2.2 Plate Tectonics Flashcards

1
Q

What is lithosphere?

A

The solid upper portion of the mantle and crust
Most rigid of earth’s layers
Coolest of earth’s layers
Divided into the world’s tectonic plates

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2
Q

What are plate tectonics?

A
  1. The earth is broken up into a number of lithospheric plates
  2. The plates move via a process called continental drift
  3. There are 3 types of plate boundaries:
    A) Conservative - sliding past each other
    B ) Convergent - moving towards each other
    C) Divergent- moving away from each other
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3
Q

What is the earth’s structure?

A

Concentric structure based on chemical properties and mechanical behaviour

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4
Q

What are the earth’s chemical properties?

A

Crust
Mantle
Core

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5
Q

What is the earth’s mechanical behaviour?

A

The lithosphere is underlaid by asthenosphere.
The lithosphere is divided into tectonic plates which move relative to one another by mechanisms not yet completely understood

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6
Q

What is the asthenosphere?

A

Composed of upper mantle
Weaker layer
Sits below the lithosphere
A ductile layer of the mantle which can flow allowing the plates to move

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7
Q

What are the key developments in the history of plate tectonics?

A

1912- Wegener releases ‘continental drift’ articles - saw a jigsaw
1915 - Releases Origin of Continents and Oceans - suggests drift from fossil similarity
1959 - Hess releases ‘history of ocean basins’ - sea floor spreads to create flat top mountains called guyots- thought all crust moved rather than individual sections
1963 - Tested sea floor spreading causing switch of magnetic fields
1963 - Tuzo - Wilson suggested mantle hot spots causing volcanic island chains like Hawaii
1965 - Suggests conservative plate boundaries eg San Andreas fault
1966 - Mackenzie released ‘the viscosity of the lower mantle’ controlling plate tectonics
1993 - Wilson suggests slab pull force as primary force of plate motion
2002 - Conrad and lithgow bertelloni support slab pull dominance
2006 - New sea spread idea of symmetrical and asymmetrical spreading to different ridges

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8
Q

Where are the continental divergent plate boundaries?

A

Mid Atlantic ridge
East African Rift Valley leading across Indian Ocean
Boundary between Pacific plate and Nazca plate and Antarctic plate

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9
Q

How do divergent plate boundaries work?

A

Rising hot material and extensional forces cause crust and lithosphere to become thinner
Volcanoes are produced due to rising magma from partial melting of mantle and mafic magma and basalt lava rises
These are footwall upthrown normal faults - FUN faults

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10
Q

Name the features that appear in oceanic divergent plate boundaries?

A
A layer of sediment 
Basalt Pillow lavas
Dolerite dykes
Homogeneous gabbro 
Layered gabbro
Mantle peridotite
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11
Q

Explain the features of sediment in divergent boundaries?

A

Sediments are thinner near ridge where crust is younger

Thicker where crust is older as there is more time to accumulate

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12
Q

Explain the features of pillow lavas in divergent boundaries?

A

Lava erupting underwater
Inside remains molten and sinks to form teardrop
Outside cools rapidly

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13
Q

Explain the features of dolerite dykes in divergent plate boundaries?

A

Magma flows to the surface through fractures in the crust creating dykes and sills

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14
Q

Explain the features of homogeneous gabbro in divergent plate boundaries?

A

Formed in magma chambers below the ridge and pushed to either side

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15
Q

What are the magnetic anomalies in divergent boundaries?

A

Lava erupts and magnetic fields of minerals go in different directions
The magnetic fields of minerals are all aligned in the same direction as the earth’s magnetic field
The lava cools below the current temperature and magnetic fields are locked in place
Newer material nearest to the ridge, older material has moved away making strips of reverse polarity
Not perfectly symmetrical as it depends how lava flows

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16
Q

How do convergent plate boundaries work -> oceanic - continental plate boundary?

A

Example of continental plate boundary is the Andes
Oceanic lithosphere subducts beneath continental plate because it is more dense
Regional metamorphism due to high temperature and pressure causes rocks to recrystallise
Deep focus earthquakes as subducting lithosphere fractures as it forces its way into asthenosphere
Shallow focus earthquakes occur due to build up and release of 2 plates against each other

17
Q

How does the convergent boundary work -> when oceanic plates meet?

A

Older and denser plate subducts
Ocean trench forms on the side of subducting plate
Partial melting of subducting mafic ocean crust leads to intermediate magmas - this causes andesite lava and explosive eruptions

18
Q

Explain the features of convergent plate boundaries -> continental - continental plates?

A

Eg Eurasia and India - Himalayas
Historic Tethys sea - where marine fossils are found
No subduction because both plates have same composition and density
Marginal ocean sediments formed upwards creating mountains
Shallow focus earthquakes close to rising surface
Folding occurs deeper where rocks are hotter
Silicic Magma produced but deep and rarely erupts at surface
Widespread regional metamorphism

19
Q

Explain symmetric spreading at the mid ocean ridge?

A

Material is created due to partial melting of mantle

New material moves away due to plate movement

20
Q

Explain asymmetric spreading in the ocean core complex?

A

Slow plate movement causes magma production to stop
Spreading continues; large scale FUN faults known as detachment faults form uplifting large amounts of mantle rocks onto the sea floor

21
Q

What is lithospheric drag and is it effective?

A

Occurs at convergent plate boundaries
Converting asthenosphere drags lithosphere down
Not the most effective movement

22
Q

What is slab pull and is it effective?

A

Denser plate subducts and pulls rest of the plate with it

It is effective

23
Q

What is ridge push and is it effective?

A

The ridge pushes the plates away
New material pushes plate away from the ridge
Not the most effective movement