Restless Earth Flashcards
Age of oceanic crusts
200 million years old
Age of continental crusts
1500 million years old
Properties of oceanic crusts
Denser, newer, younger, can be subduction, can be renewed and destroyed
Properties of continental crust
Older, less dense, cannot be subducted, cannot be renewed or destroyed
Oceanic plate subducts beneath continental plate
Destructive subduction
Two continental plates move together
Destructive collision
When plates move away and hot magma fills in the gaps between
Constructive
Two plates sliding along each other
Conservative
Where plates meet
Plate margins
The more explosive volcanoes in a cone shape
Composite volcanoes
Boob shaped volcanoes which are much less of a threat
Shield volcanoes
What melts the plate as it subducts underneath a continental plate?
Friction
What can usually be linked with destructive subduction margins when the plates rub together under the surface
Earthquakes
Usually next the a volcano on a destructive subduction margin
The sea
The name of the current which makes the hot magma rise
Convection current
Reason why magma rises
Gaseous rocks under the volcano, convection currents
An example of a destructive subduction boundary
Juan de Fuca plates subducts beneath North American plate
When the crust is nor created or destroyed
Conservative
An example of a conservative plate boundary
San Andreas Fault
Constructive plate boundaries are usually under…
Water
Constructive plate boundaries move
Apart
Over many years this may happen to constructive plate margins
Islands may break through the surface water
Shield volcanoes are usually created on a … boundary
Constructive
The name of the tectonic plates
North American, Nasca, South American, Eurasian, African, Indo-Australian, Pacific
Structure of the earth
Inner core, outer core, mantle, crust
Usual thickness of tectonic plates
0-60km thick
The Inner core is made from which two metals?
Iron and nickel
Name of a depression usually found on the oceans floor
Geosyncline
Size of young fold mountains
Taller
Size of older fold mountains
Smaller (after being eroded)
An example of fairly new fold mountains
Rocky Mountains (USA), Himalayas (Bhutan/Nepal), the Andes
How mountains are created
Destructive collision, destructive subduction
How Ocean trenches and fold mountains are made
Destructive subduction
How young fold mountains are made
1) rivers deposit sediment in the geosynclines
2) rivers sediment is then compressed
3) plates are forced together at destructive margins
4) sedimentary layers are forced upwards into fold mountains