1 Locations at risk from tectonic hazards Flashcards

1
Q

What percentage of earthquakes are found in the ‘Ring of Fire’ in the Pacific Ocean?

A

70%

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2
Q

What are the most powerful earthquakes associated with?

A

Convergent or conservative boundaries

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3
Q

What are the names of the two zones where earthquakes are found?

A
  • The oceanic fracture zone (OFZ) - a belt of activity through the oceans along the mid-ocean ridges, coming ashore in Africa, the Red Sea, the Dead Sea rift and California.
  • The continental fracture zone (CFZ) - a belt of activity following the mountain ranges from Spain via the Alps, to the Middle East, the Himalayas to the East Indies and then circumscribing the Pacific.
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4
Q

Where can a small minority of earthquakes also occur?

A

A small minority of earthquakes can also occur along old fault lines and the hazard is associated with the reactivation of this weakness, for example, the Church Stretton Fault in Shropshire.

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5
Q

What is the violence of a volcanic eruption determined by?

A

The amount of dissolved gases in the magma and how easily the gases can escape

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6
Q

How many active volcanoes are there throughout the world?

A

There are about 500 active volcanoes throughout the world and, on average, around 50 of them erupt each year.

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7
Q

What are the three types of plate boundary?

A
  • Divergent (constructive) margins, most clearly displayed at mid-ocean ridges. At these locations, there are large numbers of shallow focus and generally low magnitude earthquake events. Most are submarine.
  • Convergent (where plates move together): these are actively deforming collision locations with plate material melting in the mantle, causing frequent earthquakes and volcanoes.
  • Conservative (oblique-slip, sliding or transform) margins, where one plate slides against another. Here the relative movement is horizontal and classified as either sinistral (to the left) or dextral (to the right). The lithosphere is neither created nor subducted.
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8
Q

Where are divergent (constructive) margins, most clearly displayed?

A

At mid-ocean ridges

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9
Q

What type of earthquake occurs at divergent (constructive) margins?

A

At these locations, there are large numbers of shallow focus and generally low magnitude earthquake events. Most are submarine.

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10
Q

What type of earthquake occurs at conservative (oblique-slip, sliding or transform) margins?

A

They are sites of extensive shallow focus earthquakes, occasionally of considerable magnitude

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11
Q

What is the name of the plate margin where plates move away from each other?

A

Divergent ‘spreading ridges’

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12
Q

Why are earthquakes at divergent ‘spreading ridges’ in the oceans typically a low hazard risk?

A

The earthquakes seen at these boundaries tend to be frequent, small and typically a low hazard risk because of their geographical position (that is, the ocean) and they do not typically trigger tsunamis.

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13
Q

What is happening along the San Andreas Fault in California?

A

The Pacific Plate (moving north) creates a zone of friction against the North American Plate (moving north at a different speed)

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14
Q

What happens as two plates are moving towards each other (convergent)?

A

Typically when this happens, one plate starts sliding under the other. As the strain builds over time in the subduction zone, the friction between the two masses of rock is overcome, releasing energy. This will produce both earthquakes - such as the tsunami-generating ones off Japan in 2011 and Aceh which are fed by the melting of the subducting plate.

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15
Q

What are active subduction zones characterised by?

A

Magmatic activity, a mountain belt with thick continental crust, a narrow continental shelf and active seismicity

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16
Q

Where are passive continental margins found?

A

Along the remaining coastlines

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17
Q

What are the different tectonic settings where volcanoes are found in?

A

1 Destructive plate boundaries. These occur at locations where two plates are moving together. Here they form either a subduction zone or a continental collision, depending on the type of plates. When a dense oceanic plate collides with a less-dense continental plate, the oceanic plate is typically thrust underneath because of the greater buoyancy of the continental lithosphere, forming a subduction zone. These volcanic eruptions tend to be more infrequent but more destructive.
2 Divergent boundaries create rift volcanoes where plates diverge from one another at the site of a thermally buoyant mid-ocean ridge. These are generally less explosive and more effusive. Here there is basaltic magma, which has low viscosity.
3 Hotspot volcanoes are found in the middle of tectonic plates and are thought to be fed by underlying mantle plumes.

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18
Q

What happens when a less dense oceanic plate collides with a less-dense continental plate at a destructive plate boundary?

A

The oceanic plate is typically thrust underneath because of the greater buoyancy of the continental lithosphere, forming a subduction zone

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19
Q

Why is the oceanic plate typically thrust underneath the continental plate at a destructive plate boundary?

A

Because of the greater buoyancy of the continental lithosphere, forming a subduction zone

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20
Q

Where do plates diverge from one another at a divergent boundary?

A

At the site of a thermally buoyant mid-ocean ridge

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21
Q

What type of eruption occurs at divergent boundaries?

A

These are generally less explosive and more effusive. Here there is basaltic magma, which has low viscosity.

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22
Q

Where are hotspot volcanoes found?

A

In the middle of tectonic plates

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23
Q

What is a volcanic hotspot?

A

A volcanic hotspot is an area in the mantle from which heat rises as a hot thermal plume from deep in the Earth. High heat and lower pressure at the base of the lithosphere enable melting of the rock. This molten material, magma, rises through cracks and erupts to form active volcanoes on the Earth’s surface.

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24
Q

What does high heat and lower pressure at the base of the lithosphere enable?

A

Melting of the rock

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25
Q

What happens as the tectonic plate moves over the stationary hotspot?

A

As the tectonic plate moves over the stationary hotspot, the volcanoes are rafted away and new ones form in their place.

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26
Q

What happens as oceanic volcanoes move away from the hotspot?

A

They cool and subside, producing older islands, atolls and seamounts

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27
Q

What are the names of the two types of crust, which are made up of different types of rock?

A
  • Thin oceanic crust, which underlies the ocean basins, is composed primarily of basalt
  • Thicker continental crust, which underlies the continents, is composed primarily of granite
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28
Q

What does the geothermal gradient of the Earth’s mantle mean in terms of changes in temperature?

A

The highest temperatures occur where the mantle material is in contact with the heat-producing core so there is a steady increase of temperature with depth

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29
Q

Where does seafloor spreading occur?

A

At divergent boundaries under the oceans

30
Q

What is the technique involving the reconstruction of paleomagnetic reversals called?

A

Paleomagnetism

31
Q

What is the Benioff Zone?

A

The Benioff Zone is an area of seismicity corresponding with the slab being thrust downwards in a subduction zone.

32
Q

Why is the theoretical framework of the Benioff Zone an important factor in determining earthquake magnitude?

A

It determines the position and depth of the hypocentre

33
Q

What are earthquakes caused by?

A

Earthquakes are caused by sudden movements comparatively near to the Earth’s surface along a fault.

34
Q

What are faults?

A

Faults are zones of pre-existing weakness in the Earth’s crust.

35
Q

What events occur in the generation of an earthquake?

A

1 The movements are preceded by a gradual build-up of tectonic strain, which stores elastic energy in crustal rocks.
2 When the pressure exceeds the strength of the fault, the rock fractures.
3 This produces the sudden release of energy, creating seismic waves that radiate away from the point of fracture.
4 The brittle crust then rebounds either side of the fracture, which is the ground shaking, that is, the earthquake felt on the surface.

36
Q

Where can the point of rupture, the hypocentre, occur?

A

The point of rupture, the hypocentre, can occur at any depth between the Earth’s surface and about 700 km.

37
Q

What type of earthquake events is the most damaging?

A

The most damaging events are usually shallow focus, with a hypocentre of fewer than 40 km.

38
Q

What does a seismometer measure?

A

A seismometer measures the amount of ground shaking during an earthquake, recording both the vertical and horizontal movements of the ground.

39
Q

What are the three types of seismic waves that an earthquake produces?

A

Primary or P waves
Secondary or S waves
Love waves or L waves

40
Q

What rate of speed do primary or P waves travel at?

A

About 8 km/sec

41
Q

What rate of speed do secondary or S waves travel at?

A

Around 4 km/sec

42
Q

What is the overall severity of an earthquake linked to?

A

The amplitude and frequency of wave types

43
Q

Why are the S and L waves more destructive than the P waves?

A

They have a larger amplitude and energy force

44
Q

Explain why land adjacent to rivers and sloping ground can present a hazard.

A

Land adjacent to rivers and sloping ground can present a hazard by sliding under low-friction conditions across a liquefied soil layer. This is called lateral spreading, sometimes creating large fissures and cracks in the ground surface.

45
Q

What are the consequences of soil liquefaction?

A

The consequences of such hazards can be considerable: damage to roads and bridges as well as telecommunication and other services (gas, electricity, sewerage) which run through the upper sections of the ground. The short-term impact on the delivery of aid and the longer-term rebuild costs can be substantial.

46
Q

Where do many destructive earthquakes occur?

A

In mountainous areas

47
Q

What are more than half the earthquake deaths in Japan linked to events with?

A

A magnitude greater than 6.9

48
Q

What percentage of all deaths caused by earthquakes globally (excluding those from shaking, building collapse and tsunami), is attributable to the secondary impacts of landslides?

A

Around 70 per cent

49
Q

Why do tsunami waves not resemble normal sea waves?

A

Their wavelength is much longer

50
Q

Out to sea, why do tsunami waves not represent a hazard?

A

Out to sea, they do not represent a hazard since they are generally low in height (often below 300 mm) and generally go unnoticed.

51
Q

What happens to tsunami waves as they approach a coastline?

A

It is only as they approach a coastline that they grow in height as the water becomes shallower.

52
Q

What is a tsunami?

A

A tsunami is not a single wave but a series of waves, also known as a wave train, caused by seabed displacement.

53
Q

What is a tsunami caused by?

A

Seabed displacement

54
Q

Explain why the amount of time between successive waves (the wave period), represents a greater risk?

A

People have lost their lives after returning homes between the waves of a tsunami, thinking that the waves had stopped coming

55
Q

What percentage of all tsunami events occur within the Pacific Basin?

A

Around 90 per cent

56
Q

Where are most tsunami events generated at?

A

Most are generated at subduction zones (convergent boundaries), particularly off the Japan-Taiwan island arc, South America and Aleutian Islands (25 per cent of all historical events have been recorded in this geographic region).

57
Q

What do tsunami travel time maps give a better understanding of?

A

How an event may occur, and the potential risks for people living within a tsunami’s reach

58
Q

What physical and human factors does the impact of a tsunami depend on?

A

1 The duration of the event.
2 The Wave amplitude, water column displacement and the distance travelled.
3 The physical geography of the coast, especially water depth and gradient at the shoreline.
4 The degree of coastal ecosystem buffer.
5 The timing of the event - night versus day - and the quality of early warning systems.
6 The degree of coastal development and its proximity from the coast, especially in tourist areas.

59
Q

When do the most serious tsunami events occur?

A

When the physical and human factors interact with each other to produce a disaster

60
Q

What are the primary hazards of volcanoes?

A

These include pyroclastic flows, tephra, lava flows and volcanic gases.

61
Q

What do pyroclastic flows result from?

A

From the frothing of molten magma in the vent of the volcano

62
Q

What is tephra?

A

When a volcano erupts it will sometimes eject material such as rock fragments into the atmosphere - this is tephra.

63
Q

What is the viscosity of the lava in lava flows determined by?

A

The amount of silicon dioxide it contains

64
Q

Why is carbon dioxide dangerous?

A

Most deaths have been associated with carbon dioxide; it is dangerous because it is colourless and odourless and can accumulate in valleys undetected by people. In 1986, emissions of carbon dioxide from Lake Nyos in Cameroon killed 1700 people.

65
Q

What are the two most significant secondary impacts of volcanoes?

A

Volcanic mudflows (lahars) and catastrophic floods (jokulhlaups)

66
Q

What are lahars?

A

Lahars are volcanic mudflows generally composed of relatively fine sand and silt material.

67
Q

Why are lahars associated with heavy rainfall as a trigger?

A

Old tephra deposits on steep slopes can be re-mobilised into mudflows

68
Q

What are jokulhlaups?

A

Jokulhlaups are a type of catastrophic glacial outburst flood. They are a hazard to people and infrastructure and can cause widespread landform modification through erosion and deposition. These floods occur very suddenly with rapid discharge of large volumes of water, ice and debris from a glacial source.

69
Q

Where can jokulhaups occur?

A

They can occur anywhere water accumulates in a subglacial lake beneath a glacier.

70
Q

What is the flood associated with jokulhaups initiated by?

A

The flood is initiated following the failure of an ice or moraine dam.