Topic 1: Hazardous Earth Flashcards

1
Q

What are the effects of areas of low pressure?

A

Air rises in areas of low pressure as it is less dense. As it rises, it cools and condenses, forming moist clouds. Moisture builds up within these clouds causing high precipitation and cloudy conditions. It is the opposite for high pressure

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2
Q

What are the different cells of atmospheric circulation in order from closest to the equator?

A

Hadley cell (0-30°), Ferrel cell (30-60°), Polar Cell (60°+)

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3
Q

What naturally affects global temperatures and why?

A
  • Distribution of sun’s radiation- More concentrated radiation and “thinner” atmosphere due to angle at the equator
  • Earth’ axial tilt- The tilt in the axis of the Earth is called its ‘obliquity’. This angle changes with time, and over about 41 000 years it moves from 22.1° to 24.5° and back again. When the angle increases the summers become warmer and the winters become colder.
  • The earths precession- The Earth wobbles on its axis caused by the gravitational pull of the Moon and the Sun upon the Earth. This means that the North Pole changes where it points to in the sky. It impacts the seasonal contrasts between hemispheres and the timing of the seasons
  • Eccentricity- the earth’s rotational orbit around the sun can change pattern and shape iver thousands of years. It can move from circular (interglacial) to more elliptical (glacial). This can alter the definition of seasons and overall climate of the earth.
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4
Q

What is the coriolis effect?

A

Winds are caused when air moves from high to low pressure across the earth’s surface as a result of different places heating and cooling. Because of the earth’s rotation, the wind is deflected to the right in the Northern Hemisphere and left in the Southern Hemisphere. This is called the Coriolis effect

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5
Q

How is heat transfered by ocean currents?

A

Surface currents are caused by winds and help transfer heat away from the equator (eg: gulf stream brings warm water from Caribbean to Western Europe). Deep ocean currents are driven by water density. When 2ater freezes at the poles, the surrounding water becomes saltier, increasing its density, causing it to sink and warmer water to flow in at the surface. This warmer water is cooled and sinks, continuing the cycle.

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6
Q

Name all the natural causes of climate change

A
  • Orbital changes (eccentricity, axial tilt, precession)
  • Asteroid collisions
  • Volcanic erruptions
  • The sunspot theory
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7
Q

How do volcanic erruptions alter the earths climate?

A

Major volcanic erruptions eject large quantities of ash into the atmosphere. Some of these particles reflect the Sun’s rays so the Earth’s surface cools. Thos causes short-term changes in climate.

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8
Q

How can astroid collisions alter the earth’s climate?

A

Asteroids hitting the Earth”s surface can throw up huge amounts of dust into the atmosphere. These particles prevent the sun’s energy from reachings the Earth”s surface, causing global temperatures to fall.

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9
Q

What is the sunspot theory?

A

There are black areas on the sun’s surface called sunspots. Sometimes the sun has many, st other times they dissapear. Lots of spots tell us rhe sun is more active and therefore has a higher solar output. Cooler periods such as the Little Ice Age may have been caused by changes in sunspot activity; less active.

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10
Q

What is evidence of past glacial and interglacial periods?

A
  • Tree rings: Each ring represents a tear of growth. Warmer and wetter conditions cam show greater growht through a larger tree ring
  • Ice cores: Contain bubbles of the air from each year. Scientists analyse how much CO2 they contain. They can also learn about temperatures by measuring the relative amounts of different types of oxygen atoms in the ice and ash.
  • Historical sources: Old photos, drawings, written record, diaries and records of dates. Not very accurate but can give some evidence on recent climate change
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11
Q

Guve 3 pieces of evidence showing the climate used to be cooler.

A
  • Less sunspots in the Little Ice Age (Maunder Minimum)
  • Sightings of ice in North Scotland- Little Ice Age
  • 1816- Year without a summer (volcanic activity)
  • 1991- Planet cooled by 0.5°C (Mt Pinatubo eruption)
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12
Q

How does agriculture cause climate change?

A

Farming of livestock produces lot sof methane, rice paddies; flooded fields emit methane, Land cleared of trees, stops absorption of CO2. Population growht led to a higher demand of food.

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13
Q

How has energy caused global warming?

A

The demand for electricity is growing because of increasing population and new technologies. Most of energy is produced through burning fossil fiels, emiting CO2.

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14
Q

How has transport caused global warming?

A

Most cars, lorries, ships and planes run on fossil fuels. Car ownership is rapidly increasing, meaning more cars pn road. This increases congestion; car engines running for longer, emmiting CO2

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15
Q

How has industry caused global warming?

A

Most industries use a lot of energy. Some industrial processes also release greenhouse gasses (eg: cement made from limestone, containg carbon. When produced, lots pf CO2 is released.) Industrial waste may end up in landfill sites where it decays releasing methane.

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16
Q

Give 3 pieces of evidence hmuman activity is causing climate change

A
  • By 2012, floating sea ice in Artic has shrunk to less than hlaf the amount on 1979
  • Sea levels rose by 210mm from
    1870 to 2010. They are rising
    because the sea expands as it
    warms, called thermal expansion
  • Top ten warmest years have all been since 2000
  • Since 1950, there have been more heat waves
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17
Q

Give 2 reasons why the predictions of future global temperatures are uncertain

A
  • Population growht may vary in future years
  • Countires may or may not witch to more renewable resources
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18
Q

What are impacts of clinate change?

A
  • deaths due to heat have increased
  • Some areas may become sp hot and dry they are difficult or impossible to inhabit
  • Low lying coastal areas may flood, resulting in migration and overcrowding in other- Lower crop yields could increase malnutrition, il health and death from starvation areas
  • More extreme weather, more money has to be spent on predicting extreme weather events
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19
Q

How is solar radiation distrubuted?

A

The earth is largely spherical so more radiation is received at the Equator, the hottest part of
the earth whereas the poles are the coldest part. At the Equator, the sun’s rays are
concentrated over a small area and strike at a right angle, meanwhile at the poles they reach
the surface at a lower angle so the same radiation has to heat up a larger surface area. Also
near the poles the radiation has had to pass through ‘more’ atmosphere and travel a greater
distance so energy has been absorbed, meanwhile at the equator this is less.

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20
Q

How does wind transfer heat from the equator to the Poles?

A

1) At the equator, the sun warms the earth, transfering heat to the air above, causing it to rise, creating a low pressure belt
2) The cool dry air moves to 30° N/S
3) At 30°, the cool air sinks, creating a high pressure belt
4) The cool air reaches the ground surface and moves as surface winds either back to equator or towards poles
5) The trade winds towards the equator meet and are heated by the sun, causing them to rise
6) At 60° N/Sm the warmer surface winds meet colder air from the poles. The warm air is less dense so is forced to rise, creating low pressure.
7) Some of the air moves back towards the equator and the rest towards the poles

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21
Q

What are the outer walls pf a tropical cyclone called?

A

Rain bands

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22
Q

How do tropical cyclones form?

A

1) Strong clusters of thunderstorm drift over warm waters over 26°C
2) Very warm air from the strom and ocean surface begin rising, creating low pressu
3) Trade winds blowing in the opposite direction causing the strom to spin. Rising warm air causes pressure to decrease at higher altitudes
4) Air rises faster to fill the low pressure, drawing more warm air pff the sea and sucking in cooler, dryer air downwards
5) As the storm moves over the ocean it picks up more warm moist air. Wind speeds increase as more air is sucked into the low pressure center

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23
Q

Where do tropical cyclones occur?

A

Within 5-30° North or South of the equator

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24
Q

What is the description and impacts of high winds?

A

High winds: Teopical winds over 250km/h at times. Causes homelessness and damage to infrastructure, trees uprooted and blown over

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25
Q

What is the description and impacts of intense rainfall?

A

Tropical cyclones can release trillions of litres of water per day as rain. The rain gets heavier as you get closer to the eye of the strom. Can cause flooding, resulting in limted access to evacuation. Can oversaturate soil, damaging crops and plants.

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26
Q

What is the description and impacts of storm surges?

A

Storm surges are large rises in sea level due to low pressure. High winds drag this rise in sea level towards the shore. People may drown in the strong current created. Can damage property and carry debris. Can kill plants and crops through oversaturatiing soil and damge trees.

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27
Q

What is the description and impacts of coastal flooding?

A

Flooding occurs as a result of storm surges, high winds and rises in sea levels, driving large waves of water onto the coast. Can damage coastal defenses and local infrastrucutre. Can erode the beach and damage land and vegatation as it saturates the soil. Contaminates areas with salt water such as fresh-water lakes

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28
Q

What is the description and impacts of landslides?

A

Heavy rain males steep areas unstable, causing landslides as the soil becomes saturated through flooding and heavy rain. Can destriy property and infrastructure below and act as road blocks. Can destroy vegetation and trees as they are swept away.

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29
Q

What is the saffir simpson scale?

A

The Saffir-Simpson Hurricane Wind Scale is a 1 to 5 rating based only on a hurricane’s maximum sustained wind speed. This scale does not take into account other potentially deadly hazards such as storm surge, rainfall flooding, and tornadoes.

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30
Q

What are reasons for physical vulnerability of tropical cyclones?

A
  • Coastal areas are at significantly more risk of being affected by tropical cyclones
  • Low-lying coastal regions
  • Low relief areas at risk of high winds, storm surges, extreme rainfall and flooding
  • High relief areas at risk from the heavy rain, causing landslides particularly in steep areas
  • Islands such as the Caribbean have little land mass, so the storm loses little energy as it passes, resulting in a larger impact to people and environment
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31
Q

What are reasons for economic vulnerability of tropical cyclones?

A

Countries with high levels of development are more likely to have:

  • Access to accurate weather predicitions and modelling data, allowing preperation for cyclone, significantly reducing the impact
  • Coastal defences, coastal areas less affected by storm surges and damage caused by the cyclone will be reduced
  • Well established evacuation procedures and disaster response teams. Poorer countries often have to wait for international aid agencies to help. Supplies of food, clean water and medicine more likely to be available
  • People have insurance to cover damage
  • However, the economic impact is often greater in richer countries as they have more expensive infrastructure
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32
Q

What are reasons for social vulnerability of tropical cyclones?

A

Social inequalities can make some areas more vulnerabel tot he impacts of tropical cyclones than other.
- Housing and other construction may not be of a high standard, more easily damaged or destriyed.
- Poorer areas may not have access to shelter, food, clean water supllies and medical care after the event
- Areas with a population of higher or lower average age are more vulnerable as older people and young children are more likely tp suffer injury and have more difficulty evacuating the area. Also more at risk of disease, especially if there is less access to clean water
- People in poorer areas often don’t have access to transport routes or vehicles for evacuation

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33
Q

What is forecasting/ tracking and how does it help reduce the impact of a tropical cyclone

A

Can track the eye of the storm. When and where the storm will land can be recorded. This allows people to see if they are wihtin the path of a cyclone, allowing them to prepare or evacuate from the area before it hits, avoiding its impacts

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34
Q

What is warning/ evacuation and how does it help reduce the impact of a tropical cyclone

A

Warning stratergies are used to alert people of a tropical cyclone. This could be through the use of sirens, TV, phones, radio, etc. This allows people to prepare or leave their homes to reach safety previous to the strom. This will also make everyone aware, potenitally including the poor or homeless. Emergency services can also prepare. Furthermore, in vulnerable areas, people are regugularly given information about being prepared, including how to secure your house, emergency packs, evacuation routes.

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35
Q

What is building design and how does it help reduce the impact of a tropical cyclone

A

Houses can be built with particular structures, aualities or materials. For example, not tiled roofs, houses raised abive the ground. This can reduce the impact of a tropical cyclone on buildings and infrastructure and reduce the effects of hazards such as flooding, storm surges and extreme winds; people less able to evacuate will be safer

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36
Q

What is rescue and how does it help reduce the impact of a tropical cyclone

A

Emergency services rescue those in danger or injured due to floods, debris or the collapsing of buildings. This can reduce the deaths after the cyclone by removing those in harmful/ dangerous environments and those at risk of death or trapped.

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37
Q

What is rebuilding and how does it help reduce the impact of a tropical cyclone

A

International aid services / military aid with resources, money and temporary structures/ shelters after a cyclone. Less people will be left in camps and areas that have little access for entry or exit. Buildings and houses can be rebuilt, reducing homelessness and resources such as food and coean water can be provided preventing starvation, dehydration and disease.

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38
Q

What are 3 preperation techniques?

A
  • Forecasting/ tracking
  • Warning/ evacuation
  • Building design
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39
Q

What are the 2 response techniques?

A
  • Rescue
  • Rebuild
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40
Q

What is preperation?

A

What can be done before the event to minimise the disruption/ risk to people and environment

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41
Q

What is response?

A

The events afterwards that are put in place to help the recovery and to achieve normality

42
Q

What was the magnitude of hurricane Katrina?

A

Category 3

43
Q

What was the magnitude of Cyclone Nargis?

A

Category 4

44
Q

Where and when did Hurricane Katrina occur?

A

South East USA- 29th August 2005

45
Q

Where and when did Cyclone Nargis occur?

A

Irrawaddy delta, Myanmar- 2nd May 2008

46
Q

What were the environmental impacts of Hurricane Katrina?

A
  • Coastal habitats such as sea turtle breading beaches damaged
  • Flooding damaged oil refineries in Louisiana, causing large oil spills
47
Q

What were the environmental impacts of Cyclone Nargis?

A
  • 38000 acres of mangrove forests destroyed
  • Flooding caused erosion, saturation and salinization (increased salt content) of the land, damaging crops and plants
48
Q

What was Hurricane Katrina’s impacts on people?

A
  • Over 1800 people killed
  • 300,000 houses destroyed and hundreds of thousands of people made homeless
49
Q

What was Cyclone Nargis’ impacts on people?

A
  • Over 140,000 people killed
  • 450,000 houses destroyed and 350,000 damaged
50
Q

What were the negatives of the US’ preperation and response?

A
  • Warning is quite expensive
  • Infrastructure was not cyclone-proof
  • Flood defences to protect the city failed, causing unexoected flooding- 80% of the city was underwater
  • Many of the buildings made of heavy materials such as concrete and bricks, resulting in a larger imoact when they collapsed
  • The evacuation procedures was hampered as the highways were too congested with fleeing traffic and people didn’t use public transport
51
Q

What were the positives of the US’ preperation and response?

A
  • The USA had a sophisticated monitering system, stating where and when the hurricane would hit
  • The NHC (National Hurricane Centre) had a hurricane warning for Louisiana, Missisipe and Alabama
  • Buildings made out of stronger materials such as concrete and brick
  • Mississippi and Louisiana declares states of emergency and 70-80% of New Orleans residents were evacuated
52
Q

What were the negatuves of Myanmar’s preperation, response and defense?

A
  • Didn’t have a dedicated monitering system for tropical cyclones
  • Warnings didn’t reach people in poor rural communities
  • Lots of the mangrive forest had been chopped down for farming, reducing natural protection from flooding and storm surges.
  • Houses made of weak, destrucatbek materials
  • No evacuation plans and few transport routes or vehicles for evacuation due to severe poverty
  • Warnings didn’t reach subsistance farmers and those experiencing extreme poverty due to their lack of technology
  • Aid agencies were refused access to Myanmar for a week after the disaster
53
Q

What were the positives of Myanmar’s preperation, response and defense systems?

A
  • Indian weather agencies warned the government of Myanmar and broadcasted of TV and radio 48 hours previous to the cyclone
  • Mangrive forests partially protected the coast from flooding and storm surges
54
Q

What is the definition and properties of the lithosphere (oceanic)?

A

The part of the crust beneath the oceans. It is less dense and thinner. It is solid and composed of basalt

55
Q

What is the definition and properties of the lithosphere (continental)?

A

The part of the crust beneath land. More dense and thicker. Solid and composed of granite. 35km thick

56
Q

What is the definition and properties of the lower mantle?

A

The part of the mantle closer to the core, largest part of the earth’s layers, semi-molten. Solid, 1600-4000°C

57
Q

What is the definition and properties of the Asthenosphere (upper mantle)?

A

The top layer of the mantle, denser mobile layer of where convection currents occur. Can flow slowly, 900-1600°C

58
Q

What is the definition and properties of the outer core?

A

Thick fluid layer that sits between the lower mantle and inner core. Very dense, liquid, composed of iron and nickel, 4500-5500°C

59
Q

What is the definition and properties of the inner core?

A

Very center of the earth. Highest density and high radioactivity. Almost solid, composed of iron and nickel, 5200-6000°C

60
Q

What are tectonic plates?

A

Tectonic plates are the moving layer of the lithosphere. They can be split into Continental and Oceanic. Tectonic plates are always moving due to the rising and falling heat within the mantle. The circular movement is made within convection currents.

61
Q

How do convection currents cause plate movement?

A

Tectonic plates float on the mantle. Radioactive decay of some elements in the mantle amd core generate heat. When the lower parts of the asthenosphere heat up, they become less dense and rise. As they reach the top of the asthenosphere, they cool, become denser and sink. These circular movements pf semi-molten rock are convection currents. They crate drag and friction on the base of the tectonic plates, causing them to move

62
Q

What is radiactive decay?

A

When elements are naturally unstable and reactive, their atoms release particles from their nuclei, giving off heat

63
Q

What is residual heat?

A

The gravitational energy left over from the formation of the earth by the compression of cosmic debris

64
Q

What is a convergent plate boundary?

A

Here, two plates are moving towards each other. The plate that isdenser will be submerged under the less dense. Where an oceanic plate meets a continental plate, the oceanic will be submerged.This can cause trenches such as the Atacama Trench (Peru-Chile trench). Where continental meets continental, there is no subduction as the rock is forced to collide, forming fold mountains such as the Himalayas.

65
Q

What is a divergent boundary?

A

Here, plates are moving apart. Magma will fill the gap left between the plates, forming new crust.
These are mostly found under oceans, where underwater volcanoes are formed

66
Q

What is a conservative boundary?

A

Here, two plates are sliding past each other. They are moving at different speeds and angles and can become stuck. Pressure will build up until a plate can break free, causing earthquakes.

67
Q

What are examples and features of a covergant boundary (oceanic + continental)

A

Nazca and South American plate boundary
Ocean trench, volcano, earthquake
The Andes Mountains

68
Q

What are examples and features of a covergant boundary (continental + continental)

A

India plate and Eurasian plate
Fold mountains, earthquakes
Himilayes mountains

69
Q

What are examples and features of a divergent boundary?

A

South American and African plate boundary
Valcanoes, ocean ridges, earthquakes, new land formed
Mid-Atlantic ridge

70
Q

What are examples and features of a conservative boundary?

A

North American and Pacific plate boundary
Earthquakes
San Andreas fault line

71
Q

What is the magma chamber?

A

The source of molten rock

72
Q

What are volcanic bombs?

A

Airborne materials from a volcanic eruption

73
Q

What is a parastic cone?

A

A secondaey vent formed in the side of the mountain

74
Q

What is a lahar?

A

A destructive mudslide

75
Q

What is a pyroclastic flow?

A

A flood of gas, dust and ash down the side of a volcano

76
Q

How are composite volcanoes formed?

A

A convergenr plate boundaey occurs when plates are moving towards eachither. One plate is pushed beneath the other and melts to form magma. This magma builds up forming a magma chamber until the pressure is eventually released through a volcano.

77
Q

How are shiled volcanoes formed?

A

Dovergent boundaries occur when plates are moving apart. Magma rises from the mantle and reaches the surface. This magma solidifies and forms new crust, which repeats, forming a shield volcano. These boundaries are common in the middle of the ocean.

78
Q

What are the properties of composite volcanoes?

A

These are tall, steep-sided cones made up of alternating layers of lava and ash.
• Convergent plate boundary.
• Made of alternating layers of lava and ash.
• Andesitic lava (high silica content) meaning it is viscous.
• Lava flows short distances before cooling.
• Violent but infrequent eruptions.
• Can include lava bombs and pyroclastic
flows or lead to lahars.

79
Q

What are the properties of shield volcanoes?

A

These are low, gently sloping domes with a wide base. Lava commonly erupts from fissures as well as the crater.
• Divergent plate boundary.
• Low with gently sloping sides.
• Formed by eruptions of basaltic (low silica content) lava.
• Lava flows long distances before cooling.
• Eruptions are frequent but relatively gentle

80
Q

How can a volcano occur away from the plate margins?

A

Through hotspot volcanoes

81
Q

What are hotspots?

A

Hotspots are where magma from the mantle erupts through the crust. They do not move.

82
Q

What are mantle plumes?

A

Small, long-lasting regions exist within the mantle of the Earth. These are ‘mantle plumes’. This plume is superheated rock, not magma. They are a constant source of heat called a hotspot. The plume rises from the hot spot through the mantle. As it reaches the upper mantle, the asthenosphere and base of the lithosphere melt.

83
Q

How do hotspot volcanoes form?

A

Hotspot volcanoes for, as mantle lpplumes rise from hotspots through the mantle. As it reaches the upper mantle, the asthenosphere and base of lithosphere melt. Magma rises through these weaknesses in the crust and erupts onto the seafooor forming a seamount. Continuous eruptions causes the seamount to break through the surface of the water, forming an island volcano.

84
Q

How do volcanoes become extinct?

A

As the plate moves, the island is carried beyond the hotspot, cutting it off from the magma. Volcanic activity stops. The mantle plum remains in a fixed position, resulting in chains of volcanoes, such as Hawaii.

85
Q

What are the features of hotspot volcanoes?

A
  • Not magma but superheated rock- basaltic
  • Lava travels far
  • Potential to errupt explosively
86
Q

What is a tsunami?

A

A tsunami is a series of ocean waves, usually caused by volcanic or earthquake activity under the ocean, which can eventually crash onto the shoreline. These can reach over 30m high

87
Q

How do tsunamis form?

A

When an earthquake, volcano or landslide
happens on the ocean floor, water is displaced.
This water forms the start of the tsunami.
When the waves reach shallower water:
• they begin to slow down
• they grow in height and gain energy
It is hard to see that a tsunami is approaching.
The clearest sign is the coastal water retreats
just before the waves reach the shore. This is
the trough of the wave following behind.
If a tsunami has a deep focus, there is more
water displacement, therefore a larger tsunami
forms.

88
Q

What is information of the Japan Tohoku earthquake?

A
  • 11 March 2011
  • Magnitude 9 in North East Japan
  • Pacific oplate submerged under Eurasian plate at the Japanese trench, triggering a tsunami
  • Focus fo 30km below sea bed
  • Epicenter 130km away from coast
89
Q

What is information about the Haiti earthquake?

A
  • 12 January 2010
  • Magnitude 7
  • Conservative plate boundary between North American and Caribbean plate
  • Shallow focus 13km
  • Epicentre 25km from Port-au-Prince
90
Q

What are the primary impacts of the Japan Earthquake?

A
  • Earthquake caused severe liquifaction, causing buildings to tilt and sink
  • Between 667-1479 deaths as a direct impact
  • Over 230,00 made homeless. Many buildings destroyed. Significantly less
  • 1 dam collapsed, 2 nuclear power stations fractured and an oil refinary set on fire
91
Q

What are the primary impacts of the Haiti Earthquake?

A
  • Many houses poorly built and collapsed instantly. Around 1 million made homeless and 180,000 homes destited
  • 316,000 deaths and 30,000 injured
  • The port, communication systems and and major roads damaged beyond repair
92
Q

What are the secondary impacts of the Japan Earthquake?

A
  • Roads and railways severely damaged. 325km of track washed away
  • 15900 deaths due to tsunami, 93% of deaths caused by drowning
  • 2 nuclear reactors went into meltdown due to flooding, residents evacuated and not returned until 2015
93
Q

What are the secondary impacts of the Haiti Earthquake?

A
  • Water supply system destroyed, cholera outbreak killed over 8000 people
  • The port was destroyed- making it hard to get aid to the area
  • Looting and crime increased as government and police force collapsed
  • Haiti’s importsnt clothing factories destroyed, providing over 60% of exports. 1/5 of jobs lost
94
Q

What was the short term relief for the Japan earthquake?

A
  • International aid and search and rescue teams brought in
  • Transport and communication restored after a couple of weeks
95
Q

What was the short term relief for the Haiti earthquake?

A
  • Emergency aid initially slow with government buildings and the port destroyed
  • UK’s disaster commision raised over £100 million to supply emergency aid
96
Q

What was the long term relief for the Japan earthquake?

A
  • Japanese authorities gave an advanced warning of the earthquake and tsunami, allowing people to prepare and evacuate
  • Not a single building collapsed in Tokyo due to building desig to prevent earthquake damage
97
Q

What was the long term relief for the Haiti earthquake?

A
  • Completely unprepared with no monitering systems in the area
  • 3/4 of damaged buildings inspected and repaired. They now have earthquake resustant buildings and use lighter roofs
98
Q

What was the preperation system for the Japan earthquake?

A
  • Strict building laws help to prevent major damage during an earthquake
  • Buildings reinforced with steel frames to prevent them from collapsing
  • Anual earthquake drills
  • Tsunami walls designed to protect the coast
99
Q

What was the preperation system for the Haiti earthquake?

A
  • No alerts or warning systems to warn resident of the earthquake
  • No consideration of earthquake risks in infrastructure due to lack of resources
100
Q

What was the prediction system for the Japan earthquake?

A
  • The Japan Meteorogical Agency (JMA) and local governments moniter seismic activities
  • If an earthquake is detected, people are warned immediately
101
Q

What was the prediction system for the Haiti earthquake?

A
  • No prediction system or monitering systems set up for the prediction of earthquakes using seismic activity
  • No alerts set up in the case of an earthquake due to lack of infrastrucutre