Paper 1 - Hazardous Earth (Techtonics) Flashcards
what are the 2 types of crusts
oceanic and continental
continental crust facts
- made of thick granite
- low density
- forms over the land
oceanic crust facts
- under the oceans
- made of basalt
- high density
- 6-8km deep (thin)
lithosphere
uppermost layer of the earth - it includes the top of the mantle and the crust
—> it is cool and brittle
asthenosphere
part of the earth’s mantle below lithosphere
—> it is hot, semi-molten layer
techtonic plates
the earth’s surface is broken into large pieces
layers of the earth
- crust
- mantle
- outer core
- inner core
convection current
this occurs in the mantle and is the rising, spread, and sinking of magma
how do plates move - convection current
- hot air rises
- it looses heat and cools down
- it sinks back down to be reheated
- the magma and crust create friction which causes the plates to move
continental drift
250 million years ago, the land masses of earth were clustered into one super continent called Pangea, as millions of years passed, Pangea broke apart and large pieces of land slowly moved away into the continents as we know them today
pieces of evidence for continental drift
- the Meosuarus
- continental jigsaw
- coal deposits
what types of crusts are found at divergent plate boundaries
- oceanic
- oceanic
what types of crusts are found at convergent plate boundaries
- oceanic
- continental
what types of crusts are found at collision plate boundaries
- continental
- continental
what types of crusts are found at conservative plate boundaries
- continental
- continental
types of plate boundaries
- divergent
- convergent
- collision
- conservative
movement of divergent plate boundaries
<— —> (plates move apart)
movement of convergent plate boundaries
one plate subducts under the other
movement of collision plate boundaries
—> <— (plates collide)
movement of conservative plate boundaries
plates slide past each other
hotspot volcano
an area of the Earth’s mantle from which hot plumes rise upward, forming volcanoes on the overlying crust
how to earthquakes happen
caused by the movement of tectonic plates found at fault lines (tectonic plate boundaries); energy is built up at fault lines
what are the two case studies
- earthquake Hatu
- earthquake Japan
seismic waves
vibrations that travel through Earth carrying the energy released during an earthquake (the earthquakes energy being released)
earthquakes magnitude
the amount of energy the earthquake releases
richer scale
the scale that rates an earthquakes magnitude based on the size of its seismic waves
composite volcano
- a tall volcano made up of lava and ash
- has violent eruptions
- lava is thick and moves slowly
- less frequent
shield volcano
- a small wide volcano
- not as violent eruptions
- lava is thin and runny and moved quickly
- more frequent
hotspot
A place in the centre of a plate where magma rises; this causes the lithosphere to melt and magma pushes through the cross the form volcanoes
crater
Opening at the top of volcano
magma chamber
Store of hot molten rock beneath the volcano
layers of ash and lava
Build up overtime to form sides of volcano
main vent
The tunnel in which magma rises to the top of the volcano secondary
secondary vent and cone
Allows magma to escape from the side of the volcano
Volcanic cloud
gas, steam and ash escaping from the volcano
volcanic bombs
Large pieces of rock ejected from the volcano
volcanic explosivity index
the measure of the destructive power of a volcano in the scale 1 to 8 (1 = non explosive, 8 = largest)
volcanic explosivity index
the measure of the destructive power of a volcano in the scale 1 to 8 (1 = non explosive, 8 = largest)
epicentre
The point on the Earth surface above the focus
focus
The point inside the crust where the pressure is released
seismometer
It’s measure and records seismic waves
continental jigsaw
continents match up like a jigsaw implying they were once connected
case of the mesosaurus
- fossil remains of the mesosaurus in South America and South Africa
- the mesosaurus was a freshwater reptile so it couldn’t of swam overseas so the countries had to be close together
coal deposits
- Alfred Wegner loaded the unusual deposits of coal in the South Polar regions
- The fossils of tropical plants in the form of cold deposits were found in Antarctica
- This led to the theory that this landmass was previously much closer to the equator where the climate is warmer and the lush vegetation could flourish
What tectonic activity do you find at divergent plate boundaries?
- As the plates move apart magma below escape from the mantle - this causes volcanoes
what tectonic activity do you find at convergent/destructive plate boundaries?
the denser oceanic crust is forced under the continental plate but the continental plate cannot be destroyed so it’s forced to make fold mountains - the oceanic plate melts this caused the magma to rise the surface through the fold mountains creating volcanoes.
what tectonic activity do you find at collision plate boundaries?
Big earthquakes, because there’s a massive buildup of friction and pressure
what tectonic activity will we find at conservative plate bound
earthquakes due to huge buildup of pressure between a two plates
what’s an example of a composite volcano
mount pinatubo
whats an example of a shield volcano
queen mary’s peak
what plate boundaries are composite volcanos found at
convergent
what plate boundary are shield volcanos found at
divergent
how does a tsunami form
1) destructive plate movement causes an earthquake
2) sea above the earthquake is forced upwards
3) sea movement causes tsunami
4) seismic waves spread quickly outwards
5) waves crash onto shore