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18 Cards in this Set

  • Front
  • Back

PSI for the Autralian Big Dry

• Occured in 2002 - 2009


• Driest period in 125 years


• 40% - 60% less rainfall in 2006


• 23,000,000 population


• Water bills increased by 20% in 2008

Social consequences of Australian Big Dry

• People in rural areas left due to a lack of water. This increased pressure on cities (urban areas)


• Rural suicide rates increased

Economic consequences of Australian Big Dry

• Farmers had to sell cattle


• Food prices rose


• Water bills increased by 20% in 2008


• Tourism was negatively affected


• Agricultural production was severely affected


• 10,000 people directly employed by the cotton industry were affected


• The number of dairy farms reduced by more than 50%

Environmental consequences of Australian Big Dry

• Loss of Vegetation


• Grassland turned to scrubland


• Energy from HEP was reduced leading to more pollution as Australia resorted to the use of fossil fuels


• Water quality reduced as toxic algal outbreaks occurred in depleted rivers, dams and lakes

Causes of the Australian Big Dry

• El Niño


• Over population


Too much agriculture

PSI for the Boscastle flooding

• August 2004


• 75mm of rain in 2 hours


• 58 properties, 4 businesses, roads and bridges were destroyed/damaged


• 7 helicopters


• Around 100 people airlifted to safety


• 50 cars washed out to sea


• 90% of economy relies on tourism

Causes of the Boscastle flooding

• 75mm of rain fell in 2 hours


• Low pressure system


• Lots of rain over previous weeks meant ground was wetter and couldn't infiltrate water


• Located in a steep-sided valley close to the confluence of 3 rivers. Water ran very quickly into the river channels


• Old bridge had a low arch, over a narrow river channel. Fallen trees etc formed a dam

Consequences of the Boscastle flooding

58 properties, 4 businesses, roads and bridges were destroyed or damaged


• Flooding was so sudden that people couldn't evacuate or move belongings


• About 50 cars were washed out to sea


• The flood caused the number of tourists to significantly drop


• One person was seriously injured

Responses to the Boscastle flooding

• Emergency services quickly responded to airlift around 100 people to safety


• Residents/tourists flooded out of accommodation were invited into local accommodation and the town hall


• Homes, businesses and roads were eventually rebuilt


• Bridge was rebuilt with a higher arch, so debris is less likely to dam the river


• A £10 million flood defence scheme introduced in 2008, included the widening and deepening of the river to improve flow

PSI for the E16 eruption

• 12th April, second fissure ripped open


• 15th April, glacier burst open


• Cut through 200m of glacial ice


• Constructive plate boundary


• $2.8 billion lost in insurance costs and lost trade (Europe)


• Kenya lost $3.5 million


• Over 95,000 flights cancelled


• Plumes of tephra rose 30,000ft

Causes of the E16 eruption

• Increase in seismic activity


• Earthquakes increasing and beginning shallower, showing that magma was rising


• Ash caused by glacial ice


• Constructive plate boundary

Consequences of the E16 eruption

• Less demand for air fuel, led to an increase in petrol costs in UK and Europe


• 20 farms destroyed


• Health impacts, respiratory problems


• Grounded flights stopped deliveries of food and medicines etc


• Increased amount of tourists


• Could trigger other eruptions


• Disruption cost airlines $200 million per day

Responses to the E16 eruption

• Sophisticated monitoring mechanisms throughout Iceland: satellite imagery, thermal cameras, seismometers etc


• Well-trained National Emergency Agency to co-ordinate recovery and response tactics (replacing bridges etc)


• Other nations had to respond independently, long-term responses could include volcano insurance for travel

PSI for North Norfolk

• In the east of England


• Borders Suffolk, Lincolnshire and Cambridgeshire


• Coast runs for 70km

How human activity, including management, affects the geomorphic processes on the coast of North Norfolk

• Villages sit on higher land to reduce flooding


• At Stiffkey, area of salt marsh has developed to create a natural sea defence, they're low lying but build up as sea level rises


• Groynes slow longshore drift


• Sea walls, rip-rap barriers and gabions

PSI for the River Wye

• 5th longest river in UK, at over 210km


• Source in Plynlimon


• Decends over 700m


• Plynlimon rises nearly 2500ft high

Characteristics of the River Wye

• Runs through V-shaped valleys at the upper course of the river, removed small pieces of sediment


• Waterfalls (were removed)


• Floodplain (below city of Hereford)


• Meanders, can form ox-bow lakes

Management of the River Wye

• 200,000 people live in the Valley, could increase flood risk


• Around 9,000 properties at risk of flooding


• Agriculture


• Industry: tourism, transport, forestry, limestone quarrying