3.1.5.2 Plate Tectonics Flashcards

1
Q

What’s the crust

A

Earth’s outer shell that we live on

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2
Q

2 types of crust

A

Oceanic

Continental

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3
Q

What’s the collective name for the crust + upper mantle where tectonic plates are formed

A

Lithosphere

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4
Q

What’s the widest section of the earth called (2900km thick)

A

Mantle

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5
Q

What’s the rock in the upper mantle like

A

Solid

Sit on top of asthenosphere

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6
Q

What’s the asthenosphere

What can it do

A

Layer of softer, plastic-like rock

Can move very slowly, carrying the lithosphere on top

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7
Q

What’s the lower mantle like

A

Most dense part of mantle

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8
Q

What’s the core

A

The centre + hottest part of the earth - reach 5000*c

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9
Q

What’s the core mostly made up of

A

Iron + nickel

Extremely dense

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10
Q

Describe 2 parts of the core

A

Outer core - semi-liquid and mainly iron

Inner core - solid + made of an iron-nickel alloy

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11
Q

What’s the earth’s main internal energy sources

A

The core - heat producing convection currents

Radioactive decay

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12
Q

What are the 2 theory’s for plate tectonics

A

Wegner’s theory of plate tectonics + continental drift

Hess’s theory of sea-floor spreading

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13
Q

Describe wegners theory

A

A single continent existed about 300 million years ago that he named Pangea + it then later split into 2 continents of Laurasia + Gondwanaland

Further splitting of these land masses formed today’s continents
This is the continental drift theory

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14
Q

What did Werner name the single continent

What 2 continents did it split into

A

Pangea

Laurasia
Gondwanaland

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15
Q

2 pieces biological evidence that supported wegners continental drift theory

A
  • fossil brachiopods found in Indian limestone are comparable with similar fossils in Australia
  • fossil remains of the mesosaurus reptile are found in South America + South Africa
  • fossiled remains of a plant that existed when coal was being formed have even located only in India + Antarctica
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16
Q

2 other pieces of evidence that support wegners theory

A
  • bulge of South America fitting into indent below west Africa
  • evidence of late-Carboniferous glaciation, deposits from this are found in South America, Antarctica + India
  • striations on rocks in Brazil + west Africa
  • rock sequences in northern Scotland agree closely with those found in eastern Canada
17
Q

What did Hess discover + study to suggest that sea-floor spreading was occuring

A

The mid-Atlantic ridge

18
Q

What’s Hess’ evidence sea-floor spreading was occuring

A

The alternating polarity of the rocks that form the oceanic crust

  • iron particles in lava on ocean floor are aligned with earth’s magnetic field
  • as lavas solidify, these particles give a permanent record for earth’s polarity at time of eruption
  • but at regular intervals, earth’s polarity reverses, resulting in a series of magnetic ‘stripes’ with rocks aligned alternatively towards north + south poles
19
Q

What pattern that Hess saw, suggests the oceanic crust is slowly spreading away from this boundary

A

The striped pattern, mirrored exactly on each side of the mid-oceanic ridge

20
Q

With distance from the mid-oceanic ridge, what happens to oceanic crust

A

It gets older

21
Q

What does sea-floor spreading imply

But what must actually be happening

A

Earth must be getting bigger

But actually, plates must be being destroyed somewhere to accommodate their increase in size at mid-oceanic ridges

22
Q

What are the 7 major plates

A
African plate
Antarctic plate
Eurasian plate
Pacific plate
Indo-Australian plate
North American plate
South American plate
23
Q

What are the 8 minor plates

A
Arabian plate
Caribbean plate
Cocos plate
Nazca plate
Juan de Fuca plate
Philippine sea plate
Scotia plate
Okhotsk plate
24
Q

3 plates where there are destructive margins

A

Pacific plate
South American plate
Caribbean plate

25
Q

2 plates that are diverging (constructive)

A

Pacific plate + Nazca plate

26
Q

Where’s the main collision margin

A

Arabian plate

27
Q

3 factors about the oceanic crust

A
  • thinner
  • young
  • heavier + more dense
28
Q

3 factors about the continental crust

A
  • thicker
  • older
  • lighter + less dense
29
Q

What’s the oceanic crust made up of

A

Basalt - silicon, magnesium + oxygen (SIMA)

30
Q

What’s the continental crust made up of

A

Granite - silicon, aluminium, oxygen (SIAL)

31
Q

What was the generally accepted view of plate movement

Explain

A

It’s due to convection currents

Convection currents Move apart -> plates move apart
Convection currents converge -> plates converge

32
Q

What’s ridge push

A

Forces pushing from the ridge, dragging plates down at trenches ‘ acting along sides of plate at conservative margins

33
Q

What produces the ocean ridge at constructive margins (ridge push)

A

Upwelling of hot magma at ocean ridges generates a buoyancy effect that produces ocean ridges, 2-3km above ocean floor

34
Q

What’s gravitational sliding

A

Due to gravity, oceanic plates experience a force that acts away from the ridge -> sliding away

35
Q

What’s slab pull

A

Cool,thick oceanic lithosphere is gravitationally unstable as it’s denser than the asthenosphere
As the plate descends under the continental plate, a gravity generated force pulls the whole oceanic plate down due to the plate’s negative buoyancy

36
Q

3 forces plates are controlled by

A

Convection currents
Ridge push + gravitational sliding
Slab pull