PC Hazards Flashcards

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1
Q

What is a natural hazard?

A

The threat of substantial loss of life, substantial impact upon life or damage to property that can be caused by an natural event.

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2
Q

What is a natural event?

A

A naturally occurring physical incident.

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3
Q

What are the three types of natural hazards?

A

Geophysical - Driven by the Earth’s own internal forces e.g. plate tectonics.

Atmospheric - Driven by processes in the atmosphere.

Hydrological - Driven by water processes.

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4
Q

What are examples of geophysical processes?

A

Seismic activity such as earthquakes and volcanic events.

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5
Q

What are example of atmospheric processes?

A

Tropical storms and droughts.

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6
Q

What are examples of hydrological processes?

A

Floods, storm surges and tsunamis.

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7
Q

What are primary and secondary impacts?

A

Primary - Impacts that have an immediate effect on the affected area. E.g. destruction of buildings and infrastructure.

Secondary - Impacts that occur after a disaster. E.g. spread of disease, contamination of water sources and economic recession.

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8
Q

What is a natural disaster?

A

When a natural event causes substantial loss of life, substantial impact upon life or damage to property.

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9
Q

How does a natural event become a Natural Hazard?

A

If the area at risk has a presence of human life.

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10
Q

What reasons are there for living in areas at high risk of a natural event occurring.

A
  • Fertility of the land e.g. on flood plains and flanks of volcanoes.
  • Economic reasons e.g. jobs and employment.
  • Its where they have always lived.
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11
Q

How does whether the country affected by a hazard is a LIC or HIC affect the severity of the hazard?

A

LIC - Generally more resilient, less economically demanding but higher social and economic costs, secondary affects are worse.

HIC - Generally less resilient, more economically demanding but lower social and economic costs, primary affects are worse.

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12
Q

How does the timing of which a hazard occurs affect the severity of the hazard?

A

The time of year can affect the severity of a hazard due to natural processes which commonly occur during different times in the year e.g. snow in winter.
The time of day can also affect the severity as it is harder to see at night since it is darker.

Both of these factors affect the rescue and evacuation efforts that will occur as a result of a hazard, which can lead to more deaths and longer lasting damage which increases the severity.

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13
Q

How does a countries demographics affect the severity of the hazard that occurs there?

A

A countries demographics can have a large affect on the severity of a hazard as people can be more or less at risk. For example Russia and Japan which are both high in population. However, if an earthquake was to occur in the centre of each country, the severity would be much greater in Japan due to the high population density compared to Russia.

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14
Q

What is the Hazard Management Cycle?

A

The Hazard Management Cycle is a plan used to respond, mitigate and prepare for a hazard. It is split into 4 categories: Response, Recovery, Mitigation and Preparedness. Processes that occur are put into the different categories, e.g. medical care is a response and monitoring of seismic activity is preparedness. This is useful to help countries and communities become more resilient to hazards, e.g. NL and flooding.

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15
Q

What is the Park Model?

A

The Park Model is a model that shows how a country or community has recovered from a hazard. It displays the quality of life against time (which can be hours, days, months or years). When the line is decreasing in gradient it shows the disruption the hazard has caused. When it is increasing in gradient it shows the recovery. The quality of life can be the same, lower or higher than at the start of the model.

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16
Q

What are the 4 layers of the Earth?

A

Crust - Outermost layer of the Earth (Earth’s surface), Varies from 5-10 km thick under the oceans and 70 km under the continents.
Mantle - The widest layer of the Earth, approximately 2900 km thick, the heat and pressure in this region causes the mainly silicate rocks to be liquid which gets denser the deeper you go.
Outer Core - Semi liquid layer made primarily of iron. The 2 layers in the Core can reach 5000 degrees C.
Inner Core - Solid layer made up of an iron-nickel alloy. The 2 layers in the Core can reach 5000 degrees C.

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17
Q

What is the lithosphere?

A

The lithosphere is the outermost layer of the Earth and is approximately 100 km thick. It is made of the crust and the upper most part of the mantle which is solid. The bottom of the lithosphere is jagged and has many gaps of which molten rock or magma fills. This zone is where tectonic plates are formed.

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18
Q

What is the aesthenosphere?

A

This is a plastic-like region just below the lithosphere. The slow movement of the rock in this region can carry the lithosphere causing the tectonic plates to move.

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19
Q

What are the three types of plate margins/boundaries?

A

Constructive - The two plates are moving away from each other.
Destructive - The two plates are moving towards each other.
Conservative - The two plates are sliding past each other.

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20
Q

What is a mid-ocean ridge? Example?

A

Submarine mountain ridges that extend for thousands of kilometres along the ocean floor. These form as a result of constructive plate boundaries that are found along areas of ocean. Submarine volcanic eruptions release magma which rapidly cools when in contact with the oceanic water and forms part of the crust. Ridge push results in the oceanic plate moving further from the ridge, allowing more magma to rise.

An example of this is the Mid-Atlantic Ridge that occurs between the North American and Eurasian plates.

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21
Q

What are ridge push and slab pull?

A

Ridge push - When the higher elevation at a constructive plate boundary causes gravity to push the lithosphere that is further from the ridge.

Slab pull - Following subduction, the lithosphere sinks into the mantle under it’s own weight, helping to ‘pull’ the rest of the plate with it.

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22
Q

What is subduction?

A

A process which occurs when one tectonic plate slides beneath another (destructive boundary), moving down into the mantle. This usually involves oceanic crust sliding beneath continental crust.

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23
Q

What is a rift valley? Example?

A

A valley that is formed as a result of a constructive plate boundary between 2 continental crusts.

An example of this is the Great Rift Valley that occurs between the Somalian and African (Nubian) plates.

24
Q

What is a hotspot?

A

An area of the outer core of the Earth that is of a greater temperature than the surrounding outer core. This can cause a super plume to form.

25
Q

What is a super plume?

A

The rapid rising of magma in the mantle due to extreme heat. This is mostly as a result of a hotspot.

26
Q

What are the 7 different types of volcanic eruptions? What are the differences?

A

Icelandic:

  • Basaltic magma
  • Lava flows gently from fissures

Hawaiian:

  • Basaltic magma
  • Lava flows gently from a central vent

Strombolian:

  • (Thicker) Basaltic magma
  • Frequent explosive eruptions of tephra and steam
  • Occasionally short lava flows

Vulcanian:

  • (Thicker) Basaltic, andesitic and rhyolitic magma
  • Less frequent, but more violent eruptions of gases, ash and tephra (including lapilli)

Vesuvian:

  • (Thicker) Basaltic, andesitic and rhyolitic magma
  • Following long periods of inactivity, very violent gas explosions blast ash high into the sky

Peléean:

  • Andesitic and rhyolitic magma
  • Very violent eruptions of nuées ardentes

Plinian:

  • Rhyolitic magma
  • Exceptionally violent eruptions of gases, ash and pumice. Torrential rainstorms cause devastating lahars.
27
Q

What is a lahar?

A

Mudflow comprised mainly of volcanic ash mixed with water from a crater lake, snowmelt, glacier melt or prolonged torrential rain.

28
Q

What is a fissure?

A

A linear volcanic vent through which lava erupts.

29
Q

What is tephra?

A

Pyroclastic material that ranges in size from dust to blocks the size of cars

30
Q

What is a pyroclastic flow?

A

A fast-moving current of hot gas and rock (tephra), which reaches speeds moving away from a volcano of up to 700 km/h. These normally hug the ground and travel downhill.

31
Q

What are the different types of volcano?

A
  • Fissure
  • Basic Shield
  • Acid Dome
  • Composite cone
  • Ash cinder
  • Caldera
32
Q

What equipment can be used to monitor and predict volcanic eruptions? What do they monitor and what does this indicate?

A

Seismometer:

  • Monitors seismic activity around the volcano
  • Mini-earthquakes can occur prior to an eruption, so this can indicate when a volcano is about to erupt

Tiltmeter:

  • Monitors the angle of the slope
  • Indicates if there are any magma bulges forming on the sides of the volcano.
  • Indicates an increase in pressure

Gas Boxes:

  • Monitors the gas released by the volcano
  • Higher concentrations of SO₂ indicate an eruption will occur

Magnetometer:

  • Monitors the changes in the magnetic field
  • A stronger magnetic field indicates more magma is in the magma chamber due to the increased concentration of iron.

Cameras:

  • Monitors the lava level
  • A higher lava level indicates there is more pressure in the magma chamber
33
Q

Mt Etna Case Study (Volcano)

A

About:

  • Altitude of 3350m and covers 1250 km²
  • Strato-volcano with a conical shape
  • Europe’s most active volcano
  • 900,000 people live on the fertile slopes
  • Formed by the collision of the African and Eurasian plates
  • Most eruptions are effusive (low-viscosity lava flows) with some mild strombolian

Impacts:

  • Lava flow threatened to destroy key buildings such as the Astrophysics Observatory (Mar 1983)
  • The town of Zafferana Etnea was threatened by the largest volume of lava in 100+ years (Dec 1991 - Mar 1993)
  • Significant damage to tourist facilities (Jul-Aug 2001)
  • Catania Airport forced to close due to ash (Jul-Aug 2001)

Responses:

  • Creation of huge earthworks to redirect lava flow (Mar 1983)
  • Earth dam built to hold the lava flow (Dec 1991 - Mar 1993)
  • Lava channels plugged with concrete blocks (Dec 1991 - Mar 1993)
  • Explosives used to make human-made channels for the lava to flow into (Dec 1991 - Mar 1993)
34
Q

Tōhoku Case Study (Earthquake + Tsunami)

A

About:

  • East of the city of Sendai, on the island of Honshu, Japan
  • Occurred 11 March 2011
  • Occurred under when a 400-500km part of the North American plate that was dragged under by the subducting Pacific plate, slipped upwards by 5-10m
  • Magnitude 9.0
  • Moved the entire islands closer to North America
  • Shifted the Earth’s tilt by at least 10cm
  • The first tsunami wave hit 30mins after the earthquake
  • 3000km of coastline was hit
  • The waves reached a height of 10m and flooded up to 10km inland

Impacts:

  • Buildings collapsed due to the earthquake. Some even set on fire due to broken gas & petrol pipes
  • Almost 500km² was flooded
  • Over 18,000 people died or went missing
  • 500,000 people were made homeless
  • 1,000,000 homes lost running water & 6,000,000 homes lost electricity
  • Shortages of food, water, fuel and medical supplies
  • 3 of the 4 nuclear reactors at Fukushima Daiichi overheated and exploded releasing radioactive material into the air

Responses:

  • 150,000 people lived in temporary shelters
  • 100,000 soldiers were mobilised to establish order and distribute aid
  • International aid came from countries such as USA & China, including 63 S&R specialists, 2 rescue dogs and a medical team from the UK
  • The majority of Japanese nuclear power plants closed down
  • An exclusion zone was set up around Fukushima, with homes evacuated and iodine tablets (that prevent radiation sickness) distributed
  • In 2013, a new upgraded tsunami warning was unveiled as many people thought the tsunami would be as small as previous ones
  • Contingency planning took place to decide whether coastal defences should be built for future high magnitude, low frequency events
35
Q

Alberta Wildfire Case Study (Wildfire)

A

About:

  • Occurred in May 2016
  • 90,000 residents of Fort McMurray were evacuated
  • 600,000 ha (hectares) of land was burned
  • 0 direct injuries or deaths from the fire
  • 2,400 homes and businesses destroyed
  • 85% of the city was saved
  • Largely as a result of favourable weather conditions (low winter snowfall, early snowmelt, high temps of 30ᵒc in May, and a strong El Niño effect)
  • The fire created its own weather conditions (Mainly causing lightning which sparked additional wildfires)

Impacts:

  • Dry and scorched peaty soils could reignite until the first heavy rainfall (not safe for people to return)
  • Several million tonnes of CO₂ was released into the atmosphere
  • Ash washed into the water supplies making it unsuitable for drinking, and contaminating fish & other aquatic wildlife
  • Jobs and livelihoods were affected and movement in the area was restricted
  • Power supplies were disrupted
  • Almost 8,500 workers in the nearby oil sands industry had to be evacuated.
  • Initial insurance costs was $9 billion
  • The fire cost an estimate of $1 billion to the oil industry
  • The fire fuelled political debates about the impacts of climate change and increased vulnerability in the future

Responses:

  • A mass evacuation plan was implemented to escort the town’s population to safety
  • Aircraft was used to evacuate some oil sands workers
  • A state of emergency was declared triggering a response from the Canadian armed forces, with helicopters, water bombers and firefighters being brought in from neighbouring states
  • The Alberta government provided $1,250 to all adults and $500 to all dependants to cover living expenses in the immediate aftermath
  • $50 million was raised by the Canadian Red Cross
36
Q

Hurricane Sandy (USA, 2012) & Cyclone Winston (Fiji, 2016) Case Study

A

About:

  • Sandy started in the Caribbean Sea and travelled North over Jamaica, Cuba and The Bahamas before hitting into the East coast of the USA in New Jersey
  • Winston started NW of Fiji in the Pacific Ocean and travelled S, then NE, then W where it hit the main island of Fiji
  • Sandy became a category 3 hurricane before it merged with a cold weather system where it became an ‘extra-tropical cyclone’
  • Winston reached category 5 on the Saffir-Simpson scale when it hit Fiji

Impacts:

  • Sandy left 70% of the Jamaican population without electricity, 200,000 people in Haiti homeless and 15,000 people in Cuba homeless
  • Winston destroyed 40,000 homes and killed 44 people and left 131,000 people in need of immediate shelter
  • Sandy did $75 billion worth of damage to the USA, making it the second most costly storm after Hurricane Katrina
  • Winston did $1.4 billion worth of damage
  • Sandy affected 24 US states leaving thousands homeless and millions without electricity
  • Winston destroyed 80% of the countries electricity lines, resulting in the islands losing communication for several days (hindering S&R efforts)

Responses:

  • (Sandy) Food, water and shelter was the immediate focus with the UN sending supplies for 500,000 people to Cuba
  • (Winston) Food, water and shelter was the main priority, some of which was provided by international governments and NGOs, which also provided financial support
  • (Sandy) In the USA, power companies slowly restored electricity to the affected areas
  • (Winston) The international airport opened after 2 days allowing supplies to be airlifted from Australia & New Zealand
  • (Sandy) $37 million was raised by US agencies to help the affected people, as well as an extra $50 million funded by the US government
  • (Winston) Over $10 million was received as aid to help rebuild, with an additional $9 million from the Fijian government to provide financial aid to 40,000 people
  • (Sandy) In 2013 rebuilding efforts continued, however still an estimated 30,000 inhabitants of New York & New Jersey remained displaced
  • (Winston) The Fijian government launched the ‘Help for Homes’ programme, to help rebuild the houses of low-income families who were unable to afford reconstruction costs

Comparisons:

  • Winston reached a higher category tropical storm than Sandy, however affected less countries and therefore less people
  • Sandy affected many LICs but also affected a HIC (USA) and therefore resulted in a lot more damage than Winston
  • Relief efforts after Winston was more effective as Fiji is an LIC and is therefore more resilient (Help for Homes compared to 30,000 still displaced 1 year after)
37
Q

What are the different types of shockwaves in an earthquake?

A

Primary/Pressure (P) - These are the fastest waves to reach the surface and travel through the crust, mantle and core. These are high-frequency waves that move in a straight line and create compressions.

Secondary/Shear (S) - These are high-frequency waves that shake side to side (like a skipping rope) and travel through the crust and mantle.

Surface Love (L) - These are the slowest waves but most damaging. These move the crust side to side from the epicentre and work in tandem with Rayleigh waves.

Rayleigh (R) - These waves move in a low-frequency rolling motion from the epicentre.

38
Q

How many different types of shockwaves are there? What are they?

A
  • Primary/Pressure
  • Secondary/Shear
  • Surface Love
  • Rayleigh
39
Q

What is seismicity?

A

The frequency and distribution of earthquakes in an area

40
Q

What can cause seismicity?

A

Human activities - Mining, fracking or reservoir construction

Physical activities - Plate tectonics (main cause)

41
Q

How do tsunamis occur?

A

The main cause for tsunamis is when an earthquake occurs under the ocean a tsunami occurs. This is because the sea bed is disrupted causing high energy waves that have a large wavelength and low wave height which travel in all directions. When the wave nears the coastline, friction with the sea bed causes the wave to become more elliptical and change shape to have a low wavelength and high wave height.

However, underwater volcanic eruptions, landslides into the water, landslides underwater and meteor strikes in the water can also cause tsunamis in the same fashion as earthquakes.

42
Q

How do earthquakes occur at each plate boundary?

A

Constructive - Earthquakes occur close to the surface and very narrow to plate boundary when the plates move apart and magma rushes up.

Destructive - As the denser plate subducts under the other less dense plate, a series of shallow and deep earthquakes occur as a result of the friction.

Conservative - As the plates slide past each other, friction builds up until there is a large jolt in which the energy is released and an earthquake occurs.

43
Q

What events can occur before an earthquake strikes that indicates it will strike in the near future?

A
  • Microearthquakes
  • Bulging of the ground
  • Decreasing radon gas concentrations in groundwater
  • Raised groundwater levels
  • Electrical and magnetic changes in local rocks
  • Increased argon gas content in the soil
  • Strange/unusual animal behaviour
44
Q

What are the Richter scale and Modified Mercalli Intensity scale?

A

Richter - A logarithmic scale used to display the magnitude of an earthquake. It starts at 0 and reaches 10, with each number 10x larger than the previous.

Modified Mercalli Intensity (MMI) - A scale used to display the impact of an earthquake. It ranges I (1) - XII (12) with increasing severity. Each number signifies a different impact (e.g. IV - Moderate, is likely to rattle doors and windows or VIII - Destructive, will cause considerable damage. Chimneys and monuments will fall).

45
Q

How can buildings be protected from earthquakes?

A
  • Rubber shock absorbers between the foundation and superstructure
  • Reinforced latticework foundations deep in bedrock
  • ‘Birdcage’ interlocking steel framework
  • Reinforced lift shafts with tensioned cables
  • Panels of marble and glass flexibly anchored to the steel superstructure
  • Rolling weights in the roof to counteract shock waves
46
Q

What are characteristics of tropical storms?

A
  • Average wind speeds in excess of 120 km/h
  • Can be 500km wide
  • Becomes more intense towards the middle
  • The ‘eye of the storm’ is a region of calm in the middle, with the most intense conditions occurring just outside in the eye wall
  • Large number of waves of wind & rain
  • Form in areas of ocean with temperatures of 27ᵒC or higher
47
Q

Where are tropical storms distributed?

A

Tropical storms form between 5-20 degrees latitude above warm oceans. Therefore, they only occur around the Caribbean, Pacific, South-East Asia and the Indian Ocean.

Tropical storms have different names dependant on where they are found. Hurricanes are found in the Caribbean & North-East Pacific. Typhoons are found in South-East Asia & North-West Pacific. Cyclones are found in the Indian Ocean & South-West Pacific.

48
Q

How do tropical storms form?

A

Tropical storms form when a cluster of thunderstorms meet above water of 27ᵒC or higher. The high water temperatures causes evaporation leading to air and water vapour rising into the atmosphere and causing the storm to grow. The Coriolis effect causes surrounding air to rush in and replace the rising air.

49
Q

What is the Coriolis effect?

A

The influence of the Earth’s rotation on the surface.

This causes the distinct spinning characteristic of tropical storms.

50
Q

What is the ITCZ?

A

The Intertropical Convergence Zone is the area where the North-East and South-East trade winds converge. This creates an area of calmness.

Tropical storms tend to form here due to the warm water and low wind speeds, as well as the influx of air from the trade winds.

51
Q

What are the hazards that come with tropical storms?

A
  • Strong winds
  • Storm surges
  • Coastal and river flooding
  • Landslides
52
Q

What is the scale used to measure how severe (what category) a tropical storm is?

A

The Saffir-Simpson Scale

53
Q

What are preparedness, mitigation, prevention and adaptation to natural events?

A

Preparedness - Increasing people’s awareness and understanding of safety measures of hazards to minimise the impacts.

Mitigation - Actions to reduce the severity of the hazard, which can include direct intervention (e.g. earthquake proof homes) or post-event support (e.g. aid and insurance).

Prevention - Actions aimed at preventing large-scale events from occurring (e.g. Smoky the bear (wildfires) or stopping mass mining (earthquakes)).

Adaptation - Accepting that natural events are inevitable and adapting our behaviour accordingly.

54
Q

What are primary and secondary impacts?

A

Primary - Initial and direct impacts of an event (e.g. a tropical storm)

Secondary - Impacts that occur as a result of primary impacts

55
Q

What are environmental, social, economic and political impacts?

A

Environmental - A range of impacts on the natural world (e.g. loss of wildlife or pollution).

Social - Impacts on people and their everyday lives (e.g. death or homelessness).

Economic - The financial costs of an event to local people and governments.

Political - Governmental issues in a country (e.g. receiving international aid or political collapse).