Plate Tectonics Flashcards

1
Q

What are the 2 major types of tectonic plates?

A
  1. Oceanic plates
  2. Continental plates
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2
Q

What 3 landforms are created at constructive boundaries?

A
  1. Mid-ocean ridges (e.g., Mid-Atlantic Ridge).
  2. Rift valleys (e.g., East African Rift).
  3. Volcanoes due to rising magma.
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3
Q

What is the Pacific Ring of Fire? (Mention 2 things)

A
  • A tectonically active zone around the Pacific Ocean.
  • Contains 75% of the world’s volcanoes and 90% of earthquakes.
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4
Q

Explain what happens in the destructive plate margin in 5 steps?

A
  • Destructive margins happen when the oceanic plate slides beneath the continental plate.
  • Crust is destroyed as one plate dives under another at the subduction zone.
  • The rocks catch against each other as the plates are not smooth.
  • The pressure between plates builds until the plates can’t take the stress.
  • The plates slip past each other, which can cause both plates to move resulting in the ground shaking.
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5
Q

Explain what happens in the constructive plate margin in 5 steps?

A
  • At constructive plate margins, the plates move apart (diverge).
  • The convection currents diverge (push apart) and cause a gap between the plates.
  • Magma rises up to fill the gap that is created.
  • New crust is generated as the plates pull away from each other.
  • Rift valleys are created when the crust pulls apart, and land drops to create a valley.
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6
Q

Explain what happens in the conservative plate margin in 5 steps?

A
  • At conservative plate margins, plates are sliding past each other horizontally.
  • Crust is neither produced nor destroyed.
  • The plates are made of rock that has jagged edges so they catch and snag against one another.
  • Friction and pressure between the plates builds until the plates can’t take the stress.
  • The plates slip past each other, which can cause both plates to move resulting in the ground shaking.
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7
Q

What are the 4 features of oceanic plates?

A
  • High-density materials.
  • Made of basaltic rock.
  • Only 7-10 km thick.
  • Oceanic plates can sink (subduct) under other plates.
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8
Q

What are the 4 features of continental plates?

A
  • Thicker (25-75 km) than oceanic plates.
  • Less dense than oceanic plates.
  • Made of granitic rock.
  • Continental plates do NOT sink (subduct).
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9
Q

What 4 landforms are created at destructive boundaries?

A
  • young fold mountains (e.g. Himalayas)
  • deep sea trenches
  • island arcs
  • volcanoes
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10
Q

What is a tectonic hazard?

A

A hazard is a natural/geophysical event that has the potential to threaten both life and property.

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11
Q

What is a hotspot?

A

An area where a hot plume of magma rises from deep in the mantle.

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12
Q

How do hotspots form volcanic islands in 3 steps?

A
  1. It pushes through a weakness in a tectonic plate, forming volcanoes.
  2. As the plate moves over the hotspot, new volcanoes form, creating a chain of volcanic islands.
  3. The Hawaiian Islands were all formed by a mid-Pacific hotspot.
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13
Q

How do intra-plate volcanoes form in 3 steps?

A
  • Isolated plumes of convecting heat (mantle plumes) rise towards the surface generating basaltic volcanoes.
  • The plume remains stationary, although the tectonic plate above moves slowly over it.
  • Continuing plate movement over time produces a chain of volcanic islands, with extinct ones furthest from the plume location.
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14
Q

Give an example of intra-plate volcanoes?

A

Hawaii

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15
Q

How are intra-plate earthquakes form?

A

Zones of weaknesses are created as plates move and stresses increase

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16
Q

What are the 4 segments of the earth’s internal structure (in ascending order)?

A

1) The core
2) The mantle
3) The asthenosphere
4) The lithosphere

17
Q

What is the core?

A

The core is the central part of the Earth. It is solid at the centre and more liquid further away. It’s a source of radioactive heat.

18
Q

What is the mantle?

A

The mantle is a semi-molten body of rock between the Earth’s crust and its core

19
Q

What is the asthenosphere?

A

The asthenosphere is the upper part of the mantle.

20
Q

What is the lithosphere?

A

The lithosphere is the crust and upper mantle (80-90 km thick) which form the tectonic plates.

21
Q

What are the 5 theories of plate tectonics?

A

1) Wegener’s Continental Drift
2) Holmes’ Hypothesis
3) Sea floor spreading
4) Gravitational Sliding
5) Slab pull

22
Q

What does Wegener’s continental drift talk about?

A

In 1912, he said that our now separate continents had once been joined together as a supercontinent (Pangea)

23
Q

What does Holmes’ Hypothesis talk about?

A

He said that the Earth’s internal radioactive heat was the driving force of convection currents in the mantle that could move tectonic plates.

24
Q

What does Sea Floor Spreading talk about (2 facts)?

A
  • In the 1960s, there was a discovery of magnetic stripes in the oceanic crust of the seabed.
  • Palaeomagnetic signals from past reversals of the Earth’s magnetic field prove that new crust is created by the process of seafloor spreading at mid-ocean ridges.
25
What does Gravitational sliding talk about?
Elevated altitudes of oceanic crust at ridges at divergent plate boundaries – create a ‘slope’ down which oceanic plates slide (gravitational sliding).
26
What does Slab Pull talk about?
At convergent boundaries, high density ocean floor is being dragged down by a downward gravitational force (slab pull) beneath the adjoining continental crust.
27
What are the 4 different plate margins:
1) constructive 2) destructive 3) collisions 4) conservative
28
What are processes like in construction margins?
- Volcanic eruptions at constructive plate margins are basaltic and produce low viscosity lava. - Earthquakes at constructive plate margins are low magnitude and shallow-focus (less than 70 km deep).
29
What are processes like in destructive margins?
- Deep sea trenches and fold mountain ranges often form at destructive plate margins. - Volcanic activity at destructive plate margins is often violent due to the high viscosity lava. - Earthquakes at destructive plate margins are high magnitude, deep-focus (up to 700 km deep) and frequent.
30
What are processes like in collision margins?
- There is no volcanic activity at collision plate margins. - Earthquakes at collision plate margins are rare - when they do happen, they are high magnitude and shallow-focus (less than 70 km deep).
31
What are processes like in conservative margins?
- There is no volcanic activity at transform plate margins. - Earthquakes at transform plate margins are high magnitude, shallow-focus (less than 70 km deep) and a common occurrence.
32
What are collision plate margins?
Collision plate margins are characterised by the meeting of two continental landmasses resulting in the formation of a fold mountain belt.