Volcanoes occur at destructive and constructive plate margins
Earthquakes are caused by tension at all 3 plate margins
Moment magnitude scale
Measures the amount of energy released by an earthquake
A magnitude 7 earthquake is 10 times more powerful than a magnitude 6
How earthquakes occur
1. Plates jerk past each other, causing shockwaves
2. Shockwaves spread out from the focus
3. Stronger shockwaves from shallow focus
Effects of tectonic hazards
Primary effects
Secondary effects
People live in hazard-prone areas due to family/employment ties, confidence in government support, belief that severe events won't happen in their lifetime, fertile volcanic soil, tourism opportunities, geothermal energy
Monitoring tectonic hazards
1. Seismometers and lasers to detect earth movements
2. Remote sensing to detect heat and shape changes
3. Monitoring for precursor signs like earthquakes, gas release, bulging
Predicting tectonic hazards
1. Earthquakes difficult to predict, but locations known
2. Volcanic eruptions can be predicted from monitoring
Planning for tectonic hazards
1. Land zoning to avoid high risk areas
2. Emergency services training
3. Public education
4. Evacuation planning
5. Emergency supplies stockpiling
Protecting against tectonic hazards
1. Earthquake-resistant building design
2. Strengthening existing structures
3. Automatic shut-off for utilities
Haiti
Lower middle-income country in the Caribbean
7.2 earthquake struck Haiti
14th August 2021
Plate boundaries around Haiti
North American Plate lies to the north and the Caribbean Plate to the south
Earthquake took place at a conservative plate boundary, where the Caribbean plate moved eastwards
Haiti Earthquake
Focus was only 10 km deep
Epicentre was 125 km from the capital Port-au-Prince
The estimated cost of damages from the Haiti earthquake is around US$1.6 billion. This amounts to 9.6 per cent of Haiti's GDP.
Christchurch 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
Occurred along a conservative margin between the Pacific Plate and the Australasian Plate
Christ Church 2011 earthquake
Population of 376,700
Time and Date of Christ Church 2011 earthquake
22nd February 2011 – 12-51pm
Christ Church 2011 earthquake
Magnitude of 7.1
GDP per capita $27,700
Adult literacy rate 99% over 15 years can read/write
100% people have access to clean water
Liquefaction in Christ Church 2011 earthquake
1. Ground shaken, everything from buildings to roads to cars and trees sunk into the ground
2. Sand boils most common type of liquefaction
Impacts of Christ Church 2011 earthquake
181 people were killed, 80 of which from Christchurch TV building collapsed
2,000 people were injured
1 in 5 people lost their jobs because many buildings were destroyed
6,000 companies and institutions with over 50,000 employees in the CBD of 45% of them are likely to retain their jobs in another location
$40billion worth of damage need to repair infrastructure
Haiti 2010 earthquake
Population of 9.7 million
GDP per capita $343.89
HDI 0.456
More than half of Haiti's population – between 5 and 6 million people – live in rural areas
About 85% of the rural population practise some agriculture which accounts for about 26% of Haiti's economic output and makes agriculture
Impacts of Haiti 2010 earthquake
3,500,000 people were affected by the quake
220,000 people estimated to have died
300,000+ people were injured
Over 188,383 houses were badly damaged and 105,000 were destroyed by the earthquake (293,383 in total)
1.5m people became homeless
4,000 schools were damaged or destroyed
25% of civil servants in Port au Prince died
Over 600,000 people left their home area in Port-au-Prince and mostly stayed with host families