EQ1 Tectonics Flashcards

1
Q

What was Alfred wegeners theory

A

Continental drift

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2
Q

Evidence for continental drift

A
  • Truncated geological features
  • continents fit together
  • paleoclomactic indicators
  • fossils found across continents
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3
Q

What are convection currents

A

Hot rocks heated by mantle rise
Cool rocks sink as more dense

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4
Q

Plate boundary types

A

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

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5
Q

features at each boundary

A

Desmuctive - volcano, earthquake, fold mountain
Conservative - earthquakes
Collision - gold mountain, earthquakes
Constructive- volcanoes, fold mountains, earthquakes

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6
Q

What is slab pull?

A

Gravity acting on dense plates being subducted

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7
Q

What is mantle drag

A

Friction acting on plates as thick viscous mantle moves underheitnand drags at lithosphere

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8
Q

What is ridge push

A

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

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9
Q

What is paleomagnetism

A

Study of ancient magnetism preserved in rocks
Allow former latitudes to be determined by measuring direction of magnetism in iron bearing minerals

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10
Q

How is paleomagnetism applied in plate tectonics

A

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

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11
Q

What is a hotspot

A

Extra hot region deep in mantle

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12
Q

What is a mantle plume

A

Heat rising from hotspot through convectional processes
Facilitates rock melting at base of lithosphere, rises to form volcanos

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13
Q

What is subduction?

A

Destructive boundary Oceanic lithosphere is recycled into mantle

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14
Q

Difference in subduction angle

A

Shallow angle results in belt of deformation characteristic see by crustal thickening and mountain building

Steep angle characterised by formation of back arc basins

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15
Q

epicentre and hypocentre

A

hypocentre- the point within the earth that the rupture starts
epicentre- the point at the surface of the earth above the hypocentre

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16
Q

seismic waves

A

waves that transmit energy released by an earthquake

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17
Q

secondary impact- soil liquefaction

A

– 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

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18
Q

secondary impact- lateral spreading

A

when sloping ground slides across liquefied layer
creates large fissures and cracks in ground surface

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19
Q

secondary impact- quake lakes

A

landslides block rivers and cause flooding
water collects quickly, flooding huge areas
aftershocks collapse natural dams, sending a torrent of water

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20
Q

secondary impact- landslides/ avalanches

A

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

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21
Q

secondary impact- fire

A

Kobe Japan 1995, Indonesia 2009
caused by fractured gas mains
hard to out out due to fractured water mains

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22
Q

secondary impact- Tsunamis

A

Japan 2011
Generated by earthquakes under the ocean displace large amounts of water

23
Q

secondary impact- comms and infrastructure destroyed

A

San Fransisco, USA
road and rail links, telephone masts and wifi
hampers rescue efforts, causes injury and loss of life

24
Q

secondary impact- disease

A

Indonesia 2004
lack of water and sanitation cause cholera and dysentery to spread quickly
dead bodies add to risk when buried

25
why do intra-plate earthquakes occur
- reactivation of old fault lines - subsidence from mining or fracking - pressure on surface rocks from water in reservoirs - large manmade explosions - large avalanches and landslides
26
what is a megathrust earthquake
after frictional stress has built from plates locked together for some time and failure occurs
27
what is the benioff zone
where plates converge and one is subducted different speeds of rock create numerous deep-focused earthquakes determines position and depth of hypocentre
28
where to seismic waves originate
Benioff zone
29
3 ways to measure an earthquake
- Richer scale- vibrations plotted on a seismometer, numbered 0-10 - Moment magnitude scale- moment is product of distance moved and force required to move it - Mercalli scale- measures damage, based on visual or experienced effects. ranges from unnoticeable shaking to catastrophic damage
30
Characteristics of P waves
First wave to arrive at seismic recording stations Compresses and expands land (moves backwards and forwards) in the direction of travel
31
Characteristics of S waves
Travel through solids Secondary because Second to arrive at seismic recording stations Shake the ground side to side perpendicular to the direction of wave travel
32
Characteristic of Rayleigh waves
Surface waves Travel in rolling motion like ocean waves Can travel through solids Slow moving
33
Characteristic of a love wave
Surface waves Travel through solids - not liquids Horizontal motion that moves surface from side to side perpendicularto direction wave is travelling
34
What conditions are needed for formation of a volcano
Partially molten rock, magma below surface of the earth. Rises through natural cracks in crust, or gets safer underground while pressure rises until it erupts explosively
35
What is tephra
Solid material, ranging from volcanic bombs to ash particles ejected into the atmosphere
36
What are pyroclastics
Very hot gas charged material, includes gas and tephra
37
Name some volcanic gases
Carbon dioxide, carbon monoxide, hydrogen sulphide, sulphur dioxide, chlorine
38
Name primary effects / processes of a volcanic eruption
Tephra, pyroclastic flows, lava, volcanic gases
39
Name secondary effects in a volcanic eruption
Lahars, flooding, tsunamis, volcanic landslides, Short term climate change, jokulhlaup
40
What are lahars
Volcanic mud flows
41
Why do volcanos cause flooding
Melting of icecaps and glaciers
42
What is a jokulhlaup
Glacial melting outburst floods
43
How to volcanos form tsunamis
Caldera forming events (eg Krakatoa) generate giant waves
44
How to volcanos cause short term climate change
Inject vast amounts of debris into the atmosphere which reduced global temperatures
45
Difference between dormant, active and extinct
Active = still erupts Dormant= not currently erupting but supposed to erupt again Extinct = won’t erupt again
46
What are the 3 landform characteristics of volcanos
Shield= wide and gentle slopes, runny lava Stratovolcano= steep sloping side built up over millions of years with compositions, typically more violent Calderas =large couldron hollow forming after magma chamber empties in volcanic eruption, ground collapses leaving a depression at the surface
47
What types of eruption are there
Explosive- gas driven eruptions nwhich propel magma and tephra Effusive- outpouring of lava without significant explosive eruption
48
What are the three groups of lava
Basaltic Andesitic Rhyolitic
49
How does silica connect affect lava and eruptions
More silica means more gases! More violent, more viscous lava
50
Features of basalt lava
Fluid Low silica content Basic Hottest lava Produces shield volcanos- wide with low slopes Located at divergent margins and hotspots Effusive
51
Andesite lava
Viscous Medium silica content Medium heat Produces steep sided cones Convergent margins Violent and explosive
52
Rhyolitic lava
Viscous Hugh silica content Lowest heat around 900°C Produces steep sided cones Convergent margins Explosive
53
How many people have died due to eruptions in the last 300 years
250000