Mind map
Structure of the Earth
Map content
Structure of the Earth
Basic Structure
- Crust
- Solid
- Composition
- 46.6% Oxygen
- 27.7% Silicon
- Thickness
- Max. 70km
- Under land 30km
- Under oceans 5km
- Mantle
- Solid
- Semi-solid
- Extends from 20km to 2900km
- Half way to the centre of the Earth
- Composition
- Fe
- Mg
- Al
- Si
- O
- Temperature
- 100ºC at top
- 3700ºC at bottom
- Caused by isotope decay
- Outer Core
- Liquid
- 2300km thick
- Molten nickel-iron alloy
- Controls magnetic field
- Inner Core
- Solid
- 1200km thick
- Solid iron
- 7000K at centre
- Lithosphere
- Crust & Upper Mantle
- Solid
- >80km thick
- Thinner under oceans
- Floats on lower mantle
- Divided up into plates
- Crust
Plate Tectonics
- First Evidence
- 1912
- Shape of Africa & Americas
- Fossil evidence
- Thought to be driven by centrifugal force
- 1929
- Thought to be caused by convection in rocks
- Evidence for sea floor spreading
- Magnetic stripes
- 1912
- Plate Boundaries
- Transform boundaries
- Two plates sliding along each other
- San Andreas fault line
- Convergence boundary
- Two plates moving towards each other
- Creates a mountain chain and volcanoes
- Can be of equal or unequal density
- If density is unequal one plate rises above the other
- Andes
- Himalayas
- Divergent boundary
- Plates move apart
- Mid-Atlantic ridge
- African rift valley
- Hot spots
- Plumes of hot magma breaking the surface of the crust
- Hawii
- Transform boundaries
- Continental Drift
- Rodina
- Pangaea
- Gondwana
- Africa, South America, Antarctica, India, Australia
- Larussia
- North America, Eastern Europe, Western Europe, Siberia
- Gondwana
- Pangaea
- Rodina
- First Evidence
Volcanoes
- Stromboli eruptions
- Intermittent explosion or fountaining of basaltic lava
- Single vent or crater
- Releases volcanic gases
- Occur every few minutes or so
- Mt Etna 2002
- Hawiian eruptions
- Highly fluid lava flows
- Quiet
- several vents
- Gradually builds up to a shield volcano
- Vulcanian eruptions
- Vulcano off the coast of Italy
- Strick magma plugs up the central vent
- Magmatic gas builds up pressure
- Blasts magma and volcanic dust
- Peleean eruptions
- Violent explossions
- Glowing clouds of hot ash and dust
- Volcano blows apart
- Stromboli eruptions
Seismology
- Study of earthquakes
- Useful for determining the structure of the Earth
- Time of arrival indicates what material waves have passed through
- Seismic waves from earthquake pass through the Earth
- P-Waves
- Primary waves
- Compression waves
- Can pass through solids and liquids
- Get faster in more dense media
- Faster
- S-Waves
- Secondary waves
- Shear waves
- Can pass through solids but not liquids
- Get faster in more dense media
- Slower
- Measured with a seismograph
- Refraction of waves
- When passing from a low to high velocity medium, waves get bent
- Creation of shadow zones
- P-Waves
Information
- Description
- Earth as a Planetary System Mind Map on Structure of the Earth, created by Briony Leary on 24/08/2017.
- Created by
- Briony Leary
- Views
- 2
- Rating