1.2 THEORETICAL FRAMWORKS AND PLATE MOV Flashcards

1
Q

what is the thin oceanic crust composed of?

A

-basalt

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2
Q

what is thicker continental crust composed of?

A

-granite

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3
Q

what does the earth’s mantle have?

A

-a temp gradient

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4
Q

in the upper mantle what are rocks like?

A

-cool
-brittle

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5
Q

in the lower mantle what are rocks like?

A

-hot
-plastic

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6
Q

in upper mantle how are earthquakes caused?

A

-bcoz the rocks are brittle enough to break and produce them

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7
Q

how are convection currents driven?

A

bcoz radioactive decay rises within the mantle, driving convection currents to then move tectonic plates

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8
Q

what is seafloor spreading?

A

-it occurs at divergent plate boundaries
-under the ocean
-it’s the continuous input of magma forming a mid-ocean ridge
-e.g mid-Atlantic ridge

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9
Q

what does gravity cause in terms of crusts?

A

-causes denser oceanic crust to be pulled down at site of subduction

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10
Q

what is slab pull?

A

-pulling force exerted by cold, dense oceanic plate plunging into mantle due to own weight

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11
Q

whats ridge push?

A

-proposed driving force for plate motion in plate tectonics
-occurring in mid-ocean ridges
-as a result of lithosphere sliding down the asthenosphere

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12
Q

what is the Benioff zone?

A

-an area of seismicity corresponding with the slab being thrust downwards in a subduction zone

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13
Q

palaeomagnetism? (4)

A

-results from zone of magma locking in the earths magnetic polarity when it cools
-scientists use this tool to determine historic periods of large scale techtonic activity
-through reconstruction of relative plate motions
-creating a geo timeline

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14
Q

subduction zones? (5)

A

-where 2 plates come together
-more dense oceanic plate subducts the continental plate
-2 plates lock together causing frictional stress
-causing failure along fault planes which results in a mega-thrust earthquake
-releasing strain energy and seismic waves

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15
Q

locked fault?

A

-fault that’s not flipping because the frictional resistance on fault is greater than shear stress across fault
-stress can be stored and then released as earthquakes
-e.g the 2004 Indian Ocean tsunami

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