Tectonics Flashcards

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1
Q

Seismic hazards

A

Generated when rocks within 700km of the Earth’s surface come under such stress that they break and become displaced

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2
Q

Volcanic hazards

A

Associated with eruption events

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3
Q

Intra-plate earthquakes

A

These occur in the middle or interior of tectonic plates and are much rarer than boundary earthquakes

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4
Q

Volcano

A

A landform that develops around a weakness in the Earth’s crust from which molten magma, volcanic rock and gases are ejected or extruded

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5
Q

Plate tectonics

A

A theory developed more than 60 years ago to explain the large-scale movements of the lithosphere (the outermost layer of the Earth)
Based around evidence from seafloor spreading and ocean topography, marine magnetic anomalies, palaeomagnetism and geomagnetic field reversals
Knowledge of the Earth’s interior and outer structure is essential for the understanding of plate tectonics

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6
Q

Lithosphere

A

The surface layer of the Earth is a rigid outer shell comprised of the crust and upper mantle
It is on average 100km deep
It is always moving but very slowly, fuelled by rising heat from the mantle which makes convection currents
The distinction between the lithosphere and the atmosphere is one of physical strength rather than a difference in physical composition
The lithosphere is broken down into huge sections which are the tectonic plates

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7
Q

Palaeomagnetism

A

The zone of magma ‘locking in’ or ‘striking’ the Earth’s magnetic polarity when it cools
A tool used to determine historic periods of large-scale tectonic activity through the reconstruction of relative plate motions
They create a geo-timeline

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8
Q

Hypocentre

A

The focus point in the ground where the strain energy of the earthquake stored in the rock is first released
The distance between this and the epicentre on the surface is called the focal length

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9
Q

Soil liquefaction

A

Water saturated material temporarily loses normal strength and behaves like liquid under the pressure of strong shaking
Occurs in saturated soils
Earthquakes can cause the water pressure to increase to the point where the soil particles can move easily, especially in poorly compacted soil

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10
Q

Intensity

A

A measure of ground shaking

It is the ground shaking which causes houses to collapse and the loss of life from hazards

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11
Q

Epicentre

A

The location on the Earth’s crust that is directly above the earthquake focus i.e. the point where an earthquake originates

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12
Q

Magnitude

A

The magnitude of an earthquake is related to the amount of movement, or displacement, in the fault, which is, in turn, a measure of energy release
2004 Indonesia earthquake was magnitude 9.1 as there was a large vertical displacement (15m) along a very long fault distance approx. 1500km
Earthquake magnitude measured at the epicentre, the point on the crust directly above the hypocentre

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13
Q

Oceanic plates thickness off…

A

7-10km

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14
Q

Continental plates thickness off…..

A

25-75km

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15
Q

Tsunami

A

Tsu: port/harbour
Nami: wave/sea
Initiated by undersea earthquakes, landslides or slumps and sometimes volcanic eruptions
Have long wavelengths, 150-1000km
Low amplitudes (wave height) 0.5-5m
Fast velocities, up to 600kph in deep water

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16
Q

Hazard

A

‘A perceived natural/geophysical event that has the potential to threaten both life and property’
It would not be such without people living at or near its location
That is to say, earthquakes would be hazards if there were not people living in the buildings which collapsed
Hazards can occur at the interaction between human and natural factors

17
Q

Disaster

A

The realisation of a hazard
‘when it causes significant damage to the population’
The Centre for Research on the Epidemiology of Disasters state a hazard is a disaster when:
10 or more people have been killed
100 or more people have been affected

18
Q

Risk

A

The exposure of people to a hazardous event

The probability of a hazard occurring that leads to the loss of lives/livelihood

19
Q

Resilience

A

The ability of a system, community or society exposed to hazards to resist, absorb and recover from the effects of a hazard

20
Q

Development

A

Linked to an improving society
The provision of local services, acquisition of economic assets, improved productivity and reducing vulnerability to natural disasters
Low levels of development are closely associated with high levels of risk and vulnerability to natural disasters

21
Q

Inequality

A

Refers to an unfair situation or distribution of assets and resources
May also be used when people, nations and non-state players have different levels of authority, competence and outcomes

22
Q

Governance

A

How individuals and institutions, public and private, manage their common affairs
A continuing process where conflicting views and diverse interests may be accommodated and co-operative action may be taken
Formal institutions and regimes empowered to enforce compliance as well as informal arrangements that people and institutions have either agreed to or perceive to be in their interest

23
Q

Disaster hotspot

A

A country or area that is extremely disaster prone for a number of reasons

24
Q

Tectonic hazard profiles

A

Used to understand the physical characteristics of hazards e.g. volcanic eruption, tsunami, earthquake
Can be used to contrast the same hazard which occurs in contrasting places or at different times
Criteria such as frequency, duration and speed of onset

25
Q

Subduction Zones

A

The area in the mantle where a tectonic plate melts
Contact between plates sometimes called a megathrust fault
Plates locked together and build friction
Stress released through the megathrust earthquake and seismic waves occur
Enormous stress can be built up before release

26
Q

The process of stress, strain and failure on a tectonic plate

A

Often called the elastic rebound theory

27
Q

Locked fault

A

A fault which is not slipping due to frictional resistance being greater than the shear stress across the fault which is stuck
Stress may be held for years and then released as a large magnitude earthquake or when frictional resistance is overcome
2004 Indian Ocean tsunami was a megathrust locked fault which generated huge seismic waves and a tsunami

28
Q

P waves

Primary

A

The fastest seismic waves
Waves travel through both solids and liquids
Shunting motion
8km/sec

29
Q

S waves

Secondary

A

Seismic waves which only travel through solids and more with a sideways motion
right angle vibrations
4km/sec

30
Q

L waves

Love

A

The slowest seismic waves
All energy focussed on the Earth’s crust
surface vibrations in the crust
High amplitude