2.2 Plate Tectonics Flashcards
What is lithosphere?
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
What are plate tectonics?
- The earth is broken up into a number of lithospheric plates
- The plates move via a process called continental drift
- 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
What is the earth’s structure?
Concentric structure based on chemical properties and mechanical behaviour
What are the earth’s chemical properties?
Crust
Mantle
Core
What is the earth’s mechanical behaviour?
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
What is the asthenosphere?
Composed of upper mantle
Weaker layer
Sits below the lithosphere
A ductile layer of the mantle which can flow allowing the plates to move
What are the key developments in the history of plate tectonics?
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
Where are the continental divergent plate boundaries?
Mid Atlantic ridge
East African Rift Valley leading across Indian Ocean
Boundary between Pacific plate and Nazca plate and Antarctic plate
How do divergent plate boundaries work?
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
Name the features that appear in oceanic divergent plate boundaries?
A layer of sediment Basalt Pillow lavas Dolerite dykes Homogeneous gabbro Layered gabbro Mantle peridotite
Explain the features of sediment in divergent boundaries?
Sediments are thinner near ridge where crust is younger
Thicker where crust is older as there is more time to accumulate
Explain the features of pillow lavas in divergent boundaries?
Lava erupting underwater
Inside remains molten and sinks to form teardrop
Outside cools rapidly
Explain the features of dolerite dykes in divergent plate boundaries?
Magma flows to the surface through fractures in the crust creating dykes and sills
Explain the features of homogeneous gabbro in divergent plate boundaries?
Formed in magma chambers below the ridge and pushed to either side
What are the magnetic anomalies in divergent boundaries?
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