platetechtonics. continental drift the theory discovered by alfred wegener that states the...
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Platetechtonics
Plate techtonics
Continental Drift
The theory discovered by Alfred Wegener that states the continents were once connected but later drifted apart to their current locations.
Evidence supporting continental drift
1) Shapes of the continents- The continents fit together like a jigsaw puzzle.
The first piece put in place was the Eastern side of South America and the Western side of Africa
Evidence supporting continental drift
2) Matching geological structuresMountain Ranges:- Mountain Ranges on one continent end at
the coast and appear to continue on a different continent
Types of rock:- Similarities between the fold and age of
rocks were found on different continents
Evidence supporting continental drift
3) Matching Fossils: - The fossils of one species were found on two
separate continents.
- Of these the most important was a freshwater reptile found in Africa and South America(it would not be able to cross the ocean)
Evidence supporting continental drift3) Paleoglaciation: When glaciers move forward or retreat they
leave u-shaped valleys in the earth.- Many of these were found in tropical parts of
Africa and South America : These places are now found in the tropics where glaciers would not form
- The pattern of the glaciers on these continent only make sense if the continents were together at some point
Layers of the Earth
Layers of the Earth
Layer of the Earth
Layers of the Earth
Layers of the EarthCrust: Outer most layer. Made of solid brittle
rockLithosphere: Contains the crust and the
uppermost mantle. Made up of the tectonic plates
Layers of the EarthCrust: Outer most layer. Made of solid brittle
rockLithosphere: Contains the crust and the
uppermost mantle. Made up of the tectonic plates
Athenosphere: found above the upper mantle. Made up of partly molten rock
Mantle: the thickest layer on the earth. Broken into two parts upper and lower
Layers of the EarthCrust: Outer most layer. Made of solid brittle rockLithosphere: Contains the crust and the uppermost
mantle. Made up of the tectonic platesAthenosphere: found above the upper mantle. Made
up of partly molten rock Mantle: the thickest layer on the earth. Broken into
two parts upper and lowerUpper Mantle: Made of partly molten rock containing
Fe and Mg (lava the consistency of toothpaste)Lower Mantle: Solid dense material also containing
Mg and Fe
Layers of the Earth
Outer Core: A liquid made mainly from iron and nickel
Inner Core: A solid mixture of mainly iron and nickel at 5000 – 6000 C. The high pressure makes it solid