Tectonic hazards Flashcards
(44 cards)
Cross section of the Earth
Crust, mantle, outer core, inner core
What is the mantle?
Made of semi-molten rock, magma
Thickest section - 2900km
Magnesium and iron
What is the inner core?
Solid layer of iron and nickel
Temperature of 5500 oC
What is the outer core?
Liquid layer of the Earth’s core, made of iron and nickel
Characteristics of continental plates
Older
Less dense
Can’t sink
Characteristics of oceanic plates
Younger
Very dense
Can sink
Explain the theory of convection currents
Magma near the outer core is heated. As the magma warms, it expands and becomes less dense. The less dense magma then starts to rise towards the crust. As the magma nears the crust, it begins to cool. The cooling magma becomes denser and begins to sink. The rising and falling magma creates circular currents with the mantle. These currents create friction with the crust above and causes it to move. These are known as convection currents.
Explain the theory of ridge push
Magma rises as the plates move apart. Magma cools to form new plate material. As it cools it becomes denser and slides down away from the ridge. This causes tectonic plates to move away from each other. Occurs at constructive plate margins.
Explain the theory of slab pull
Denser plate sinks back into the mantle under the influence of gravity. It pulls the rest of the plate along behind it.
Which plate margins are earthquakes found at?
All 3 (constructive, destructive, conservative)
Which plate margins are volcanoes found at?
Constructive and destructive
Explain the constructive plate boundary
The plates move away from each other. When this happens, the magma from the mantle rises up and cools to make new land in the form of a shield volcano. Ridge push occurs. The movement of plates over the mantle can cause earthquakes. Ridges can form.
Explain the destructive plate boundary
The dense oceanic plate is subducted under the lighter continental plate into the mantle. Slab pull occurs. Friction causes melting of the oceanic plate and may trigger earthquakes. Destructive plates cause both volcanoes and earthquakes.
Landforms formed at constructive boundaries
Shield volcanoes and ocean ridges
Landforms formed at destructive boundaries
Composite volcanoes, oceanic trenches
Explain the conservative plate boundary
As the plates move, friction occurs and plates become stuck. Pressure builds up because the plates are still trying to move. When the pressure is released, it sends out a huge amount of energy causing an earthquake.
How do plates move at constructive margins?
Away from each other
How do plates moves at destructive margins?
Towards each other
How do plates move at conservative margins?
Move past each other in same or opposite direction but at different speeds
Landforms at conservative margins
Fault lines (San Andreas fault line)
How many killed in L’Aquila earthquake?
308
How many killed in Gorka, Nepal earthquake?
8,841
Economic damage of L’Aquila
$11,400 million in damage
Economic damage of Gorka
$5 billion damage