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restless Earth

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restless Earth
Structure of the world
- Inner core= solid Iron + Nickel. 15,000 degrees
- Outer core= liquid layer Nickel + Iron
- Mantle= semi molten rock. 4000 degrees. The thickest layer- makes up half the earth- about 2900 Km thick
- crust= solid, made up of plates- thinnest layer- about 20 Km
- Mantle= semi molten rock. 4000 degrees. The thickest layer- makes up half the earth- about 2900 Km thick
- Outer core= liquid layer Nickel + Iron
- Inner core= solid Iron + Nickel. 15,000 degrees
Continental drift
- Evidence
- Plates fit together. Africa+ south America
- Matching fossils different continents
- Wegener
- Pangaea
- Continents were joined together
- Explanation
- molten rock heated by earths core
- rises towards crust
- cools sinks back down again
- process= convection current
- cools sinks back down again
- rises towards crust
- plates floating on mantle
- convection currents in liquid mantle
- Drag floating plates as they circulate
- molten rock heated by earths core
- Evidence
Plate boundaries
- constructive
- Formations
- shield volcanoe
- Earthquakes
- 2 plates move apart. magma fills the gap
- Formations
- conservative
- formations
- Earthquake
- plates scrape past each other travelling opposite directions/same direction different speeds
- formations
- Destructive
- oceanic +continental plate collide. Oceanic plate sub ducted under continental plate
- formations
- composite volcanoes
- ocean trenches
- earthquakes
- constructive
types of plate
- Oceanic
- Heavy
- Less thick
- dense
- Continental
- thicker
- light not dense
- Oceanic
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- Description
- introduction into the topic restless earth
- Created by
- chapel.jacquesel
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