Before and after: how the 2011 earthquake changed Christchurch
Many parts of central Christchurch are unrecognisable now
Christchurch mayor Lianne Dalziel was born and raised in the city she now represents. But she finds it hard to describe how it has changed since the earthquake.
“I don’t know whether it’s a post-disaster thing,” Dalziel says. “But for me, it’s sometimes hard to remember what was there before.”
Many Christchurch residents say the same. Their home has undergone enormous transformation in the past 10 years after a 6.3-magnitude earthquake killed 185 people , disrupted tens of thousands of lives and reduced 80% of the city centre to rubble.
Today, the streets of Christchurch are bustling, following a period of sustained construction: first, commercial development of glass-fronted office blocks and high-end retail space – and then civic and cultural buildings, which were either restored or replaced.
Though the rebuild is ongoing, traces of the destruction – fenced-off broken buildings and sports field-size stretches of land slated for development – are more likely to be noticed by tourists than locals, who know how far the city has come.
“Every now and then I get to see the city through the eyes of people who are visiting here for the first time in a long time, and hear their excitement about … what it’s becoming,” says Dalziel.
After 10 years, Christchurch is no longer, first and foremost, an earthquake-damaged city – but progress to this point has been slow and hard-won. In 2013, the cost of the recovery was put at $40bn; it was likely more.
Asked about the missed opportunities of the rebuild, Dalziel laughs. “How long have you got?”
Stressing the advantage of hindsight, Dalizel – who was elected in October 2013, nearly three years after the quake – says agencies could have been better aligned.
For example, individual telco and power companies took different approaches to repairing damaged infrastructure from the council, meaning the same roads were dug up many times.
Those lessons of the Stronger Christchurch Infrastructure Rebuild Team (SCIRT) have been made publicly available for the benefit of other cities facing a post-disaster rebuild, Dalziel says.
But the defining problem of the rebuild was the relationship between local and national government.
On 1 May 2011, the national government established the Canterbury Earthquake Recovery Authority (Cera) , a public service bureaucracy with wide-ranging powers to lead its response to the recovery – including over local authorities.
The approach taken by Cera led to widespread discontent, with both the council and residents feeling sidelined.
Dalziel suggests the central government and council could instead have set up an independent entity to operate together, appointing directors that were accountable to both of them.
In April 2012, a unit within Cera took over responsibility for the rebuild of the central city, making its own version of the council’s draft recovery plan – what became known as “the blueprint”.
It was based on dedicated precincts, such as for innovation, health and performing arts; and “anchor projects” that, it was hoped, would encourage organic investment. (One, for a “sustainable village”, was finally abandoned last week.)
But local knowledge from the council’s public consultation was lost, says Dalziel. The blueprint “wasn’t of the city; it was a creature of government”. Cera itself was disbanded in 2016.
Meanwhile, the council approached the task of a new central library, Tūranga, with granular attention to community engagement: one resident’s suggestion of a “Harry Potter staircase” was reflected in the finished building, which opened in October 2018.
It is widely considered one of the triumphs of the rebuild, frequented by a wide cross-section of the Christchurch population – often indicative of a genuine attention to diversity and inclusion in the design process.
That kind of civic-mindedness seemed absent in the first buildings to spring up after the earthquake, spurred by private investment. For a time, Christchurch’s inner city was dominated by low-rise commercial developments made of glass and steel, such as the Deloitte and PWC buildings.
Hundreds of heritage buildings were lost – either to the earthquake, or the demolition drive to move on from it.
The town hall and Edwardian-era Isaac Theatre Royal have both been restored and reopened; but demolition of the Christchurch Basilica, which first opened its doors in 1905, began only in December. (Construction of its replacement has been delayed by rare seagulls nesting on the Armagh St site.)
The city’s cultural renewal was led by grassroots groups such as Greening the Rubble, Gap Filler and Agropolis, which set up small, often temporary “soft infrastructure” projects to revitalise the city at a street level, and a human one.
A coin-operated community dancefloor , gardens in vacant lots and other displays of the “ingenuity of its hardy residents” was highlighted by the New York Times in naming Christchurch its second-best place to travel to in 2014 . It was singled out again last year .
Gap Filler is now a partner in a major residential project, led by Fletcher Living covering six blocks in the inner city.
The One Central development is central to the blueprint’s bid to increase the residential population of central Christchurch – but sales got off to a slow start , prompting concern that construction may be outpacing demand.
It speaks to the evolving challenge of the rebuild. Central Christchurch is unrecognisable from the disaster zone it was post-quake, and significantly changed from how it was even five years ago. And the city it is yet to become is still emerging.
Regardless of what has been built so far, Dalziel says: “We are absolutely the best city for the future … From every disaster, any crisis, there is always opportunity – Christchurch has all of its opportunity in front of us, and people can now see it.”
For her, the new Christchurch is most evident along the banks of the Avon river: home to the new Riverside indoor market, an indie theatre, and a hip new hospitality development.
“If I walk by on a summer evening, it’s just filled with people: in the bars and restaurants, family groups, out walking and cycling – it’s got this blissful feel to it … You’d never want to go back to the way it was.”
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Teacher guidance
Kaiako must ensure that ākonga are clear about the purpose for exploring the spatial distribution of a phenomenon. For example, the significance of where earthquakes occur in Aotearoa New Zealand or globally, and their proximity to urban centres and rural communities.
Prior to the assessment, kaiako could:
- explore examples of the spatial distribution of a phenomenon using unrelated topics
- consider a range of different factors and processes that determine the spatial distribution of unrelated topics. For example, this could include global examples that explore the spatial distribution of volcanoes or deserts.
- explore tectonic processes that have helped to shape the landscape(s) of your chosen context
- explore examples of earthquakes and impacts they have on place.
If the chosen context for the Assessment Activity is Aotearoa New Zealand:
- explore concepts, values, and knowledge within mātauranga Māori related to the spatial distribution of different phenomena and their impacts within te taiao
- seek opportunities to connect their ākonga with local knowledge holders in a collaborative setting, to gain understanding and evidence about the phenomenon and its impacts on place. Knowledge holders could be kaumatua, rangatira, council, or organisations.
Possible resources for Aotearoa New Zealand:
- Earthquakes (GNS Science) .
- Our plate boundary (GNS Science) .
- The big ones (Alpine Fault Magnitude 8) .
- Story: Earthquakes (Te Ara — The Encyclopedia of New Zealand) .
- Christchurch earthquake case study (Internet Geography) .
- Recent quakes (GeoNet) .
Possible resources for global distribution of earthquakes:
- Earthquakes (BBC) .
- Earthquakes (National Geographic) .
- Where do earthquakes occur? (British Geological Survey) .
- Where do earthquakes occur? (U.S. Geological Survey) .
- Turkey Earthquake: Where did it hit and why was it so deadly? (BBC) .
- Haiti earthquake: Facts, FAQs, and how to help (World Vision) .
Kaiako should also:
- determine the timing of the assessment event
- provide assessment resources for ākonga to complete the Assessment Activity successfully.
Ākonga may:
- work together in a group to explore their learning, but they must individually present their work to show they have met all of the requirements of the Standard
- work on their assessment in and out of class time over the assessment period specified by the kaiako.
While this Assessment Activity focuses on the phenomenon of earthquakes, kaiako may choose to focus on a different phenomenon that is of interest or relevance to ākonga, using the same approach as shown in this Assessment Activity.
Assessment schedule
[ file resource ].
- Title: GO 1.1c Assessment Schedule 1 (Aotearoa New Zealand)
- Description: GO 1.1c Assessment Schedule 1 (Aotearoa New Zealand)
- File URL: https://ncea-live-3-storagestack-53q-assetstorages3bucket-2o21xte0r81u.s3.amazonaws.com/s3fs-public/2023-12/GO%201.1c%20Aotearoa%20NZ%20Assessment%20Schedule.docx?VersionId=aTPpycOoGBWCkQOv7TkiR_UYVFLhruq.
- File Extension: docx
- File Size: 64KB
- GO 1.1c Assessment Schedule 1 (Aotearoa New Zealand).docx
GO 1.1c Assessment Schedule 1 (Aotearoa New Zealand)
- Title: GO 1.1c Assessment Schedule 2 (Global)
- Description: GO 1.1c Assessment Schedule 2 (Global)
- File URL: https://ncea-live-3-storagestack-53q-assetstorages3bucket-2o21xte0r81u.s3.amazonaws.com/s3fs-public/2023-12/GO%201.1c%20Global%20Assessment%20Schedule.docx?VersionId=o9Eat1UiuKlvUeWh69ZumZU_okVVb.0P
- GO 1.1c Assessment Schedule 2 (Global).docx
GO 1.1c Assessment Schedule 2 (Global)
Assessment Activity thumbnail image from Fitzgerald Avenue 94 © Schwede66, CC BY-SA 3.0
Christchurch Case study
The Christchurch earthquake of February 2011
- The earthquake occurred on New Zealand’s South Island 10km to the West of Christchurch, Canterbury. It lasted only 10 seconds.
- The earthquake happened on a conservative plate margin between the Pacific Plate and the Australian Plate.
- The epicentre of the quake was just 2km west of the port town of Lyttelton
- It measured 6.3 on the Richter Magnitude scale.
- Christchurch is New Zealand’s second largest city and suffered extensive damage
- Killed 185 people
- The earthquake was only 5 km deep
- The earthquake struck at 12:51 pm on Tuesday, 22 February, 2011
- 6 months earlier on 4th September 2010 another massive magnitude 7.1 earthquake caused significant damage to Christchurch and the central Canterbury region, but with no direct fatalities.
Tectonic setting & Cause
The earthquake was created along a conservative plate margin where the Pacific Plate slid past the Australian Plate in the opposite direction. Where the plates move like this strain energy builds up as the plates lock in place, it reaches a critical level then is breaks, releasing seismic energy. The earthquake occurred on a fault running off this major plate boundary. It was a strike slip event along the fault, mostly horizontal movement with some vertical movement upwards. The earthquake generated its own significant aftershocks;
- 2 Hours after the main earthquake - Largest aftershock of magnitude 5.9
- The first week post event - 361+ aftershocks (magnitude 3+ foreshocks) in the first week
EFFECTS OF THE FEBRUARY 2011 EARTHQUAKE
Primary effects (caused directly by the earthquake)
- 185 people were killed in the earthquake. Over half of the deaths occurred in the six-storey Canterbury Television (CTV) Building, which collapsed and caught fire in the quake.
- 3,129 people injured
- April 2013, the total estimated cost had ballooned to $40 billion
- Significant liquefaction affected the eastern suburbs, producing around 400,000 tonnes of silt
- Building damage to the central city and eastern suburbs of Christchurch. The damage was made worse by buildings and infrastructure already being weakened by the 4 September 2010 earthquake and its aftershock. Up to 100,000 buildings were damaged and about 10,000 buildings needed to be demolished.
- 3.5 m tsunami waves in Tasman Lake, following quake-triggered glacier calving from Tasman Glacier
- Water pipes, roads, bridges, power lines, cell phone towers and ordinary phone lines were broken or damaged.
- 50% + of Central City buildings severely damaged including the city’s cathedral which lost its spire
Secondary effects (things that happen after the primary effects but often as a result of them)
- Some economists have estimated it will take the New Zealand economy 50 to 100 years to completely recover.
- 80% of the water and sewerage system was severely damaged
- An additional 1,293 people were injured in the aftermath
- Psychological impacts – in a survey post event (2013) 80% of respondents stated their lives had changed significantly since the earthquakes. Almost a third said the earthquakes had caused them financial problems, while 64% said they felt guilty that other Cantabrians were more affected by the earthquakes.
- Outmigration of a fifth of the city population
- The population, which had been growing for decades, declined in the years after the quake
- Damage to roads through liquefaction made it difficult for people and emergency services to move around
- Christchurch could no longer host Rugby World Cup matches so lost the benefits, e.g. tourism and income
- Schools had to join together
- Rescue crews from all over the world came to help. There were crews from Japan, the United States, the United Kingdom, Taiwan, Australia and other countries.
- Aid money poured in – Australia gave $5 million (Aus $) in aid.
- The government declared a state of national emergency, which stayed in force until 30 April 2011
- Domestic help was available - The Farmy Army was made up of 800 farmers who brought their farm machines and muscle to help clean up the city.
- The most vulnerable people were cared for and people were kept safe away from dangerous buildings
- Chemical toilets were provided for 30,000 residents
- The Red Cross and other charities supplied aid workers
- More than 300 Australian police officers flew into Christchurch three days after the earthquake.
- The government provided temporary housing and ensured all damaged housing was kept water tight
- Water and sewerage was restored for all residents by August
- Roads and houses were cleared of silt from liquefaction by August and 80% of roads & 50% of footpaths were repaired
- Many Non-government organisations including Save the Children helped with long term recovery efforts
- Canterbury Earthquake Recovery Authority was created to organise the REBUILD of the region. It had special powers to change planning laws and regulations.
Green Zone land was undamaged and could be built on again. Orange Zone more checks were needed before the land could be built on. White Zone was the area that had not been checked at all yet. Red Zone areas were very unstable: building on it safely would be difficult.
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Case Study: Christchurch, New Zealand Earthquake
Earthquake case study - christchurch, new zealand.
Two earthquakes hit the city of Christchurch, on New Zealand's south-east coast, in late 2010/early 2011. The second one hit the city centre, killing 185 and destroying much of the CBD.
1st earthquake (4/9/10)
- Magnitude 7.1.
- People were asleep and the streets mostly empty.
- Buildings were weakened, which became an issue in the 2nd earthquake.
- E.g. 'Turtle safe' - an earthquake safety resource aimed at preschool children which encourages them to act like a turtle during an earthquake.
2nd earthquake (22/2/11) facts
- Magnitude 6.3, hit closer to the CBD than the first earthquake.
- Thousands of people were out and about at work and school.
- The city centre was busy.
- 130 deaths caused by the collapsing of the Canterbury TV and Pyne Gould Corporation buildings.
2nd earthquake damage
- The Provincial Council Chambers and the Anglican Christchurch Cathedral were completely destroyed.
- Over half of the buildings in the central business district have been (intentionally) demolished since as they were no longer safe, including the Hotel Grand Chancellor.
- Liquefaction sludge moved upwards through cracks in residential streets.
- Water and sewage from broken pipes flooded the streets.
- Several thousand homes in the 'red zone' were demolished because they could no longer be safely inhabited.
2nd earthquake responses
- State of emergency declared by national government on 23rd February.
- Christchurch's CBD was cordoned off until June 2013 in some locations.
- 75% of power reinstated within 96 hours.
- Local residents and the creative community have been taking over the 'empty spaces' in the CBD with art installations and street art.
1 Geography Skills
1.1 Mapping
1.1.1 Map Making
1.1.2 OS Maps
1.1.3 Grid References
1.1.4 Contour Lines
1.1.5 Symbols, Scale and Distance
1.1.6 Directions on Maps
1.1.7 Describing Routes
1.1.8 Map Projections
1.1.9 Aerial & Satellite Images
1.1.10 Using Maps to Make Decisions
1.2 Geographical Information Systems
1.2.1 Geographical Information Systems
1.2.2 How do Geographical Information Systems Work?
1.2.3 Using Geographical Information Systems
1.2.4 End of Topic Test - Geography Skills
2 Geology of the UK
2.1 The UK's Rocks
2.1.1 The UK's Main Rock Types
2.1.2 The UK's Landscape
2.1.3 Using Rocks
2.1.4 Weathering
2.2 Case Study: The Peak District
2.2.1 The Peak District
2.2.2 Limestone Landforms
2.2.3 Quarrying
3 Geography of the World
3.1 Geography of America & Europe
3.1.1 North America
3.1.2 South America
3.1.3 Europe
3.1.4 The European Union
3.1.5 The Continents
3.1.6 The Oceans
3.1.7 Longitude
3.1.8 Latitude
3.1.9 End of Topic Test - Geography of the World
4 Development
4.1 Development
4.1.1 Classifying Development
4.1.3 Evaluation of GDP
4.1.4 The Human Development Index
4.1.5 Population Structure
4.1.6 Developing Countries
4.1.7 Emerging Countries
4.1.8 Developed Countries
4.1.9 Comparing Development
4.2 Uneven Development
4.2.1 Consequences of Uneven Development
4.2.2 Physical Factors Affecting Development
4.2.3 Historic Factors Affecting Development
4.2.4 Human & Social Factors Affecting Development
4.2.5 Breaking Out of the Poverty Cycle
4.3 Case Study: Democratic Republic of Congo
4.3.1 The DRC: An Overview
4.3.2 Political & Social Factors Affecting Development
4.3.3 Environmental Factors Affecting the DRC
4.3.4 The DRC: Aid
4.3.5 The Pros & Cons of Aid in DRC
4.3.6 Top-Down vs Bottom-Up in DRC
4.3.7 The DRC: Comparison with the UK
4.3.8 The DRC: Against Malaria Foundation
4.4 Case Study: Nigeria
4.4.1 The Importance & Development of Nigeria
4.4.2 Nigeria's Relationships with the Rest of the World
4.4.3 Urban Growth in Lagos
4.4.4 Population Growth in Lagos
4.4.5 Factors influencing Nigeria's Growth
4.4.6 Nigeria: Comparison with the UK
5 Weather & Climate
5.1 Weather
5.1.1 Weather & Climate
5.1.2 Components of Weather
5.1.3 Temperature
5.1.4 Sunshine, Humidity & Air Pressure
5.1.5 Cloud Cover
5.1.6 Precipitation
5.1.7 Convectional Precipitation
5.1.8 Frontal Precipitation
5.1.9 Relief or Orographic Precipitation
5.1.10 Wind
5.1.11 Extreme Wind
5.1.12 Recording the Weather
5.1.13 Extreme Weather
5.2 Climate
5.2.1 Climate of the British Isles
5.2.2 Comparing Weather & Climate London
5.2.3 Climate of the Tropical Rainforest
5.2.4 End of Topic Test - Weather & Climate
5.3 Tropical Storms
5.3.1 Formation of Tropical Storms
5.3.2 Features of Tropical Storms
5.3.3 The Structure of Tropical Storms
5.3.4 Tropical Storms Case Study: Katrina Effects
5.3.5 Tropical Storms Case Study: Katrina Responses
6 The World of Work
6.1 Tourism
6.1.1 Landscapes
6.1.2 The Growth of Tourism
6.1.3 Benefits of Tourism
6.1.4 Economic Costs of Tourism
6.1.5 Social, Cultural & Environmental Costs of Tourism
6.1.6 Tourism Case Study: Blackpool
6.1.7 Ecotourism
6.1.8 Tourism Case Study: Kenya
7 Natural Resources
7.1.1 What are Rocks?
7.1.2 Types of Rock
7.1.4 The Rock Cycle - Weathering
7.1.5 The Rock Cycle - Erosion
7.1.6 What is Soil?
7.1.7 Soil Profiles
7.1.8 Water
7.1.9 Global Water Demand
7.2 Fossil Fuels
7.2.1 Introduction to Fossil Fuels
7.2.2 Fossil Fuels
7.2.3 The Global Energy Supply
7.2.5 What is Peak Oil?
7.2.6 End of Topic Test - Natural Resources
8.1 River Processes & Landforms
8.1.1 Overview of Rivers
8.1.2 The Bradshaw Model
8.1.3 Erosion
8.1.4 Sediment Transport
8.1.5 River Deposition
8.1.6 River Profiles: Long Profiles
8.1.7 River Profiles: Cross Profiles
8.1.8 Waterfalls & Gorges
8.1.9 Interlocking Spurs
8.1.10 Meanders
8.1.11 Floodplains
8.1.12 Levees
8.1.13 Case Study: River Tees
8.2 Rivers & Flooding
8.2.1 Flood Risk Factors
8.2.2 Flood Management: Hard Engineering
8.2.3 Flood Management: Soft Engineering
8.2.4 Flooding Case Study: Boscastle
8.2.5 Flooding Case Study: Consequences of Boscastle
8.2.6 Flooding Case Study: Responses to Boscastle
8.2.7 Flooding Case Study: Bangladesh
8.2.8 End of Topic Test - Rivers
8.2.9 Rivers Case Study: The Nile
8.2.10 Rivers Case Study: The Mississippi
9.1 Formation of Coastal Landforms
9.1.1 Weathering
9.1.2 Erosion
9.1.3 Headlands & Bays
9.1.4 Caves, Arches & Stacks
9.1.5 Wave-Cut Platforms & Cliffs
9.1.6 Waves
9.1.7 Longshore Drift
9.1.8 Coastal Deposition
9.1.9 Spits, Bars & Sand Dunes
9.2 Coast Management
9.2.1 Management Strategies for Coastal Erosion
9.2.2 Case Study: The Holderness Coast
9.2.3 Case Study: Lyme Regis
9.2.4 End of Topic Test - Coasts
10 Glaciers
10.1 Overview of Glaciers & How They Work
10.1.1 Distribution of Glaciers
10.1.2 Types of Glaciers
10.1.3 The Last Ice Age
10.1.4 Formation & Movement of Glaciers
10.1.5 Shaping of Landscapes by Glaciers
10.1.6 Glacial Landforms Created by Erosion
10.1.7 Glacial Till & Outwash Plain
10.1.8 Moraines
10.1.9 Drumlins & Erratics
10.1.10 End of Topic Tests - Glaciers
10.1.11 Tourism in Glacial Landscapes
10.1.12 Strategies for Coping with Tourists
10.1.13 Case Study - Lake District: Tourism
10.1.14 Case Study - Lake District: Management
11 Tectonics
11.1 Continental Drift & Plate Tectonics
11.1.1 The Theory of Plate Tectonics
11.1.2 The Structure of the Earth
11.1.3 Tectonic Plates
11.1.4 Plate Margins
11.2 Volcanoes
11.2.1 Volcanoes & Their Products
11.2.2 The Development of Volcanoes
11.2.3 Living Near Volcanoes
11.3 Earthquakes
11.3.1 Overview of Earthquakes
11.3.2 Consequences of Earthquakes
11.3.3 Case Study: Christchurch, New Zealand Earthquake
11.4 Tsunamis
11.4.1 Formation of Tsunamis
11.4.2 Case Study: Japan 2010 Tsunami
11.5 Managing the Risk of Volcanoes & Earthquakes
11.5.1 Coping With Earthquakes & Volcanoes
11.5.2 End of Topic Test - Tectonics
12 Climate Change
12.1 The Causes & Consequences of Climate Change
12.1.1 Evidence for Climate Change
12.1.2 Natural Causes of Climate Change
12.1.3 Human Causes of Climate Change
12.1.4 The Greenhouse Effect
12.1.5 Effects of Climate Change on the Environment
12.1.6 Effects of Climate Change on People
12.1.7 Climate Change Predictions
12.1.8 Uncertainty About Future Climate Change
12.1.9 Mitigating Against Climate Change
12.1.10 Adapting to Climate Change
12.1.11 Case Study: Bangladesh
13 Global Population & Inequality
13.1 Global Populations
13.1.1 World Population
13.1.2 Population Structure
13.1.3 Ageing Populations
13.1.4 Youthful Populations
13.1.5 Population Control
13.1.6 Mexico to USA Migration
13.1.7 End of Topic Test - Development & Population
14 Urbanisation
14.1 Urbanisation
14.1.1 Rural Characterisitcs
14.1.2 Urban Characteristics
14.1.3 Urbanisation Growth
14.1.4 The Land Use Model
14.1.5 Rural-Urban Pull Factors
14.1.6 Rural-Urban Push Factors
14.1.7 The Impacts of Migration
14.1.8 Challenges of Urban Areas in Developed Countries
14.1.9 Challenges of Urban Areas in Developing Countries
14.1.10 Urban Sustainability
14.1.11 Case Study: China's Urbanisation
14.1.12 Major UK Cities
14.1.13 Urbanisation in the UK
14.1.14 End of Topic Test- Urbanisation
14.1.15 End of Topic Test - Urban Issues
15 Ecosystems
15.1 The Major Biomes
15.1.1 Distribution of Major Biomes
15.1.2 What Affects the Distribution of Biomes?
15.1.3 Biome Features: Tropical Forests
15.1.4 Biome Features: Temperate Forests
15.1.5 Biome Features: Tundra
15.1.6 Biome Features: Deserts
15.1.7 Biome Features: Tropical Grasslands
15.1.8 Biome Features: Temperate Grasslands
15.2 Case Study: The Amazon Rainforest
15.2.1 Interdependence of Rainforest Ecosystems
15.2.2 Nutrient Cycling in Tropical Rainforests
15.2.3 Deforestation in the Amazon
15.2.4 Impacts of Deforestation in the Amazon
15.2.5 Protecting the Amazon
15.2.6 Adaptations of Plants to Rainforests
15.2.7 Adaptations of Animals to Rainforests
16 Life in an Emerging Country
16.1 Case Studies
16.1.1 Mumbai: Opportunities
16.1.2 Mumbai: Challenges
17 Analysis of Africa
17.1 Africa
17.1.1 Desert Biomes in Africa
17.1.2 The Semi-Desert Biome
17.1.3 The Savanna Biome
17.1.4 Overview of Tropical Rainforests
17.1.5 Colonisation History
17.1.6 Population Distribution in Africa
17.1.7 Economic Resources in Africa
17.1.8 Urbanisation in Africa
17.1.9 Africa's Location
17.1.10 Physical Geography of Africa
17.1.11 Desertification in Africa
17.1.12 Reducing the Risk of Desertification
17.1.13 Case Study: The Sahara Desert - Opportunities
17.1.14 Case Study: The Sahara Desert - Development
18 Analysis of India
18.1 India - Physical Geography
18.1.1 Geographical Location of India
18.1.2 Physical Geography of India
18.1.3 India's Climate
18.1.4 Natural Disasters in India
18.1.5 Case Study: The Thar Desert
18.1.6 Case Study: The Thar Desert - Challenges
18.2 India - Human Geography
18.2.1 Population Distribution in India
18.2.2 Urabinsation in India
18.2.3 The History of India
18.2.4 Economic Resources in India
19 Analysis of the Middle East
19.1 The Middle East
19.1.1 Physical Geography of the Middle East
19.1.2 Human Geography of the Middle East
19.1.3 Climate Zones in the Middle East
19.1.4 Climate Comparison with the UK
19.1.5 Oil & Natural Gas in the Middle East
19.1.6 Water in the Middle East
19.1.7 Population of the Middle East
19.1.8 Development Case Studies: The UAE
19.1.9 Development Case Studies: Yemen
19.1.10 Supporting Development in Yemen
19.1.11 Connection to the UK
19.1.12 Importance of Oil
19.1.13 Oil & Tourism in the UAE
20 Analysis of Bangladesh
20.1 Bangladesh Physical Geography
20.1.1 Location of Bangladesh
20.1.2 Climate of Bangladesh
20.1.3 Rivers in Bangladesh
20.1.4 Flooding in Bangladesh
20.2 Bangladesh Human Geography
20.2.1 Population Structure in Bangladesh
20.2.2 Urbanisation in Bangladesh
20.2.3 Bangladesh's Economy
20.2.4 Energy & Sustainability in Bangladesh
21 Analysis of Russia
21.1 Russia's Physical Geography
21.1.1 Russia's Climate
21.1.2 Russia's Landscape
21.2 Russia's Human Geography
21.2.1 Population of Russia
21.2.2 Russia's Economy
21.2.3 Energy & Sustainability in Russia
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A level Geography earthquake case study- Christchurch 2011 vs Sichuan 2008
Subject: Geography
Age range: 16+
Resource type: Assessment and revision
Last updated
19 July 2020
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Comprehensive 4 page revision resource comparing the May 2008 Sichuan earthquake with the February 2011 Christchurch earthquake. This resource compares:
- The place (including the tectonic setting)
- The epicentre & focus
- Liquefaction & mass movement
- Aftershocks
- Primary impacts
- Secondary impacts
- Existing management
- Short term responses
- Long term responses
- Current situation
- Political implications
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Eduqas A level Geography: Tectonic Hazards
A collection of resources for Eduqas A level Geography Component 3: Tectonic Hazards. Useful to aid both teaching and revision.
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Geography Case Studies
All of our geography case studies in one place
Coastal Erosion
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The Holderness Coast
The Dorset Coast
Happisburgh
Coastal Management
Sandscaping at Bacton, Norfolk
Coastal Realignment Donna Nook
Coastal Realignment Medmerry
Coastal Deposition
Spurn Point
Blakeney Point Spit
Earthquakes
Amatrice Earthquake Case Study
Chile Earthquake 2010
Christchurch Earthquake
Haiti Earthquake
Japan Earthquake 2011
L’Aquila Earthquake
Lombok Indonesia Earthquake 2018
Nepal Earthquake 2015
Sulawesi, Indonesia Earthquake and Tsunami 2018
Taiwan (Hualien) Earthquake 2024
New Zealand 2016
Malaysia Causes of Deforestation
Malaysia Impacts of Deforestation
Alaska Case Study
Epping Forest Case Study
Sahara Desert Case Study
Svalbard Case Study
Thar Desert Case Study
Western Desert Case Study
Energy Resources
Chambamontera Micro-hydro Scheme
Extreme Weather in the UK
Beast from the East Case Study
Storm Ciera Case Study
Food Resources
Almería, Spain: a large-scale agricultural development
The Indus Basin Irrigation System: a large-scale agricultural development
Sustainable food supplies in a LIC – Bangladesh
Sustainable food supplies in a LIC – Makueni, Kenya
Landforms on the River Tees
Landforms on the River Severn
Indus River Basin (CIE)
River Flooding
Jubilee River Flood Management Scheme
Banbury Flood Management Scheme
Boscastle Floods
Kerala Flood 2018
Wainfleet Floods 2019
The Somerset Levels Flood Case Study
UK Floods Case Study November 2019
River Management
The Three Gorges Dam
Mekong River
The Changing Economic World
How can the growth of tourism reduce the development gap? Jamaica Case Study
How can the growth of tourism reduce the development gap? Tunisia Case Study
India Case Study of Development
Nigeria – A NEE
Torr Quarry
Nissan Sunderland
The London Sustainable Industries Park (London SIP)
Tropical Storms
Beast from the East
Hurricane Andrew
Cyclone Eline
Cyclone Idai Case Study
Typhoon Haiyan 2013
Hurricane Irma 2017
Typhoon Jebi 2018
Hurricane Florence 2018
Typhoon Mangkhut 2018
Urban Issues
Birmingham – Edexcel B
Urban Growth in Brazil – Rio de Janeiro
Urban Growth in India – Mumbai
Urban Growth in Nigeria – Lagos
London – A Case Study of a UK City
Inner City Redevelopment – London Docklands
Sustainable Urban Living – Freiburg
Sustainable Urban Living – East Village
Sustainable Urban Transport Bristol Case Study
Bristol – A major UK city
Volcanic Eruptions
Eyjafjallajokull – 2010
Mount Merapi – 2010
Mount Pinatubo – 1991
Sakurajima Case Study
Nyiragongo Case Study
Water Resources
Hitosa, Ethiopia – A local water supply scheme in an LIC
The South-North Water Transfer Project, China
Wakal River Basin Project
Lesotho Large-Scale Water Transfer Scheme
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The earthquake occurred on New Zealand's South Island, 10km west of Christchurch, at 12.51 pm on 22nd February 2011 and lasted just 10 seconds. Measuring 6.3 on the Richter Scale and, at 4.99 km deep, the earthquake was very shallow. The earthquake occurred along a conservative margin between the Pacific Plate and the Australasian Plate.
The earthquake struck New Zealand's South Island, 10km west of Christchurch, at 12:51 pm on 22nd February 2011, lasting just 10 seconds. It measured 6.3 on the Richter Scale and had a shallow depth of 4.99 km.
Haiti Earthquake Case Study What? A 7.0 magnitude earthquake. When? The earthquake occurred on January 12th, 2010, at 16.53 local time (21.53 GMT). Where? The earthquake occurred at 18.457°N, 72.533°W. The epicentre was near the town of Léogâne, Ouest department, approximately 25 kilometres (16 mi) west of Port-au-Prince, Haiti's capital.
The strongest recorded earthquake in recent years in New Zealand was north-east of Christchurch on 14 November 2016, in a small town called Kaikoura which measured 7.8 magnitude, and had a depth ...
Their home has undergone enormous transformation in the past 10 years after a 6.3-magnitude earthquake killed 185 people, disrupted tens of thousands of lives and reduced 80% of the city centre to ...
Case Study Report: 2010 Canterbury and 2011 Christchurch Earthquakes - Demolition and Disaster Waste Management April 2012 Charlotte Brown Mark Milke Executive Summary On 4 September 2010, the Canterbury region of New Zealand was struck by a 7.1 magnitude earthquake. The event caused significant damage but no loss of lives.
It's an earthquake! Ākonga will demonstrate understanding of the spatial distribution of earthquakes across Aotearoa New Zealand or globally. Assessment Activity Version: 2. Geography 1.1. Demonstrate understanding of the spatial distribution of a phenomenon and its impacts on place. 91932 5 Credits. Internal.
The second part is an in-depth case study of the February 2011 earthquake in Christchurch. A devastating event for the city's residents and surrounding landscape, viewers hear firsthand accounts from seismology experts, emergency response leaders, rebuilding and reconstruction co-ordinators, and locals.
The epicentre of the quake was just 2km west of the port town of Lyttelton. It measured 6.3 on the Richter Magnitude scale. Christchurch is New Zealand's second largest city and suffered extensive damage. Killed 185 people. The earthquake was only 5 km deep. The earthquake struck at 12:51 pm on Tuesday, 22 February, 2011.
There were nearly 400 aftershocks in the following week, the largest of which took place 2 hours after the earthquake and had a magnitude of 5.9. Economic effects of the Christchurch earthquake. •$3 billion estimated damage cost. •Rebuilding work will cost insurers an estimated NZ$20-30 billion making it New Zealand's costliest disaster ever.
This study provides a commentary of the Christchurch earthquakes of 2010 and 2011 as a theoretical (as well as empirical) event. Drawing on the ideas of Alain Badiou, it represents the earthquakes and their aftershocks as a rupturing of the established order of things; a distinctive space in which fidelity to the event has the potential to unleash new beginnings and imaginations.
Department of Geography, College of Life and Environmental Science, University. of Exeter, Exeter, UK. Abstract: This study provides a commentary of the Christchurch earthquakes of. 2010 and 2011 ...
Christchurch, New Zealand, earthquakes of 2010-11. The principal event, sometimes referred to as the Darfield earthquake, struck at 4:35 am on September 4, 2010. The earthquake's epicentre was located some 25 miles (40 km) west of Christchurch near the town of Darfield, and the focus was located about 6 miles (10 km) beneath the surface.
A KS3-4 geography case study resource covering the effects of and responses to the Christchurch earthquake, New Zealand. Students colour code the primary and secondary effects and the immediate and long-term responses. There is a case study fact file to complete which summarises this information.
Earthquake Case Study - Christchurch, New Zealand. Two earthquakes hit the city of Christchurch, on New Zealand's south-east coast, in late 2010/early 2011. The second one hit the city centre, killing 185 and destroying much of the CBD. ... Geography Skills. 2 Geology of the UK. 2.1 The UK's Rocks. 2.1.1 The UK's Main Rock Types. 2.1.2 The UK's ...
There were nearly 400 aftershocks in the following week, the largest of which took place 2 hours after the earthquake and had a magnitude of 5.9. •$3 billion estimated damage cost. •Rebuilding work will cost insurers an estimated NZ$20-30 billion making it New Zealand's costliest disaster ever.
AQA Geography Case Study Christchurch Earthquake Learn with flashcards, games, and more — for free.
A powerful magnitude-7.8 earthquake struck New Zealand's South Island, killing at least two people, on November 14th 2016. The earthquake occurred at 00.02 am. 2016 New Zealand Earthquake Map - Source BBC News. It was felt as far afield as the capital Wellington on the North Island, 120 miles (200km) away. A tsunami arrived about two hours ...
-the CBD (central business district) of Christchurch, Canterbury, East New Zealand -in Oceana-on the Pacific Ring of fire -volcanoes to the north but not to the south Click the card to flip 👆 1 / 43
Age range: 16+. Resource type: Assessment and revision. File previews. docx, 46.14 KB. Comprehensive 4 page revision resource comparing the May 2008 Sichuan earthquake with the February 2011 Christchurch earthquake. This resource compares: The place (including the tectonic setting) The event. The epicentre & focus.
Christchurch Earthquake Case Study; Nepal Earthquake 2015; Amatrice Earthquake Case Study; ... Please Support Internet Geography. If you've found the resources on this site useful please consider making a secure donation via PayPal to support the development of the site. The site is self-funded and your support is really appreciated.