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Chapter 2: Canada’s Physical Landscape. Formation of the Earth 2.1. Formation of the Earth. 2.1 Planet Earth. Formation of the Earth’s Interior.
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Formation of the Earth 2.1 Formation of the Earth 2.1 Planet Earth
Formation of the Earth’s Interior • @5 billion years ago, plantesimals (meterorites,icy comets) collide heat released (Kinetic energy to thermal energy) • Entire planet melts (still cooling today) • Gravity sorts materials by density • Fe (iron) in center • All other compounds towards surface
Earth’s Four Layers • Crust • Mantle • Outer Core • Inner Core
Outer layer 5-100 km thick 2 types of crust Oceanic (very dense) Continental (less dense) The Crust
Middle layer Very thick layer The Mantle
The Core • Made mostly of iron • 1/3 of the earth’s mass • Very hot
How are the earth’s layers similar to an egg? Shell=crust Egg white=mantle Yolk=core Earth’s Layers
The Earth’s Interior Distance: 6730 km (3963 miles)
What is ‘ Plate Tectonics’? • From Greek ‘tektonikus’ meaning building or construction • Plate tectonics refers to the process of plate formation, movement, and destruction.
Tectonic Plates • Earth’s crust is broken into about 19 pieces • These plates move on top of the crust.
1915 Alfred Wegener proposes theory of continental drift. • Supercontinent Pangaea (‘all-earth’) [225mya]. • Continents ‘broke apart’ and moved into current positions.
Evidence for Continental Drift? • Wegner’s evidence • Fit of continents • Match of magnetic bands on rocks on either side of the Mid-Atlantic Ridge • Fossil plants, animals, rock types / geology • match on opposite shores • deposits inconsistent with current geography
Wegener suggested that the pattern formed with continents together at the south pole. Glacial deposits, including structures that indicate ice flow direction are located in ancient rocks as shown on the left.
Plate Margins: how do we know? • Marked by volcanic and tectonic activity
Crustal Processes • Destruction (subduction) • Creation (volcanism) • Alteration / deformation (folding and faulting)
Subduction Zones • Activity: • Subduction zone; shallow to deep earthquakes; volcanism (continental) • Examples: • ocean trench (Pacific Ocean by Japan); explosive volcanic mountains ‘Ring of Fire’