Global Tectonics: Plates and Plumes Flashcards

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1
Q

How does continental drift relate to plate tectonics?

A

Wegner saw the continents as a jigsaw puzzle that fit together into a prior single supercontinent, Pangea, surrounded by the sea Panthalassa

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2
Q

The earth is made up of what 3 layers?

A
  • core
  • mantle
  • crust
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3
Q

The crust:

A
  • Is where we live
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4
Q

The Earth’s crust is made of:

A
  • Continental and Oceanic crust
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5
Q

Continental crust

A
  • 10-70km thick
  • Buoyant (less dense than oceanic)
  • Mostly old
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6
Q

Oceanic Crust

A
  • Thin (~7km)
  • Dense (sinks under continental crust
  • Young
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7
Q

How many plates is the earths crust divided in to?

A

The earth is divided into 12 major plates which are moved in various directions

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8
Q

What does the word tectonic refer to?

A

It refers to the deformation of the crust as a consequence of plate interaction

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9
Q

Plates are made of:

A

rigid lithosphere

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10
Q

What lies beneath the tectonic plates?

A
  • The asthenosphere
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11
Q

The lithosphere makes up:

A

The tectonic plates

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12
Q

Plate Movement

A

Plates of lithosphere are moved around by the underlying hot mantle connection cells

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13
Q

Plate Tectonic Theory

A
  • Strong lithospheric plates move atop the weaker, plastic asthenosphere
  • Deformation occurs at or near the edges of plates where they interact with other plates
  • The interiors of the plates are relatively undeformed
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14
Q

Three types of plate boundary:

A
  • Divergent
  • Convergent
  • Transform
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15
Q

Divergent plate boundaries

A
  • Show the creation of new oceanic lithosphere from the upwelling mafic magmas as well as a widening of the ocean basin
    Eg.) Iceland is an example of a mid-ocean ridge exposed above sea level - widening at the rate of ~4 mm/year
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16
Q

Convergent Boundaries

A

Three types:

  • Continent-oceanic crust collision
  • Ocean-ocean collision
  • Continent-continent collision
17
Q

Oceanic-continental boundary

A
  • Much of the western boundary of South America is this type of boundary.
  • Denser oceanic lithosphere flexes under the less dense, much older, continental crust.
  • When oceanic and continental plates converge, the oceanic plate must subduct beneath the continental plate because the density of thick continental crust is too low to permit it to sink into the asthenosphere
18
Q

Oceanic-oceanic boundary

A
  • When a convergent boundary forms between plates of oceanic lithosphere, the plate that is older, thicker, and denser subduct the less dense plate.
  • Several areas of the western Pacific typify this boundary, such as the area around Japan
19
Q

How is a Subduction Zone formed?

A

They are formed when two oceanic plates collide. One runs over the other which causes it to sink into the mantle

20
Q

Continental-continental boundaries

A

When subduction brings two continents together limited subduction may occur, but the buoyancy of continental crus eventually stops the subduction. The contraction of crust in the collision zone doubles the thickness of continental crust and creates high mountains.

21
Q

Volcanoes are formed by:

A
  • Subduction
  • Rifting
  • Hotspots
22
Q

Hotspots

A
  • Form where narrow columns (plumes) of unusually hot mantle convectively rise from the core-mantle boundary
  • They leave tracks on moving plates.
23
Q

Plumes

A

are an upwelling of abnormally hot rock within earths mantle. They are stationary in the mantle and other data indicates that they move slowly, if at all