Hazards - Tectonic Hazards (Booklets 2A, 2B) Flashcards
1
Q
Earth Structure
A
- crust
- mantle
- core
2
Q
continental crust
A
- 20-200km thick
- light
- older than oceanic (3.8bn)
- rock type: granite
3
Q
oceanic crust
A
- thin: 5-10km
- dense
- younger (<200mil)
- rock: basalt
4
Q
plate motion
theory 1
A
- 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
5
Q
plate motion
theory 2
A
- plates are v heavy so gravity acts = pulls them apart
- lithosphere cools and they become less dense, sink - slab pull
6
Q
lithosphere
A
crust + upper-most mantle
7
Q
plate tectonics evidence
jigsaw fit
A
- many continents fit together perfectly
- e.g. south america + africa
8
Q
plate tectonics evidence
fossil evidence
A
- lystrosaurus (mammal-like dinosaur) fossils found in africa, south america, india
- this dinosaur cant fly or swim
9
Q
plate tectonics evidence
paleomagnetism
A
- 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
10
Q
plate tectonics evidence
climatic
A
evidence of ice sheets found in tropics - even during coldest periods impossible for ice to form in tropics
11
Q
plate tectonics evidence
geological
A
- rocks with exact same characteristics found v faraway from each other
- eg. murica east coast and wales
12
Q
earthquake + volcano location
A
- occur in linear clusters
- or plate boundaries
- clustering edge around pacific plate
13
Q
conservative plate boundary
A
- 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
14
Q
destrucive plate margin: subduction
A
- 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
15
Q
destructive plate margin: collision zone
A
- continental meets continental
- same density = no subduction
- sediments pushed upwards = fold mountains
- himalayas