Plate Tectonics Flashcards

(104 cards)

1
Q

What is a Geoid and how is it formed?

A

Bulging at equator due to centrifugal forces (kids on a roundabout)

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2
Q

What is the oceanic crust?

A

5-10km, occasionally broken layer of basalt known as ‘Sima’ – Silica and Magnesium

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3
Q

What is the continental crust?

A

up to 70km, mostly granite known as ‘Sial’ – Silica and Aluminium

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4
Q

Difference between ‘Sial’ and ‘Sima’

A

‘Sial’ (Conti) is less dense and thicker, found above ‘Sima’ (Ocean)

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5
Q

What is the Lithosphere?

A

Tectonic plates are formed here

upper-mantle + crust (100km)

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6
Q

What is the Mantle?

A

(2900km) – great heat and pressure results in liquid dense the deeper you go

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7
Q

Core Characteristics

A

Core (5000’C) is 4 times denser than crust

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8
Q

Outer Core characteristics

A

Outer Core – semi-liquid=Iron

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9
Q

Inner Core Characteristics

A

Inner Core=Iron + Nickel

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10
Q

Convection currents are causes by..?

A

The heat generated by the core creates convection current

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11
Q

Who and when - Theory of Continental Drift

A

Alfred Wegner – 1912

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12
Q

6 Things the theory of continental dift is based on:

A

1) Jigsaw fit of SA and A
2) Matching rock in East Cnd to NW Sco
3) Coal beneath Antarctica
4) Fossils in India matched in Aus
5) Unique Mesosaurus in A + Bra
6) Glacial deposits in Bra match west A

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13
Q

Scientific Community reaction to Theory of Continental Drift

A

Evidence but no explanation dismissed his theories

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14
Q

Theory - 1950’s?

A

50s – nuclear submarines – Oceanic Floor Mapping

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15
Q

1962?

A

Sea floor spreading – youngest rock in the middle of Atlantic, newest in Iceland

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16
Q

Palaomagnitism?

A

During Polarity every 400,000 years, there were eruptions of magnetite, Symmetrical patterns either side of the Atlantic ridge – confirming sea floor spreading

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17
Q

Explain Convection Currents

A

Plates are driven by convection currents which rise and spread in the asthenosphere before cooling and sinking back down

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18
Q

Oceanic Crust Contructive Formations

A

Mid-Ocean Ridge
Faults cut across separating sections of the ridge widening at different rates, creating shallow focus earthquakes
Rift valleys in the middle of ridges
Submarine volcanoes can eventually create volcanic islands

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19
Q

Continental Crust Contructive Formations

A

Rift Valleys

Lithosphere splits – fractures in parallel faults

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20
Q

Oceanic > Continental Destructive Formations

A

Denser Oceanic Plate subducts beneath Continental = deep ocean trench
Continental land is uplifted, compressed and folded > chains of fold mountains
Oceanic land is destroyed/melted between 100-700 km (Benioff Zone) due to heat and friction which may also cause deep-focus earthquakes
Turned into magma, oceanic rock is less dense than asthenosphere =rising in faults where the continental plate has buckled, before reaching the surface to form explosive volcanic eruptions

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21
Q

Oceanic > Oceanic Destructive Formations

A

The faster/ denser plate subducts > deep ocean trench

Rising magma melted in the Benioff zone > volcanic island arcs

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22
Q

Continental > Continental Destructive Formations

A

Subduction does not occur because continental is not dense enough > High Fold Mountains
Shallow focus earth-quakes can be triggered

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23
Q

Conservative Formations

A

Crust is not destroyed and no subduction > no volcanic activity + no formation of new crust
Extremely active
Shallow Focus Earthquakes when sticking occurs and stress builds

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24
Q

Contructive Crust and Volcanoes

A

Oceanic crust is formed by basaltic magma rising from the asthenosphere
Basic submarine volcanoes
Volcanic islands

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25
Destructive Volcanoes
Explosive acid volcanoes where there is subduction
26
Conservative Volcanoes
No subduction > no Volcanicity
27
Hot Spots
When radioactive decay at the core is concentrated, it can create localise thermal currents where plumes of magma rise vertically The hotspot remains stationary, whilst the plate moves resulting in chain islands
28
Dykes
When magma solidifies in a vertical fissure | Once solidified into igneous rock, it is usually more resistant to erosion, leaving a prominent wall-like feature
29
Sills
Forms when magma solidifies into horizontal/inclined layers of existing rock
30
Laccolith
Form where viscous magma forcing into overlying rock strata to arch into a dome
31
Batholith
Larger scale where often, the other features will feed off of them Extreme heat/ pressure (metamorphism)= metamorphic aureole
32
Extrusive Features
Gaseous emissions – steam, carbon monoxide, hydrogen sulphide, sulphur dioxide and chlorine Solids – ash, dust, glassy cinders Liquids – lava bombs (tephra/pyroclasts), solidify mid-air
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Basic Lava
(basaltic) is low in silica, allowing gas bubbles to move freely – fluid and free-flowing
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Acid Lavas
rich in silica – viscous > gas bubbles cannot expand - build up of pressure = violent eruptions
35
Basic Shield Volcanoes
Mid-ocean ridge, rift valleys and hotspots – direct access to surface Repeated eruptions Runny lava forms gentle sloping volcanic cones and shields
36
Acid Dome Volcanoes
Destructive margins Viscous lava cannot flow far before cooling = steep convex cones Rhyolitic lava is thick and unable to flow Explosive pyroclastic flows of superheated gases, ash and pumice
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Dormant Volcano
Hasn't erupted within historic times
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Extinct Volcano
10,000 years dormant
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Composite cones
Alternating eruptions of ash, tephra (incl. lapilli), lava building volcano in layers Often covered by secondary (parasitic) cones and fissures
40
Ash and Cinder Cones
Ash, cinder and tephra erupted in the central crater | Steep-sided concave in shape
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Calderas
Emptying of the magma chamber allows flanks to cave in creating a vast pit which can be flooded as a sea or lake
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Icelandic Volcano
Basaltic | Gentle flow from fissures
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Hawaiian
Basaltic | Gentle flow from central vent
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Strombolian
Frequent explosive eruptions of tephra and steam
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Vulcanian
Thicker basaltic + Andesitic + Rhyolitic | Less frequent, more violent eruption of gas, ash and tephra
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Vesuvian
Thicker basaltic + Andesitic + Rhyolitic Long periods of inactivity Very violent gas explosion
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Peléan
Andesitic + rhyolitic | Very Violent eruption of nuées ardentes
48
plinian
Rhyolitic Exeptionally violent eruptions of gases, ash and pumice Create rainstorms and lahars
49
Minor extrusive activity
Geysers Fumaroles Hot Springs Boiling Mud
50
Geysers
Boil from contact with hot rocks Hot volcanic gases build up pressure until an explosion of water takes place The vent re-fills and it’s all repeated Short-lived features
51
Fumaroles
Low pressure outlets of steam and gas | Solfatara when the gas is sulphurous – leaves yellow deposits
52
Hot Springs + Boiling Mud
Not under pressure Not all volcanic Heated deep below the surface Dissolved minerals create boiling mud
53
Surtsey
In 1963  Powerful underwater eruptions led to the birth of a new island off the coast of Iceland As lava erupted onto the seafloor it solidified, eventually formed an island that emerged out of the water
54
Great African Rift Valley
Constructive plate boundary on two continental plates Magma plume below Extends 5000 Km Shield volcanoes form
55
Hawaii Hotspot
Shows the movement of the plates since the plume of radioactive decay from the core stays in the same place, so volcanic islands form in the direction of the movement of the plate The largest island is called Big island and is where there is an active volcano Then further west smaller islands are areas where the basalt lava rock is older, therefore showing how they used to be above the plume They get smaller because they are older ad are eroded To the east of big island is Liohi, an underwater volcano which will eventually form the new island
56
San Andreas
Shallow focus quakes occur like San Fran 1906,1989 and LA 1994 Where the Pacific and North American late are moving parallel to each other The same direction but the pacific plate is moving about 3 times faster at 5-9 cm a year Stresses build up creating transform faults
57
Himalays
Continental/Continental Tallest mountain range on earth where the Indian Plate is colliding into the Eurasian Plate Everest grows 4mm a year, predictions of up to 8 cm shift upwards since the April Nepalese Earthquake 2015
58
Monserrat
Caribbean plate slips under the South American | Dramatic heat at Benioff zone creates the chain of volcanic islands known as the Lesser Antilles
59
Andes
Subduction of oceanic Nazca plate below continental South American Plate The rise of the Andes is down to compression from the Nazca Plate and the Antarctic Plate creating fold mountains The Peru- Chile Trench is a depression where the Nazca plate is subducting
60
Nyiragongo general
African rift valley, main crater is 250m deep, containing a lava lake Frequent! Along with its neighbouring volcano, it is responsible for 40% of Africa's recorded eruptions Lava flows, can me as fast as 90km/h 13km fissure was opened up, flowing to Goma and lake Kivu Stratovolcano 20km from Goma (1,000,000) , just west of Rwanda $480 GDP Per Capita Home to The Great African War from 98 to 03 Stratovolcano
61
Nyiragongo Primary Effects
Lava flows destroyed over 1/3 of Goma; Water, power and medical facilities destroyed including 3 health centres and 1 hospital Part of the airport was covered 147 Died Sulphurous lava contaminated Lake Kivu Medical attention for those effected by smoke and fumes 14 villages destroyed completely
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Nyiragongo 2002 secondary effects
Accompanying earthquakes caused structural damage to buildings Medical attention for diseases spread by contaminated water Looting homes and a petrol station exploded during looting 220,000 fled to Rwanda to escape lave, making aid difficult 500,000 homeless
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Nyiragongo 2002 immediate responses
UN supplied enough food to feed 700,000 for a week | Full evacuation of Goma
64
Nyiragongo 2002 longer-term responses
Volcanologists monitor Lake Kivu after fears lava, would release large amounts of carbon dioxide and methane
65
Eyjaffajokull 2010 general
The caldera is 2.5km wide Constructive plate – North American plate moving west and the Eurasian moving east 11Km ash plume – fine grained ash 150m Ice cap $47,000 GDP Per Capita Sparsely-population, very volcanic, and cold Strombolian
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Eyjaffajokull 2010 Primary effects
Agricultural land damaged, farms hit by ash fall Roads destroyed No deaths or injuries A small number of people had respiratory and irritation issues
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Eyjaffajokull 2010 secondary effect
10 million airline passenger stranded abroad with over 100,000 flights cancelled over 8 days Ash contaminated local water supplies, impacting livestock Kenya lost $3.5 million as loss in exports Train industry boosted Cost $2.6Bn to Europe Flooding from glacier melt Flooding up to a year later due the silting up of rivers
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Eyjaffajokull 2010 immediate response
People asked to stay indoors because of ash in the air 700 evacuated from flooding Entirely domestic responses
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Eyjaffajokull 2010 long term response
Far more tests on what planes can cope with in terms of ash, very little was known about this at the time
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Primary effect of earthquakes
``` Ground shaking education damage death + injury lahars/avalanches liquefaction power station damge panic fear and hunger ```
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Secondary and long-term effects of Ground shaking
Fire due to broken Gas pipes/power lines Emergency services hindered Contaminated water = disease
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Secondary and long-term effects of Education damage
Education suspended | Lost generation + poor economic development locally
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Secondary and long-term effects of Immediate death and injury
Un-buried bodies lead to more disease Disability trauma Long-term illness
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Secondary and long-term effects of Lahars/ Avalanches
Death and injury Flooding Loss of farmland and prouction Disruption to natural drainage basin
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Secondary and long-term effects of Liquefaction
Foundations subside = death and injury | Repairs are difficult and expensive
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Secondary and long-term effects of Power station damage
Power cuts hinder emergency services | Reconstruction is very expensive
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Secondary and long-term effects of panic fear and hunger
disorder and looting | Restoration of trust in neighbours
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Explain seismicity
Friction builds up stress in the lithosphere Once overcome they fracture along cracks called faults The breaking point is the focus (hypocentre) Epicentre = point of surface above the focus
79
What are the seismic shock waves?
Primary/Pressure waves are the fastest – high frequency-Push-travel through mantle and core Secondary/Shear waves are half as fast – high frequency- shake – travel through mantle but not core Surface Love waves – slowest – most damage – side to side Rayleigh waves – radiate in complicated low frequency rolling up and down motion
80
Two ways of measuring earthquakes
Richter scale = magnitude – logarithmic | Mercalli Scale = intensity of damage – observations
81
How can you predict an earthquake
``` Micro quakes Bulging ground Electrical and magnetic changes within rocks Increased argon in soil Animal behaviour ```
82
What are the characteristics of a Tsunami
Wave height is less than 1m but can be up to 25m at shore Wavelength 100-1000km 650-1000kmh Series of waves, first not always the biggest Time between each wave = 10-60 minutes On approaching the coast, the front will slow down allowing the rear to pile up
83
Nepal April 2015 General
7.8 magnitude and 15km deep – shallow 265 aftershocks a month on, 7.3 magnitude in May, caused further devastation Maximum of Severe on the Mercalli scale Landlocked, extremely mountainous country One of the poorest countries in the world with under $700 GDP per capita Caused by a sudden thrust along the major fault line where the Indian Plate, is sub ducting underneath the Eurasian Plate
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Nepal April 2015 Primary effects
``` 9000 dead, 20,000 injured Thousands of houses destroyed Airport closed for a day Death in churches due to the time of impact and old buildings 700,000 houses destroyed 5000 schools destroyed, 16,000 damaged ```
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Nepal April 2015 Secondary Effects
Avalanche on Everest – killing 19 – bad for tourist industry Hundreds of thousands homeless Landslides and aftershock – 200 dead from may aftershock Trauma, many aftershock Survivors preyed upon by human traffickers involved in brothels Sleeping in the streets cold, too scared to go back inside Displacement of people
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Nepal April 2015 Immediate Responses
90% of Nepalese army sent the worst areas Rainfall, after shock and small airport run-way slowed things down, aid had to be over landed on poor roads from India Social Media, Drone footage and satellite imaging were used $350 million donated from the international community
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Nepal April 2015 Longer-term responses
Calls for more aid – estimated just 10% of relief came from overseas Re-building of building sensibly Calls to build wider run-ways
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New Zealand Feb 2011 General
Very shallow- 5 km, 6.3 magnitude, 6 miles from Christchurch Occurred on a conservative plate margin where the Pacific Plate slid past the Australian Plate in the opposite direction. It was the aftershock from a larger earthquake in 2010 but the impacts were more severe $42,000 GDP per capita
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New Zealand Feb 2011 Primary Effects
181 killed, 2000, injured Hundreds of kilometres of water and sewage piper were damaged Over half of the city buildings were damaged Moderate amount of liquefaction An iceberg of 20 football fields broke off 80% without electricity
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New Zealand Feb 2011 Secondary Effects
Businesses put out of action causing losses of income and jobs Schools sharing classrooms due to damage elsewhere Difficult to get around due to transport destroyed Trauma, due to aftershocks, injury and death Tourism loss because they couldn’t host rugby world cup matches
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New Zealand Feb 2011 Immediate Responses
Chemical toiles provided for 30,000 International aid of around $7 million and aid workers 300 Australian police arrived Earthquake commission assessed all buildings to ensure they were safe
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New Zealand Feb 2011 Long term responses
Red Cross provide grants to families with children under 5 years Water and sewage all restored fully by august Roads and housed cleared of silt from liquefaction, 80% clear by August
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How do japan earthquake proof buildings
Rolling weights on roof to counter-act shock waves Panels of marble and glass flexibly anchored to steel structure Bird cage like interlocking steel frame Reinforced latticework foundations deep in bedrock Rubber shock absorbers
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How does japan prepare for earthquakes
Earthquake proof buildings Education – everyone knows what to do – practice drills Every one has an emergency survival kit You cant buy a phone without overriding warning software Warnings seconds before impact are simultaneously across all media Large network of seismometers Prediction- micro quakes, bulging, electrical and magnetic changes with rocks, in creased argon gas content in soil and curious animal behaviours 10m sea wall to prevent the effect of a Tsunami
95
Indian Ocean Tsunami 2004 Secondary Effects
500,000 into refugee camps in just one region of Indonesia Economies like fishing, agriculture and tourism ruined 44% of one region of Indonesia lost their livelihoods £226m damage to the Thai fishing industry Water supplies contaminated Inequality increases
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Indian Ocean Tsunami 2004 Immediate Responses
Relief efforts with more than 160 aid agencies | Foreign military troops
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Indian Ocean Tsunami 2004 General
Second biggest earthquake in history – 9.3 240Km of the coast of Sumatra Cause – the release of stress along a 1000km thrust fault Indian plate moved downwards by 15m, forcing the ocean floor above the thrust fault 8 aftershocks followed Warning were slow - with nothing on the media in Thailand until an hour after the first wave
98
Indian Ocean Tsunami 2004 Primary Effects
290,000 died, thousands missing Vegetation + top soil removed up to 800m in land Infrastructure destroyed Coastal settlements devastated
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Indian Ocean Tsunami 2004 Longer-term responses
Reconstruction- still thousands in tents a year on Aid was delayed by rebel group Tamil tigers in Sri Lanka Underclasses ignored by the government A UN group set up a warning system but it relies on the countries own alerts – tourist areas with sirens, rural communities with radio warning More education on awareness with drills and plans Areas at more risk were mapped
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Japan March 2011 Tsunami General
9.0 – 10m waves 100km from Sendai 500 km segment of the North American Plate dragged down my sub ducting pacific plate, moving upwards 10m 10 waves 1km apart
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Japan March 2011 Tsunami Primary Effects
Weaker buildings collapsed Flooded 500 square metres 25,000 dead or missing
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Japan March 2011 Tsunami Secondary Effects
500,000 homeless Some homes without water or electricity, petrol had to rationed 700 aftershock traumatised people Explosions and leaks at Fukushima nuclear plant panicked the whole world, with stock markets plummeting
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Japan March 2011 Tsunami Immediate Responses
``` Helicopter rescues on roofs 100,000 soldiers Many countries offered aid Fukushima exclusion zone No reports of looting ```
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Japan March 2011 Tsunami Long Term Responses
Level of sea defence increased Government borrowing even more increased, resulting in austerity and tensions Trauma, illness and disablement