EQ1 Tectonics Flashcards
What was Alfred wegeners theory
Continental drift
Evidence for continental drift
- Truncated geological features
- continents fit together
- paleoclomactic indicators
- fossils found across continents
What are convection currents
Hot rocks heated by mantle rise
Cool rocks sink as more dense
Plate boundary types
Conservative - plates move parallel to one another
Constructive - plates more away from eachother and new land forms where hot magma rises
Destructive- ocean and and plates move towards eachother, oceanic plate subducted as is denser
Collision - two land plates move towards eachother
features at each boundary
Desmuctive - volcano, earthquake, fold mountain
Conservative - earthquakes
Collision - gold mountain, earthquakes
Constructive- volcanoes, fold mountains, earthquakes
What is slab pull?
Gravity acting on dense plates being subducted
What is mantle drag
Friction acting on plates as thick viscous mantle moves underheitnand drags at lithosphere
What is ridge push
Driving force for plate motion that occurs mid ocean ridge
Newer plates less dense so rise to form ridges
Elevation causes gravity to pull them away from older plates
Plates slide down into asthenosphere
What is paleomagnetism
Study of ancient magnetism preserved in rocks
Allow former latitudes to be determined by measuring direction of magnetism in iron bearing minerals
How is paleomagnetism applied in plate tectonics
Sea floor spreading at divergent boundaries
Variations in magnetic field show striped pattern across ocean floor
Confirms newest rock along ridge and older rock progressively further away
What is a hotspot
Extra hot region deep in mantle
What is a mantle plume
Heat rising from hotspot through convectional processes
Facilitates rock melting at base of lithosphere, rises to form volcanos
What is subduction?
Destructive boundary Oceanic lithosphere is recycled into mantle
Difference in subduction angle
Shallow angle results in belt of deformation characteristic see by crustal thickening and mountain building
Steep angle characterised by formation of back arc basins
epicentre and hypocentre
hypocentre- the point within the earth that the rupture starts
epicentre- the point at the surface of the earth above the hypocentre
seismic waves
waves that transmit energy released by an earthquake
secondary impact- soil liquefaction
– Christchurch 2010
surface rock loses strength and become like liquid due to violent shaking
causes buildings to tilt, settle or even collapse
short term impact on delivery of aid, LT impact on recovery costs
secondary impact- lateral spreading
when sloping ground slides across liquefied layer
creates large fissures and cracks in ground surface
secondary impact- quake lakes
landslides block rivers and cause flooding
water collects quickly, flooding huge areas
aftershocks collapse natural dams, sending a torrent of water
secondary impact- landslides/ avalanches
2010 Christchurch, 2010 Nepal
occur when magnitude 4<
slopes weaken and fail, made more likely by heavy rain or fractured rock
around 70% of all earthquake deaths caused by landslides
secondary impact- fire
Kobe Japan 1995, Indonesia 2009
caused by fractured gas mains
hard to out out due to fractured water mains
secondary impact- Tsunamis
Japan 2011
Generated by earthquakes under the ocean displace large amounts of water
secondary impact- comms and infrastructure destroyed
San Fransisco, USA
road and rail links, telephone masts and wifi
hampers rescue efforts, causes injury and loss of life
secondary impact- disease
Indonesia 2004
lack of water and sanitation cause cholera and dysentery to spread quickly
dead bodies add to risk when buried