Tectonic hazards Flashcards

(44 cards)

1
Q

Cross section of the Earth


A

Crust, mantle, outer core, inner core

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2
Q

What is the mantle?


A

Made of semi-molten rock, magma
Thickest section - 2900km
Magnesium and iron

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3
Q

What is the inner core?


A

Solid layer of iron and nickel
Temperature of 5500 oC

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4
Q

What is the outer core?


A

Liquid layer of the Earth’s core, made of iron and nickel

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5
Q

Characteristics of continental plates


A

Older
Less dense
Can’t sink

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6
Q

Characteristics of oceanic plates


A

Younger
Very dense
Can sink

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7
Q

Explain the theory of convection currents


A

Magma near the outer core is heated. As the magma warms, it expands and becomes less dense. The less dense magma then starts to rise towards the crust. As the magma nears the crust, it begins to cool. The cooling magma becomes denser and begins to sink. The rising and falling magma creates circular currents with the mantle. These currents create friction with the crust above and causes it to move. These are known as convection currents.

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8
Q

Explain the theory of ridge push


A

Magma rises as the plates move apart. Magma cools to form new plate material. As it cools it becomes denser and slides down away from the ridge. This causes tectonic plates to move away from each other. Occurs at constructive plate margins.

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9
Q

Explain the theory of slab pull


A

Denser plate sinks back into the mantle under the influence of gravity. It pulls the rest of the plate along behind it.

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10
Q

Which plate margins are earthquakes found at?


A

All 3 (constructive, destructive, conservative)

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11
Q

Which plate margins are volcanoes found at?


A

Constructive and destructive

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12
Q

Explain the constructive plate boundary


A

The plates move away from each other. When this happens, the magma from the mantle rises up and cools to make new land in the form of a shield volcano. Ridge push occurs. The movement of plates over the mantle can cause earthquakes. Ridges can form.

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13
Q

Explain the destructive plate boundary

A

The dense oceanic plate is subducted under the lighter continental plate into the mantle. Slab pull occurs. Friction causes melting of the oceanic plate and may trigger earthquakes. Destructive plates cause both volcanoes and earthquakes.

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14
Q

Landforms formed at constructive boundaries


A

Shield volcanoes and ocean ridges

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15
Q

Landforms formed at destructive boundaries


A

Composite volcanoes, oceanic trenches

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16
Q

Explain the conservative plate boundary


A

As the plates move, friction occurs and plates become stuck. Pressure builds up because the plates are still trying to move. When the pressure is released, it sends out a huge amount of energy causing an earthquake.

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17
Q

How do plates move at constructive margins?


A

Away from each other

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18
Q

How do plates moves at destructive margins?


A

Towards each other

19
Q

How do plates move at conservative margins?


A

Move past each other in same or opposite direction but at different speeds

20
Q

Landforms at conservative margins


A

Fault lines (San Andreas fault line)

21
Q

How many killed in L’Aquila earthquake?


22
Q

How many killed in Gorka, Nepal earthquake?


23
Q

Economic damage of L’Aquila


A

$11,400 million in damage

24
Q

Economic damage of Gorka


A

$5 billion damage

25
Primary effects of L'Aquila earthquake 

308 killed and 1500 injured $11,000 million in damage 15,000 buildings collapsed including San Salvatore hospital and L'Aquila university
26
Secondary effects of L'Aquila earthquake

Landslides damaged housing and transport House prices and rent increased Some of city cordoned off, reducing business. Burst water pipeline caused a mudflow.
27
Immediate responses to the L'Aquila earthquake

Free mobile calls 10,000 sheltered at hotels, 40,000 tents given. $550 million raised from EU Solidarity Fund . Dog units searched for survivors.
28
Long-term responses to the L'Aquila earthquake

Torch-lit procession with Catholic mass every year. No taxes for residents during 2010. Students university fees waived and received free public transport.
29
When was the L'Aquila earthquake, Italy?

April 2009
30
When was the Gorka earthquake, Nepal?

April 2015
31
Primary effects of the Nepal Earthquake.

8,841 died. 1 million made homeless UNESCO heritage site destroyed $5 billion damage. International airport congested as aid arrived. 7,000 schools and 26 hospitals destroyed
32
Secondary effects of the Nepal earthquake

Tourism employment and income declined. Landslides and avalanches on Mount Everest killed 19 people. Landslide blocked river so people evacuated in case of flooding. Blocked roads slowed aid. Rice seed ruined, food shortages and income loss.
33
Immediate responses to the Nepal earthquake

International help requested. 500,000 tents provided. Rescues from avalanches on Mount Everest made by helicopter. UN and World Health organisation sent medical supplies to the worst affected districts. Field hospitals set up.
34
Long-term responses to the Nepal earthquake

$247 million aid money committed to recovery. Lakes and river valleys cleared of landslide material to avoid flooding. Stricter building controls enforced. New trekking routes on Mount Everest opened.
35
Social reasons people live at risk from tectonic hazards

People want to stay near families and friends Threat isn't great enough People are confident that the buildings will keep them safe
36
Economic reasons people live at risk from tectonic hazards

Geothermal energy provides energy for area. Nutrient-rich soils helps agriculture Mining provides energy and income Tourism creates jobs and provides income Cheaper to stay than to move
37
How can volcanic eruptions be monitored?

Changes in shape of ground using tiltmeters and GPS satellites. Radon and sulphur gas can be measured using gas-trapping bottles Thermal heat sensors, ground surface and river temperatures Earthquakes near magma chamber using seismometers
38
How can volcanic eruptions be predicted?

Easier to predict than earthquakes as they give warning signals before erupting.
39
How can people be protected against volcanic eruptions?

Buildings can't be designed to completely protect against eruption. Evacuation issued by authorities.
40
How can people plan for volcanic eruption?

Evacuation Exclusion zones Education First-aid training
41
How can earthquakes be monitored?

Foreshocks using seismometers and GPS. Radon using radon detection devices. Harder to monitor than volcanoes
42
How can earthquakes be predicted?

They can't
43
How can people be protected against earthquakes?

Building infrastructure - foundations with rubber shock absorbers Sea walls in case of tsunamis
44
How can people plan for earthquakes?

Practice drills Preparing emergency supplies Knowing location of evacuation centres Securing furniture