Tectonic Hazards Flashcards
What is a destructive plate margin?
When continental and oceanic plates moves towards each other. the denser oceanic plate is subducted under the continental plate forming an ocean trench, and the continental plate folds to form mountains - earthquakes and volcanoes occur here.
What is a constructive plate margin?
When plates move apart magma rises to the surface and cools to form new land, e.g. a mid-ocean ridge, which can cause volcanoes and earthquakes.
What is a conservative plate margin?
When two plates slide past each other, either in opposite directions, or in the same direction but at different speeds. The plates can stick and jolt free causing earthquakes. There is no rising magma so no volcanoes.
What affects hazard risk?
Poverty, urbanisation, farming, climate change.
Poverty
Land is cheaper in risky places
Urbanisation
People may be forced to live on steep slopes or flood plains.
Farming
Farmers choose to live on floodplains or volcano slopes becasue of fertile land.
Climate change
More extreme weather events in the future
Continental drift
Crust broken into plates that move - used to be one ‘super-continent’.
Convection currents
Theory that plates moved due to movement of magma in the mantle.
Ridge push
New crust formed at constructive margins rises to form ocean ridges - older seafloor on either side slides away.
Slab pull
At subduction zones older denser plates sink into the mantle - pulling newer/less dense bits of plate with it.
Layers of the earth
Crust, mantle, core (inner core is solid - outer core is liquid) , lithosphere, asthenosphere.
Continental crust
- 20-200km thick
- less dense
- mainly granite
- up to 3.8 billion years old
Oceanic crust
- 5-10km thick
- very dense
- mainly basalt
- less than 200 million years old
Primary impacts
The direct impacts (caused either by the earth shaking or a volcano erupting) - they happen during or immediately after the event, e.g. loss of life and numbers injured, buildings destroyed, transport infrastructure damaged, water/gas pipes breaking, electricity cables falling down; volcanoes - ash clouds covering everything, lava/ash contaminating water supplies.
secondary impacts
The indirect impacts (caused by the primary impacts) - they happen in the coming hours, day and weeks, e.g. tsunamis and landslides. communities being cut off (from damaged roads), outbreaks of waterborne diseases (from contaminated water), fires and power cuts (from broken cables). BUT, also increase in tourism after volcanic eruptions, e.g. Iceland.
Immediate responses
Emergency aid/assistance given within the first few hours/days - vital to reduce death toll, e.g. search and rescue, medical care such as pain relief and emergency surgery, temporary shelter, providing food and clean water.
Long-term responses
Take place in the weeks and months after - focus on rebuilding and helping people return to normal lives, e.g. restoring essential utilities, repairing/rebuilding domestic and commercial buildings, repairing transport links. Also measures to reduce future damage.
Monitoring
Using scientific equipment to detect warning signs, e.g. measuring changes in temperature and bulges in the volcano dome as magma rises, monitoring seismic activity.
Prediction
Using historical evidence/live data to estimate when a tectonic hazard might happen, e.g. historical records show where earthquakes might occur, particularly is pressure is building up after no recent activity.
Protection
Designing buildings/structures to withstand tectonic hazards, e.g. shock absorbers at the base of tall buildings to make them sway, cross-bracing and automatic window shutters.
Planning
Identifying and avoiding places most at risk and preparing for a disaster, e.g. drawing up hazard maps, setting up ‘no-go’ areas, practising earthquake drills, stocking up on food, water and fuel, and knowing where to evacuate to.
Why live in tectonic areas ?
- geothermal energy
- mining
- farming
- tourism
Composite volcanoes
Found in destructive plate margins. Acidic lava. Steep sides
Shield volcanoes
Found in constructive plate margins. Non-acidic lava. Gentle sides.