Plate tectonics Flashcards

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1
Q

What is the thickness of the crust like?

A

Varies in thickness:
Under ocean: 5-20km
Under continents: 70km

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2
Q

Describe 4 characteristics of the continental crust.

A
  • 30-70km thick
  • over 1500 million years old
  • Less dense than the oceanic crust
  • Mainly granite rock (sial)
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3
Q

Describe 4 characteristics of the oceanic crust.

A
  • 6-10km
  • Less than 200 million years old
  • More dense than the continental crust
  • Mainly basalt rock (sima)
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4
Q

What is the moho boundary?

A

The boundary zone between the earth’s crust and the mantle. In this section, there is a change in seismic wave velocity.

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5
Q

Describe the lithosphere.

A
  • the rigid upper section of the crust
  • 80-90km thick
  • Made from tectonic plates (oceanic and continental)
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6
Q

What is the asthenosphere?

A

The layer beneath the lithosphere which is semi-molten on which tectonic plates constantly move due to convection currents.

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7
Q

Describe 3 characteristics of the mantle.

A
  1. The mantle gets close to melting but does not due to the geothermal gradient.
  2. Widest section of the earth (2900km thick)
  3. Semi-molten state due to silicate rock content
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8
Q

How is the upper mantle different to the lower mantle?

A

In the upper mantle, the rocks are solid whereas in the lower mantle (asthenosphere) there is softer plastic which moves very slowly.

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9
Q

Where is the lithosphere situated?

A

On top of the asthenosphere.

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10
Q

Describe 3 characteristics of the inner core.

A
  1. Solid ball of iron and nickel
  2. Responsible for the Earth’s internal heat due to energy released by radioactive decay.
  3. 1,250 km-thick
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11
Q

Describe 3 characteristics of the outer core.

A
  1. Semi-molten state
  2. 2,200 km-thick
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12
Q

Describe 3 characteristics of the asthenosphere.

A
  1. Extends from 100 km down to 300 km
  2. Within the asthenosphere convection currents exist
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13
Q

What is the Earth’s heat engine (the source of the Earth’s internal heat)?

A

Radiogenic heat is released due to the radioactive decay of isotopes which releases energy in the form of heat. When this migrates to the earth’s surface, convection currents are formed.

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