GCSE

Geography

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  1. Introduction to GCSE Geography (AQA)
  2. 1. Living with the Physical Environment

  3. 1.1 The Challenge of Natural Hazards
  4. 1.2 The Living World
  5. 1.3 Physical Landscapes in the UK
  6. 2. Challenges in the Human Environment
  7. 2.1 Urban Issues and Challenges
  8. 2.2 The Changing Economic World
  9. 2.3 The Challenge of Resource Management
  10. 3. Geographical Applications
  11. 3.1 Issue Evaluation
  12. 3.2 Fieldwork
  13. 4. Geographical Skills
  14. 4.1 Cartographic Skills
  15. 4.2 Graphical Skills
  16. 4.3 Numerical Skills
  17. 4.4 Statistical Skills
  18. 4.5 Use of Qualitative and Quantitative Data
  19. 4.6 Formulate Enquiry and Argument
  20. 4.7 Literacy
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Learning
Study

Tectonic hazards have primary and secondary effects, each often have their own immediate and long-term responses. The effects can also differ, particularly with inequality, we will explore what this can mean with the use of an example. You will only need to give examples of earthquakes or volcanoes, but not both.

Primary and Secondary Effects of Tectonic Hazards

Primary effects refer to the immediate and direct impacts of a tectonic hazard. They can include:

  • Ground shaking and surface rupture during earthquakes, leading to infrastructure damage and collapse.
  • Lava flows and pyroclastic flows during volcanic eruptions, destroying vegetation and infrastructure in their path.
Figure 13. (Left) Lava flows in Hawaii. (Right) Pyroclastic flow at Mayon volcano, 2010.

Secondary effects are the indirect consequences that occur as a result of primary effects. They can include:

  • Landslides, avalanches, or tsunamis triggered by earthquakes or volcanic activity, causing further destruction.
  • Fires, floods, or contamination of water sources due to infrastructure damage, exacerbating the impacts of the initial hazard.
  • Displacement of populations, loss of livelihoods, and social disruptions.
Figure 14. (Left) Avalanche from the Ismoil Somoni Peak, Tajikistan in 1985. (Right) Local residents in Tacloban City, Philippines displaced after Typhoon Haiyan in November 2013.

Immediate and Long-Term Responses to Tectonic Hazards

Immediate responses are actions taken immediately after a tectonic hazard occurs to address the urgent needs of affected communities. They can include:

  • Emergency search and rescue operations to save lives and recover survivors.
  • Provision of medical aid and emergency shelters to meet the basic needs of affected populations.
  • Activation of early warning systems and evacuation plans to minimise casualties.
Figure 16. (Left) Emergency rescue workers during 2011 earthquakes in Van, Turkey. (Right) Early warning system in Japan.

Long-term responses focus on the recovery, reconstruction, and prevention of future impacts. They can include:

  • Rebuilding damaged infrastructure, such as homes, schools, hospitals, and transportation networks.
  • Implementing measures for hazard mitigation, such as constructing earthquake-resistant buildings or implementing land-use planning to reduce vulnerability.
  • Enhancing community resilience through education, awareness campaigns, and training programs.

Contrasting Effects and Responses in Areas of Contrasting Wealth

To illustrate how the effects and responses to tectonic hazards vary between areas with different levels of wealth, let’s consider two examples of earthquakes:

Haiti (Lower Income Country)

The 2010 Haiti earthquake (Richter magnitude 7.0) had devastating consequences due to the country’s limited resources and infrastructure. It resulted in widespread destruction, a high number of casualties, and significant economic and social impacts. 230,000 people died and a further 300,000 were injured. Buildings were damaged, costing around $8 billion.

Figure 17. Flag of Haiti (left) and its location depicted in dark green (right).

Immediate responses involved international humanitarian aid, search and rescue operations, and temporary shelters. However, the long-term recovery process faced challenges due to limited financial resources, inadequate infrastructure, and political instability.

Figure 18. (Left) Damaged buildings in Port-au-Prince, the capital of Haiti. (Right) US emergency aid airdrop in Haiti.

Japan (Developed Country)

Japan experiences frequent earthquakes and volcanic eruptions but has developed robust infrastructure and disaster preparedness measures. As a result, the impacts of tectonic hazards are often mitigated. For example, strict building codes and early warning systems minimise casualties and infrastructure damage in the 2011 earthquake. Even though the earthquake was stronger at a Richter magnitude of 9.0, only 19,000 people died and 6,000 injured.

Figure 19. Flag of Japan (left) and its location depicted in dark green (right).

Japan’s responses to tectonic hazards involve a well-coordinated approach, including efficient emergency response systems, advanced technology for monitoring and early detection, and comprehensive disaster management plans. Reconstruction efforts focus on rapid recovery and the implementation of measures to enhance resilience. 100 million soldiers were immediately mobilised to help with search and rescue missions.

Figure 20. (Left) The aftermath of Japan’s 2011 earthquake in Kesennuma, Miyagi, Japan. (Right) A member of the UK search and rescue team searching a destroyed building in Unosumia, Kamaishi.
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