Tectonics: Earth's Structure + Plate Movement Theoretical Framework Flashcards

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1
Q

Describe the continent lithosphere 

A

Up to 70 km, thick, solid, less dense 2.8 g/cm³ Granite

O and S waves thro

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2
Q

Describe oceanic lithosphere

A

Up to 7 km, thick solid denser 3.3 g/cm³. Basalt, P and S waves pass through 

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3
Q

Describe the mantle

A

Solid but plastic with different densities made of periodite silica, rich Rock

P and S waves pass through a variable rates due to changes in density

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4
Q

Describe outer core

A

Liquid, dense, 12% sulphur, 88% iron only P-waves past thro high temperature

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5
Q

Describe inner core

A

Solid densest, hottest 20% nickel, 80% iron

only P waves reach the inner core and pass thro

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6
Q

What heats up the inner core?

A

Residual heat and radioactive decay

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7
Q

What three mechanisms move plates?

A

Convection current slab, pull ridge push

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8
Q

How to convection currents occur

A

Core is hot and heats up surrounding magma which makes it less dense. This causes the rock or magma to rise as it rises it cools down, gets denser- as sinks it pushes against the plates, helping them move.

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9
Q

What is slab pull?

A

As a plate subducts its weight pulls, the rest of plate along - the more that is subducting the greater the force of the pull

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10
Q

What is ridge push?

A

As magma make its way to the surface and pushes through it separates and pushes against the surrounding plate

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11
Q

evidence for continental drift - biological

A

fossil remains across continents e.g. mesosaurus fresh water species fossil remains in south afric and brazil - can’t have swam across salt sea

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12
Q

evidence for continental drift -climatological

A

carboniferous limestone pennines and uk coal deposists need high temp and wet - fast decomp - suggests Eng was in tropics

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13
Q

evidence for continental drift - geological

A

mount ranges across continents - Appalachian (NA) and Caledonian (Scandenavia and UK)

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14
Q

what is the plate tectonic theory

A

earths surface is made up of plates which move relative to each other at diff speeds or directions. The boundaries btw plates are zone of tectonic activity like seismicity, vulcanity and mountain building

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15
Q

Wadatti Benioff
Date
Idea
Significance

A

1920
EQ at Wadatti Benioff due to subduction - zone where plates no longer exist
Explains EQs

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16
Q

Mantle Convection Current

A
17
Q

Evidence for seafloor spreading

A

Magnetic properties of the erupted basalt
earths magnetic field have been shown to flip occasionally so north and south pole swap
salts contains minute magnetic minerals and this changes directions depending on the earths magnetic field at the time of eruption 

18
Q

magnetic stripes

A

Polarity reversal from rock formations at the, mid-Atlantic ridge 

19
Q

Arthur Holmes, date, hypothesis and critique

A

1927 British geologist, he suggested convection currents. As a reason for continental drift. He suggest a radioactive decay generate enough heat for convection currents. As mantle is not exact same temperature throughout. Heat not evenly distributed, causing a magma to sink and rise

Holmes taken seriously as he had no real evidence.

20
Q

Harry Hess theory, date, evidence and hypothesis and critique

A

1961 seafloor spreading hypothesis

Using naval submarine detection technology recorded young age is four pieces on or near ridges are much older ages for ocean rock near the continental masses began to theorise that made ocean ridges. Mark structurally weak spots are in the ocean floor is being pushed to either side, new magma from deep within the Earth rises easily for this weak spots and eventually creates new seafloor

Critique is if new ocean floor is continually being made, why has earth not expanded

21
Q

Frederick, Vine and Drummond, Matthews, date, theory and significance

A

1963 theory of palaeomagnetism repeated reversals of earths magnetic field

as underwater volcanic, eruption occurred and the basaltic lava entries intrudes crust during the cooling process process. Particles of iron oxide align themselves along the earths magnetic field, which provides a permanent record of the polarity at the time which alternates approximately every 200,000 400,000 years creating a series of magnetic stripes with rocks aligned. this can be used to age the rocks

deep ocean trenches cut across existing magnetic anomalies. The boundary between the ages of lithosphere suggest that older or denser oceanic crust subducts, which provides an explanation to Hess’s greatest critique.

22
Q

Tuzo Wilson, date, theory and significance

A

Propose the Conservative plate Boundry - fault slips, horizontally, connecting oceanic ridges divergent plate, boundaries to ocean trenches of convergent boundaries. They were consider the last puzzle of the tectonic theory .

Explained the earthquakes and tectonic activity is that occur around these plate boundaries.

23
Q

Dan McKenzie year and contribution

A

Professor Vidya, physics and University of Cambridge, 1966,

use mathematical evidence to back up the theory

McKenzie modeled generation of magma at both mid ocean ridges and mantle plumes and helped us understand factors controlling partial, melting and

used knowledge of math physics and thermodynamics to understand the mechanisms for Earth cast movement.