1/11
Looks like no tags are added yet.
Name | Mastery | Learn | Test | Matching | Spaced |
---|
No study sessions yet.
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
Where is the oceanic crust formed and destroyed
Formed at the spreading centre, destroyed by melting following subduction
What drives convection cells in the asthenosphere
Heat from radioactive decay
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
How do heat flow measurements change with distance from the spreading centre
Decreases in temperature away from the spreading centre
Where are earthquake epicentres concentrated along
Ocean ridged, transform faults, trenches, volcanic island arcs,
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
What 2 factors show decreasing heat flow through the ocean crust
Increasing distance from the spreading surface
Increasing age of crust
What does the Vine-Matthews-Morley hypothesis show records of
Record of reversals in basaltic rock
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
What is the Hawaiian island chain an example of
Oceanic crust moving over stationary hotspots
What happens to young vs old islands in the Hawaiian
Younger islands are active, whilst older islands subside as they cool