plate techtonics and Christchurch Flashcards
Risk
Is the probability of a hazard happening and creating a loss of lives
Vulnerability
describes the risk of exposure to hazards combined with an inability to cope with them
Resilience
the degree to which the environment can absorb a hazardous even
3 ways to increase capacity to cope
- having emergency evacuation
- using earthquake proof buildings
- land use planning
2 Social impacts of the Christchurch earthquake
- 184 people were killed and over 1500 injured in 2011 quake
- 4 months after the earthquake around 50,000 Christchurch residents had moved permanently to other parts of NZ or Australia. (worse sense of community)
(however in the long term there was a net increase in population do to employment opportunities in recovery)
2 economic impacts of the Christchurch earthquake
- Some potential tourists may not travel to Christchurch now as the rugby World Cup could no longer be hosted (no multiplier effect)
- Total loss to the NZ economy was estimated as £16 billion, which is about 13% of GDP
2 Responses to the Christchurch earthquake
- Christchurch used land use planning with
The Green Zone – about 100,000 houses located here and these are likely to be rebuilt. However they are ‘rebuilt better’ – to reduce the impact of liquefaction the foundations are strengthened and piles can be driven 25m down to reach solid ground.
· Red zone – the worst affected residential areas – many along the valley slopes of the River Avon close to the inner city. Land in this area suffered badly from Liquefaction. The government agreed to buy over 5000 of the worst affected properties or the land on which they were built.
- In the first few months much of the CBD of Christchurch was converted into a complex of shipping container boxes, each replacing services like shops, banks and fast food outlets
focus
where the pressure from underground is released
epicenter
the point on the ground directly above the focus
Constructive plates
they move apart
destructive plates
two plates move towards each other resulting in the denser of the two plates to subduct causing friction
——–>
Conservative plates
Plates move in the same direction at different speeds. Friction the to get stuck. As pressure builds over time its can rebound and cause an earthquake.
- ————————->
- —————>
how does sea floor spreading occur
ocean ridges
Seafloor spreading occurs at divergent plate boundaries.
1. As tectonic plates slowly move away from each other, heat from the mantle’s convection currents makes the crust more plastic and less dense.
- The less-dense material rises, often forming a mountain or elevated area of the seafloor.
- Eventually, the crust cracks. Hot magma fueled by mantle convection bubbles up to fill these fractures and spills onto the crust. This bubbled-up magma is cooled by frigid seawater to form igneous rock. This rock (basalt) becomes a new part of Earth’s crust.
how do volcanos occur at subduction zones
- oceanic crust is melted when submerged into the magma
- as it is light and dense it rises up back into the continental crust
- these volcanoes are much more upright as the lava is andesitic which is more viscous and more explosive
example of composite volcanoes
mt Șt helens in North America
steep sided