About 1400km in diameter, a solid and dense layer composed of iron and nickel with temperatures of about 5500 degrees Celsius
Outer core:
About 2100 km thick, a semi-moltenmetal layer with temperatures between about 5000 - 5500 degrees Celsius
Mantle:
About 2900km thick, a semi-molten layer which is less dense than the outer core
Crust:
The thickness varies, and is made up of two types of crust.
There are two types of crust:
The Oceanic crust and The continental crust
The Oceanic Crust is thinner (5-10km) but heavier and denser
The Continental crust is thicker (25-90km) but is older and lighter
Oceanic crust is continually being created and destroyed as a result of plate movement, where it is denser and so subducts under the continental crust.
This is why continental crust is much older than oceanic crust, as it isn't destroyed
Plate tectonics
The crust is broken into a number of tectonic plates
These plates move on top of the semi-molten mantle below.
Tectonic theory once stated the movement of the plates was the result of convection currents in the mantle
Current theory is called slab pull theory which suggests that the movement is the result of the weight of the denser oceanic plates subducting and dragging the rest of the plate along
A plate boundary or margin is where two plates meet
Volcano distribution
Most volcanoes occur at constructive and destructiveplate boundaries
The majority of active volcanoes (approximately 75%) are located around the rim of the Pacific Ocean called the 'Ring of Fire'
Hotspots occur away from plate boundaries and are plumes/columns of magma which escape through the Earth's crust
Distribution of Earthquakes & Volcanoes
Earthquake distribution
Earthquakes occur at all types of plate boundaries
Most occur along the Pacific 'Ring of Fire' (approximately 90%)
Plate Boundaries
-Types of plate boundary
Volcanic eruptions and earthquakes most commonly occur at or near plateboundaries
There are three main types of plate boundaries:
Constructive
Destructive
Conservative (transform)
Constructive plate boundary
At a constructive boundary the plates are moving apart
The Mid Atlantic Ridge is an example of a constructive plate boundary
Both volcanic eruptions and earthquakes can occur at this type of plate boundary
Destructive plate boundary
At a destructive plate boundary the plates are moving together
The denser, heavier oceanic plate subducts under the lighter, less dense continentalplate
The boundary between the Nazca plate and the South American plate is one example
Both volcanic eruptions and earthquakes occur at this type of plate boundary
Conservative (transform) boundary
At a conservative (transform)boundary the plates move passed each other in opposite directions or in the same direction at different speeds
Earthquakes are the only hazard at this type of boundary
The Primary Hazard of Tectonic Activity
Volcanic Eruption
Ash
Pyroclastic flow (Clouds of superheated material up to 700 degrees centigrade which can travel up to 500 kmph)
Lava flow
Gas emissions
Volcanic bombs
The Primary Hazard of Tectonic Activity
Earthquake
Ground shaking
Gas emissions
The Secondary Hazards of Tectonic Activity
Volcanic Eruption
Lahars (When water(often from melting snow and ice) mixes with volcanic ash to create a fast moving mudflow)
Acidification (Sulphur emissions from volcanic eruptions increase the acidity of water)
Landslides
Climate change
Fires
Floods
The Secondary Hazards of Tectonic Activity
Earthquake
Building collapse
Landslides
Gas leaks
Fires
Soil liquefaction (When loose material including soil and rock acts like a liquid due to an earthquake.)
Subsidence(The sudden sinking of the Earth's surface)