Geography Volcanoes And Earthquakes Flashcards
Names the different layers of the Earth
Inner core
Outer Core
Mantle
Crust
Characteristics of the Inner Core
Hottest part of the Earth
It is solid
1260m thick
Made up of metal, mainly iron mixed with nickel
Outer core characteristics
This part of the core is liquid
About 2220km thick
Made up of iron mixed with nickel
Mantel characteristics
Thickest part of the Earth at about 2900km thick
The outer mantle is hard, but further in it is like soft toffee
Crust characteristics
8-65km thick
This is like the earths hard skin.
Made form less dense rock so able to float on the mantle
Oceanic Crust characteristics
Forms on ocean floor
Denser (heavier)
Thinner - on average 7km thick
Mainly made of basalt
Continental Crust characteristics
Makes up land masses
Less denser (lighter)
Thicker - on average 50km thick
Mainly made of granite
Constructive margin
When the two plates are diverging above the upward plume of a convection cell. Magma rises through the gap between the two plates, resulting in volcanoes.There are lots of eruptions and earthquakes along constructive margins but they are generally gentle.
Destructive margins
They occur when two plates one made of oceanic crust and one made of continental crust are converging. This can lead to pressure in a sudden slippage of the plates, resulting in a powerful earthquake and volcanic eruptions.
Subduction
At destructive plate margins when the two plates meet, the oceanic plate dives beneath the continental plate, because it is denser. This process is known as subduction.
How are fold mountains created?
The continental crust of a destructive plate margin buckles upwards, creating a range of fold mountains.
Collision margins
A collision margin occurs when two plates made of continental crust converge. Because neither plate is denser than the other, subduction does not occur. Therefore, the plates simple buckle up to create a range of fold mountains. There are no volcanos along collision margins but there are powerful earthquakes.
Conservative margins
Conservative plate margins occur when two plates move alongside to one another in opposite directions or in the same directions. When the plates slip, this pressure is released as a powerful earthquake. There are no volcanos.
Epicentre
The point underground where the plates slip and from where the seismic waves radiate outwards.
Focus
The point in the Earths surface directly above the focus; shaking here will be strongest.
Aftershocks
Smaller earthquakes that occur in the hours, days, weeks and months following the main ever
Not caused by the plates slipping a little more as they settle down into their new configuration.
Seismic waves
Energy waves that radiate out from the focus and cause the ground to shake, Primary waves stretch compress the ground, whilst secondary waves shake it from side to side.
Fault line
A fracture in the rock at a plate margins when where pressure builds up if the moving plates stick.
Magnitude
The higher the magnitude of an earthquake, the more energy is released and the greater the potential for damage to buildings and therefore deaths/injuries to people.
Richter Scale
It assesses the amount of energy released by the earthquake, the intensity of shaking. It is a logarithmic scale, which means that every point you go up on the scales sees a 3 fold increase in energy released.
Mercalli Scale
It assesses at the impacts of an earthquake by looking at things like the structural damage to buildings.This is correlated with the earths energy, but is influenced by other factors too.
Acidic lava and basic lava differences
- acidic lava is viscous, is light in colour and has higher silica content. Basic lava is non-viscous, is darker in colour and has lower silica content.
Stratovolcanoes
They are found on constructive margins.
Has basic lava and this means that eruptions are effusive and more frequent. The lava flows relatively rapidly from the vent. The volcano that is created has a very wide base but very gentle slopes.
Stratovolcanoes
Found on destructive margins. They have acidic lava. It is steep.