 N
Sedimentary Mountains Eroding Mountains Forming Sedimentary Plains APPALACHIAN MOUNTAINS PACIFIC OCEAN ROCKY MOUNTAINS Igneous Rock ATLANTIC OCEAN INTERIOR PLAINS CANADIAN SHIELD
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Plate Tectonics - Continental Drift
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Plate Tectonics - Continental Drift
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Plate Tectonics - Continental Drift
PROOF!
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Plate Tectonics Map
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Plate Tectonics Processes
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Plate Tectonics Separating
Mid Atlantic Ridge
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Plate Tectonics Separating
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Plate Tectonics Separating
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Plate Tectonics Separating
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Plate Tectonics Colliding
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Plate Tectonics Colliding
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Plate Tectonics Sliding
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Plate Tectonics Sliding
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Plate Tectonics Sliding
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Plate Tectonics Sliding
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Plate Tectonics Sliding
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Earth’s Interior HYDROSPHERE ATMOSPHERE Crust - 8-64 km thick
Air ATMOSPHERE Water Crust km thick - cold & fragile - Granite and Basalt Land LITHOSPHERE Mantle km thick - hot & molten - Magnesium and Silicon Outer Core km thick °C - liquid Nickel and Iron Inner Core km thick °C - solid Nickel and Iron
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Rock Cycle MAGMA Heats and melts Cools and hardens IGNEOUS METAMORPHIC
Weathers, erodes, and deposits Stresses or heats SEDIMENTARY
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Rock Cycle
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Erosion and Weathering
Water – sheet erosion Wind – massive dust Storm during the 1930s
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Erosion and Weathering
Wind Erosion Hoodoos
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Erosion and Weathering
Erosion by Gravity Freeze and Thaw
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Erosion and Weathering
Mountain (Alpine Glaciers) Fiords
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Glaciers of the Ice Age
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Glacier Features Glacial Erratic Glacial erratics are large pieces of rock that have been transported away from their source areas by moving glacial ice sheets. These can be found throughout southwestern Ontario and were carved out of the Canadian Shield and moved here by the ice.
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Striations are scratches in rock made by rock held in the ice which scoured the earth as it moved over.
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Drumlins are made of till and are formed at the base of a retreating glacial ice sheet by sediments washing out as the glacier melted. The narrow end points in the direction of retreat. Drumlins are evident around Kitchener and Guelph.
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Potholes were formed by glacial meltwater streams carrying great amounts of sediment which eroded the rock.
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Formation of Great Lakes
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