Year 11 Plate Tectonics Flashcards

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1
Q

Crust

A

Solid, hard outer shell

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2
Q

Mantle

A

Soft molten rock about 3800*C

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3
Q

Outer core

A

Liquid iron and nickel

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4
Q

Inner core

A

Combination of nickel and iron, solid, up to 5500*C

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5
Q

How do we know about the different layers that exist

A

Because the seismic waves are refracted and travel at different speeds which gives us an image

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6
Q
Continental crust:
Where?
Thickness?
Density?
Age?
Rock type?
A

Lies under continental land masses
25-100km thick
less dense, doesn’t sink
3-4 billion years old
new crust never formed and can’t be destroyed
Granite with large crystals, as rock cools slowly

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7
Q
Oceanic crust
Where?
Thickness?
Density?
Age?
Rock type?
A

Lies under oceab
5-10km thick
more dense, sinks into mantle when meets continental
Oldest only 180 million years old
Constantly formed at constructive boundaries where it’s destroyed
Basalt with small crystals as cools quickly

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8
Q

What are tectonic plates

A

Large sections of the Earth’s crust able to move separately from each other

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9
Q

Conservative margin: what? Earthquakes? Volcanoes? Example

A

Plates more past each other, Earthquakes, no volcanoes e.g. Haiti Earthquake 2010 American and Caribbean

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10
Q

Constructive margin: what? Earthquakes? Volcanoes? Example

A

Plates move apart, earthquakes and volcanoes e.g. Iceland, Eurasian and n’ American

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11
Q

Destructive margin: what? Earthquakes? Volcanoes? Example

A

Plates moving together, earthquakes and volcanoes e.g. Chile earthquake 2010 Nazca and s.American plate

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12
Q

Why do plates move

A

Convection current, as magma heated it rises, as it rises it cool so sinks again causing the plates above to move

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13
Q

What’s ridge push

A

As the lithosphere cools, it becomes denser and starts to slide down, away from the ridge, causing the plates to diverge

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14
Q

What’s slab pull

A

At destructive margins, the denser plate subducts down into the mantle due to gravity/ This motion pulls the rest of the plate along with it

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15
Q

What happens at constructive plate boundaries

A

As plates slowly move apart, magma rises to earth’s surface, it cools and solidifies forming new igneous rock. Eventually rock builds up forming a shield volcano, some so large they form islands such as Iceland

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16
Q

What happens at destructive plate boundaries (continental and oceanic)

A

Oceanic plate denser so forced beneath continental, know as subduction zone. As subducted, it melts forming magma and earthquakes triggered. Magma collects and rises up through cracks, building up pressure, triggering volcanic eruptions. Fold mountains formed at subduction zones e.g. Andes

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17
Q

What happens at destructive plate boundaries (oceanic and oceanic)

A

The older, denser oceanic slap is force under the other, creating a trench at subduction zone. Volcanoes formed and earthquakes, same as c+o e.g Pacific and n.American plate

18
Q

What’s the Pacific ring of fire

A

An area of high seismic and volcanic activity around the Pacific ocean. There are many destructive margins around the Pacific plate which creates tectonic activity

19
Q

What happens when two continental plates converge

A

Both plates have the same density so both pushed upwards forming mountain ranges. Magma can’s penetrate the thick crust so no volcanoes. The collision of the plates cause many earthquakes such as Himalayas

20
Q

What happens at conservative plate boundaries

A

Occurs when plates slide past each other in opposite or same direction but at different speeds. Friction is eventually overcome and the plates slip past in a sudden movement causing an earthquake e.g. San Andreas fault

21
Q

Name the point in the crust where the pressure is released

A

Focus

22
Q

What is the epicentre

A

The point on the Earth’s surface above the focus where the most intense shaking occurs

23
Q

Factors affecting the impact of an earthquake

Level of development

A

Richer LICs and NEEs more likely to have the resources and technology for monitoring and prediction

24
Q

Factors affecting the impact of an earthquake

Population density

A

More densely populated the area, the greater the hazard will be so more deaths and casualties

25
Q

Factors affecting the impact of an earthquake

Communication

A

Accessibility for rescue teams, earthquakes often damage bridges etc

26
Q

Factors affecting the impact of an earthquake

Time of day

A

This influences weather people are in their homes, at work or travelling if during rush hour could be devastating

27
Q

Factors affecting the impact of an earthquake

Time of year and climate

A

Will influence survival rates and the rate that disease is spread. Hot tropical places are particularly bad

28
Q

Richter scale

A

Measures the magnitude of a tremor using seismograph, has no upper limit, is a logarithmic scale so each is 10x larger than the previous

29
Q

Mercalli scale

A

Scale from 1-XII and measures the effects of earthquakes. Uses subjective descriptions of the resulting damage

30
Q
Chile earthquake
Date/ GDP ranking
magnitude
focus depth
epicentre
cause
A
27th February 2010
46
8.8 
35km
11km from Concepcion
Nazca plate and s. American plate (convergent)
31
Q
Haiti earthquake
Date/ GDP ranking
magnitude
focus depth
epicentre
cause
A
12th January 2010
143
7.0
13km
25km west of port-Au-prince
Caribbean plate and north American plate (conservative)
32
Q

Deaths, injuries, no. of homes damaged- Chile

A

500 deaths, 12,000 causalities, nearly 400,000 homes damaged

33
Q

Deaths, injuries, no. of homes damaged- Haiti

A

230,000 deaths, 300,000 casualties, 250,000 homes damaged

34
Q

Secondary effects- Chile

A

150 deaths from Tsunami,
est $15-30 billion damage
Lost power, fire at chemical plant

35
Q

Secondary effects- Haiti

A

All hospitals in the capital were destroyed, public phones not available
Looting, debris blocked main road
2 million left without food and water

36
Q

Short term response- Chile

A
Government vowed to deliver aid quickly
Firefighters combed rubble for people
Army sent 10,000 troops,
curfew imposed to prevent looting 
Communications in the capital restored within 4 days
37
Q

Short term response- Haiti

A

Government appealed quickly for aid
Over 1st weekend received many food and water packets
Hard to get aid as the port was damaged

38
Q

Long term response- Chile

A

Month later, government launched a housing reconstruction plan
Strong economy so could rebuild without relying on foreign aid

39
Q

Long term response- Haiti

A

Dominican republic accepted some refugees

Senegal offered land to anyone in Haiti who wanted it

40
Q

Preparation and protection- Chile

A

Building code require shake-resistant construction and rapid emergency response
Regular anti-disaster drills
Prepared following 1960 earthquake

41
Q

Preparation and protection- Haiti

A

Tsunami warning was issued immediately after initial earthquake, but quickly cancelled it
Not prepared as never had an earthquake before
Port-Au-Prince had 2.5 mil population so overcrowded and houses were poorly built