Emergence of ocean basins

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12 Terms

1
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Who was the first person to propose the theory of continental drift

Alfred Wagner - the theory was largely rejected due to lack of mechanism explanation

2
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Where is the oceanic crust formed and destroyed

Formed at the spreading centre, destroyed by melting following subduction

3
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What drives convection cells in the asthenosphere

Heat from radioactive decay

4
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What are 4 observations directly related to crustal motion

Geographical variability of crustal heat flow, geographical variability of the thickness of deep-sea sediment, geographical location, magnetic anomalies

5
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How do heat flow measurements change with distance from the spreading centre

Decreases in temperature away from the spreading centre

6
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Where are earthquake epicentres concentrated along

Ocean ridged, transform faults, trenches, volcanic island arcs,

7
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How does earthquake magnitude change a different positions on the sea floor

Highest at trenches due to impression from subduction

lowest at ridges due to spreading

8
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What 2 factors show decreasing heat flow through the ocean crust

Increasing distance from the spreading surface

Increasing age of crust

9
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What does the Vine-Matthews-Morley hypothesis show records of

Record of reversals in basaltic rock

10
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What does the VMM hypothesis state

New ocean crust is formed at ocean ridges and magnetic orientation is reserved

Therefore

Magnetometer records should reveal magnetic anomalies and should show a stride pattern parallel to the ridges

11
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What is the Hawaiian island chain an example of

Oceanic crust moving over stationary hotspots

12
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What happens to young vs old islands in the Hawaiian

Younger islands are active, whilst older islands subside as they cool