Plate tectonics (KQ1) Flashcards

1
Q

What is the internal structure of the earth made up of?

A
  • crust
  • lithosphere
  • mantle
  • aesthenosphere
  • core
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2
Q

What is the outermost layer of the earth made up of?

A
  • basalt
  • granite
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3
Q

How thick is the outermost layer of the earth?

A
  • varies from a few km to more than 70km thick
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4
Q

What is the lithosphere made of?

A
  • crust

- uppermost mantle

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5
Q

What is the mantle made up of (other than lithosphere)?

A
  • aesthenosphere

- mostly solid rock that flows under high temperatures and pressure

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6
Q

How thick is the mantle?

A
  • about 2500km thick
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7
Q

What is the temperature of the mantle?

A
  • between 800 to 3000 degrees celsius
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8
Q

What is the core made up of?

A
  • iron
  • nickel
  • separated into liquid outer core and solid inner core
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9
Q

How thick is the core?

A
  • about 3300km thick
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10
Q

What is the temperature of the core?

A
  • between 3000 to 5000 degrees celsius
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11
Q

What are the two different types of crust?

A
  • oceanic
  • continental
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12
Q

Where is the oceanic crust located?

A
  • beneath deep oceans
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13
Q

Where is the continental crust located?

A
  • beneath the earth’s land masses
  • under shallow seas close to continents
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14
Q

What are some characteristics of the oceanic crust?

A
  • denser (basalt)

- thinner (between 5-8km)

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15
Q

What are some characteristics of continental crust?

A
  • less dense (granite)
  • thicker (35-70km)
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16
Q

Why do tectonic plates move?

A
  • plate movement is caused by a combination of convection currents and slab-pull force
  • movement of convection currents refer to the movement of heat within the mantle
17
Q

How do convection currents cause plate movement?

A
  • as the mantle is heated by the core, the material expands, rises and spreads out beneath the plates
  • this pulls the plates apart as they are dragged along
  • as mantle material spreads further, it cools and sinks, pulling the plates along
  • the sinking mantle material heats up again as it nears the core, repeating the entire process
18
Q

How does slab-pull force cause plate movement?

A
  • as denser oceanic plates sink at the subduction zone, it pulls the rest of the plate
  • this process is known as slab-pull force (pulling force exerted by a dense oceanic plate plunging into the mantle due to its own weight)
19
Q

What happens when oceanic-oceanic plates diverge?

A
  • magma rises from the mantle to fill the gap between the plates as they diverge
  • a new seafloor is formed when lava flows out onto the seafloor and then cools and solidifies (seafloor spreading
  • it then forms a mid-oceanic ridge
20
Q

What are some characteristics of divergent oceanic-oceanic plate type?

A
  • newly formed (youngest) rocks are closest to the middle of the ridge
  • at various points along the ridge, magma builds up above the ocean to form volcanic islands
21
Q

What are some examples of landforms caused by 2 oceanic plates diverging around the world?

A
  • iceland

- mid-atlantic ridge found in the middle of the atlantic ocean

22
Q

What happens when continental-continental plates diverge?

A
  • when plates diverge, they are stretched
  • this causes fractures at the plate boundary
  • the land in between the 2 continental plates then sinks to form a linear depression (rift valley)
  • this divergence can cause continents to break apart
23
Q

What are some examples of landforms around the world caused by continental plates diverging?

A
  • East African Rift Valley
24
Q

What happens when 2 oceanic plates converge?

A
  • denser plate subducts beneath the less dense plate
  • a deep oceanic trench is formed at the point of subduction
  • subducted oceanic plates causes the mantle material above it to melt, forming magma
  • magma rises through the cracks to form a volcano and eventually, a chain of islands
  • earthquakes may occur due to friction
25
Q

What are some examples of landforms around the world caused by 2 oceanic plates converging?

A
  • marina trench
  • marina islands (eventually)
26
Q

What happens when continental-continental plates converge?

A
  • little to no subduction occurs due to both plates being too thick & buoyant
  • layers of rock on the upper part of the crust are compressed together
  • this causes them to fold upwards or sideways, forming fold mountains
27
Q

What are some examples of landforms that form when 2 continental plates converge?

A
  • Himalayas
28
Q

What happens when oceanic-continental plates converge?

A
  • denser oceanic plate subducts
  • oceanic trench forms at the subduction zone while fold mountains form on the continental plate
  • volcanoes are also formed on the continental plate when magma rises through the cracks to the surface
  • earthquakes may occur
29
Q

What are some examples of landforms caused by oceanic and continental plates converging around the world?

A
  • The Andes, Chile
30
Q

What are transform plate boundaries?

A
  • where plates slide past each other, resulting in a transform fault
  • tremendous stress builds up and is eventually released as an earthquake
31
Q

What are some examples around the world of landforms caused by transform plate boundaries?

A
  • San Andreas fault between the pacific and north American plates