Hazards - Tectonic Hazards (Booklets 2A, 2B) Flashcards
(37 cards)
Earth Structure
- crust
- mantle
- core
continental crust
- 20-200km thick
- light
- older than oceanic (3.8bn)
- rock type: granite
oceanic crust
- thin: 5-10km
- dense
- younger (<200mil)
- rock: basalt
plate motion
theory 1
- magma heated at the centre of earth
- rises towards the crust
- it spreads out when in contact with crust and pulls crust with it - convection currents
plate motion
theory 2
- plates are v heavy so gravity acts = pulls them apart
- lithosphere cools and they become less dense, sink - slab pull
lithosphere
crust + upper-most mantle
plate tectonics evidence
jigsaw fit
- many continents fit together perfectly
- e.g. south america + africa
plate tectonics evidence
fossil evidence
- lystrosaurus (mammal-like dinosaur) fossils found in africa, south america, india
- this dinosaur cant fly or swim
plate tectonics evidence
paleomagnetism
- ships map magnetic orientation of rocks
- new rock is created in centre of ocean, old rock pushed to side
- new rock shows the current magnetic orientation imprinted on it
- patterns can be analysed to show bew rock forming
plate tectonics evidence
climatic
evidence of ice sheets found in tropics - even during coldest periods impossible for ice to form in tropics
plate tectonics evidence
geological
- rocks with exact same characteristics found v faraway from each other
- eg. murica east coast and wales
earthquake + volcano location
- occur in linear clusters
- or plate boundaries
- clustering edge around pacific plate
conservative plate boundary
- two plates slide past each other along a fault
- no volcanoes
- yes earthquakes
- as they move past each other, they stick, so pressure builds up, pressure released in sudden movement = earthquake
- eg san andreas fault in california
destrucive plate margin: subduction
- continental meets oceanic = ocean trench
- convection currents + denser plate + gravity influence = oceanic plate is subducted underneath continental
- oceanic begins to melt due to friction = magma
- magma rises through lithosphere = erupts at surface = volcano chain
- pressure builds up due to plates sticking = rocks fracture = earthquake
destructive plate margin: collision zone
- continental meets continental
- same density = no subduction
- sediments pushed upwards = fold mountains
- himalayas
constructive plate margin
- two plates move apart bc convection currents
- magma rise up to fill gap = may less force volcano
- earthquake
economic impact
effect on the wealth on an area/community
social impact
effect on the lives of ppl
environmental impact
effect on the ecology/landscape of surrounding area
secondary effect
- results of primary effect
- eg. tsunami, wildfire, landslides
primary effect
- caused by ground shaking
- includes deaths, injuries, damaga to infrastructure
immediate response
- reaction of ppl as disaster happens
- immediate aftermath: food, shelter, medical care
long term response
- later reactions that occur weeks/months/years
- eg. rebuilding infrastructure
haiti
- 9mil pop
- 1300USD GDP per capita
- 49% adult literacy rate
- high risk from infectious diseases