Types of Plate Margin Flashcards

1
Q

what types of margin do earthquakes and volcanoes occur at

A

constructive and destructive

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2
Q

where does a constructive plate margin occur

A

where two plates are moving apart (diverging)

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3
Q

how does a volcano form?

A

plates move apart, pressure is released at the margin, release of pressure causes mantle to melt, producing magma, magma is less dense than plate above, so it rises and can erupt to form a volcano

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4
Q

how does an earthquake occur?

A

plates don’t move in a uniform way - some parts move faster than others, causes pressure to build up, pressure becomes too much and plate cracks, makes a fault line, causes an earthquake. Further earthquakes can occur along the fault line once created.

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5
Q

what landforms occur at constructive plate margins

A

mid-ocean ridges and rift valleys

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6
Q

example of an ocean ridge

A

mid-atlantic ridge

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7
Q

what can form along mid-ocean ridges

A

underwater volcanoes, can build up to be above sea level e.g. iceland

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8
Q

how are rift valleys formed?

A
  • plates diverge beneath land, rising magma causes continental crust to bulge and fracture forming fault lines
  • crust between parallel fault lines drops when plates move apart to form a rift valley
  • as process continues, valley widens until it becomes a large basin that fills with sediment from the rift walls
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9
Q

where does a destructive plate margin occur

A

two plates moving towards each other (converging)

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10
Q

what occurs at a destructive oceanic-continental plate margin?

A
  • deep sea trench
  • fold mountains
  • volcanoes
  • earthquake
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11
Q

how is an ocean trench formed?

A
  • continental and oceanic crust converge, more dense oceanic crust is forced under less dense continental crust
  • seafloor and lithosphere bend and form a steep v-shaped depression
  • leading edge of a less-dense tectonic plate meets the leading edge off a dense plate
  • denser plate moves downwards into the subduction zone
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12
Q

what is an ocean trench?

A

are steep depressions in the deepest parts on the ocean where an old oceanic crust is pushed beneath either another oceanic plate or a continental plate

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13
Q

what is a mid-ocean ridge

A

an elevated region with a central valley on an ocean floor at a boundary between two diverging plates where crust forms from outpouring magma

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14
Q

what are the two processes concerning the formation of mid-ocean ridges

A

ridge-push and slab-pull

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15
Q

explain ridge-push (mid ocean ridges)

A

occurs when the growing bulk of the ridge pushes the rest of the tectonic plate away from the ridge, often towards the subduction zone

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16
Q

explain slab-pull (mid ocean ridges)

A

comes into effect in the subduction zone - is where the weights of the tectonic plate being subducted below the overlying plate dragging the rest of the plate along with it.

17
Q

what is a rift valley

A

a linear-shaped lowland between highlands or mountain ranges created by the action of a geologic fault

18
Q

what are fold mountains?

A

mountains formed from the folding of sedimentary rocks (sediment taken from rivers)

19
Q

how are fold mountains formed?

A
  • two plates pushed together, at compressing boundary
  • takes millions of years
  • compression zone, tectonic activity forces crustal compression at the edge of crust formation
  • rocks are often less stable and so more susceptible to folding
  • two plates force rock upwards into a series of folds
20
Q

how do volcanoes occur at destructive plate margins

A
  • oceanic crust is heated by friction and contact with upper mantle, this melts it into magma
  • magma is less dense than continental crust above and so rises to the surface - creates volcanoes
21
Q

how does an earthquake occur at a destructive plate margin

A
  • when one plate moves under another, it can get stuck
  • this causes pressure to build up
  • pressure becomes too much and so plates jerk past each other - causes earhtquake
22
Q

what occurs at a destructive oceanic-oceanic plate boundary

A
  • ocean trench
  • earthquakes
  • volcanic eruptions
  • island arcs
23
Q

processes occurring at oceanic-oceanic destructive plate margin

A

same processes occur as at continental-oceanic, two plates moving towards each other, the denser of the two will be subducted

forms ocean trench and triggers an earthquake and volcanic eruptions

24
Q

what creates an island arc

A

volcanic eruptions that take place under water

25
Q

what are island arcs

A

they are a curved chain of volcanic islands located at a destructive plate margin often with a deep ocean trench on the curved side

26
Q

how are island arcs formed

A
  • 2 convergent oceanic plates meet, one denser and heavier than the other, denser plate sinks under the other
  • oceanic lithosphere melts in the asthenosphere and turns into magma
  • some magma may leak into the crust and bubble up to the surface of the sea bed
  • when it bubbles volcanoes form at subduction zone and when they erupt they build up rock on the sea bed
  • overtime enough builds up to create a volcanic island that rises above the surface - look like islands
27
Q

what happens when two continental plates meet?

A

neither is subducted so no volcanoes form, but pressure builds up so earthquakes can form.

fold mountains occur when continental crusts converge e.g. Himalayas.

28
Q

what occurs at conservative plate margins

A

only earthquakes

29
Q

when does a conservative plate margin occur

A

when two plates are moving past eachother

30
Q

how does an earthquake occur at a conservative plate margin

A
  • two plates get locked together in places and pressure builds up
  • causes plates to jerk past each other (or crack forming fault lines)
  • releases energy as an earthquake
31
Q

example of conservative plate margin

A

pacific plate moving past the north american plate - many plates occur along this margin e.g. San Andreas fault