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Describe the nature of the continental crust
35-70km thick
1500 m years old
Granite composition
Rich in silicon, aluminium
LESS DENSE, LIGHT COLOUR
list all the movements of tectonic plates:
Convection theory
Hotspot
Ridge push
Slap pull
Explain convection theory
radioactive decay in earths core produces heat.
Hot magma rises in convection currents
Cools at surface
Sinks as denser.
Explain convection theory
radioactive decay in earths core produces heat.
Hot magma rises in convection currents
Cools at surface
Sinks as denser.
Ridge push - explain:
magma intrusion at ocean spreading ridges, which propels the two plates apart.
Explain slab pull:
the force that the sinking (colder and denser oceanic crust) edge of the plate exerts on the rest of the plate. So gravity forces down
List all the types of plate boundaries and give a location
oceanic constructive [Mid Atlantic ridge] N.American and Eurasian plate
Continental constructive [Mid Atlantic Ridge]
Oceanic/continental destructive [Nazca subduction under S.American plate]
Oceanic destructive [japanese arcs- PACIFIC PLATE UNDER PHILIPINNES PLATE]
Continental-continental convergent [The Himalayas - follows complete destruction of oceanic plate so continental converges with continental - neither subduct]
Conservative [san andreas fault]
List all the types of plate boundaries and give a location
oceanic constructive [Mid Atlantic ridge] N.American and Eurasian plate
Continental constructive [Mid Atlantic Ridge]
Oceanic/continental destructive [Nazca subduction under S.American plate]
Oceanic destructive [japanese arcs- PACIFIC PLATE UNDER PHILIPINNES PLATE]
Continental-continental convergent [The Himalayas - follows complete destruction of oceanic plate so continental converges with continental - neither subduct]
Conservative [san andreas fault]
Explain how constructive boundaries form - oceanic (under the ocean)
Plates pull apart. / divergent as rising convection currents within mantle spread sideways forcing plates apart creating a rift. Through which molten basal comes to surface along fissure eruptions and through volcanoes. magma then cools and solidifies.
Transform fault: created at 90 degrees to ridge due to variations at which sea floor is spreading - get sheered apart.
example: N.American pull apart from Eurasian plate
explain how constructive/ divergent plat boundaries occur continental -continental (rift valley)
magma rises up and it pushes up the earth's crust → ridge created due to expansion or crust and pressure.
The land in middle (parallel fault lines) forced apart → rift valley
Volcanoes form where magma rises → graben
Example: MID ATLANTIC RIDGE
/destructive boundaries - oceanic-oceanic
1) more dense crust subduction under other crust or the one that’s moving faster
2) slab pull
3) forms oceanic trench + island arc/ chain of volcanoes
example: pacific plate subduction under phillipense plate
Japanese arc islands
Destructive plate boundaries - continental - oceanic
1) oceanic plate more dense subducts
2) Ridge push, slab pull and conventional drag
3) tension and sudden release of friction = earthquake
4) Sediment compress and uplift to form FOLD MOUNTAINS
Oceanic trench + volcanoes
EXAMPLE: NAZCA PLATE AND S.A PLATE
Fold mountains = the Andes
Convergent continental-continental
1) following destruction of oceanic crust
2) converge
Neither subducts and uplift
Himalayas mountains = fold mountains
Explain what happens at the conservative boundary
1) convection currents in mantel
2) parallel plates move in opposing direction or at different speeds
3) Pressure builds up
4) oceanic crust displace water
5) continental = fault index and earthquakes form sudden release of pressure after being stuck
EXAMPLE: San Andreas fault
Pacific plate moving NW
N.A plate moving NW but slower
Nature of oceanic plate
Denser
Older
Crust/Lithosphere
Outermost layer
Continental and Oceanic crust
Mantle/ asthenosphere
A layer of hot melted rock
Core
inner core solid nickel
Outer core molten lower density