Tectonics EQ1 Flashcards

1
Q

What are the layers of the earth?

A

Core
Mantle
Asthenosphere
Lithosphere

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2
Q

Describe the core

A

Central part of the earth
Made up of inner and outer core
Inner core is solid, outer core is liquid
Inner and outer core made from iron and nickel
Core is a source of radioactive heat

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3
Q

Describe the mantle

A

Semi-molten body of rock between the earths crust and its core

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4
Q

Describe the asthenosphere

A

Part of the mantle
Semi-molten
Below the lithosphere

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5
Q

Describe the lithosphere

A

The crust and upper mantle which form the tectonic plates
80-90km thick
Crust changes in thickness under oceans and continents: 6-10km thick under oceans, 30-40km under continents

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6
Q

What is a convergent plate margin

A

When two plates move towards each other

Oceanic plate slides beneath the continental plate

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7
Q

Describe what happens at a convergent margin

A

Crust is destroyed at oceanic plate subducts under continental at subduction zone
Rock catches against each other
Pressure between plates builds until plates can’t take stress
Plates slip past each, which can cause plates to move resulting in ground shaking

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8
Q

What is a conservative plate margin

A

When two plates slide past each other horizontally

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9
Q

Describe what happens at a conservative plate margin

A

Crust is neither produced nor destroyed
Plates catch and snag against each other
Friction and pressure builds until plates can’t take stress
Plates slip past each other which can cause both plates to move = ground shaking

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10
Q

What is a divergent plate margin

A

When two plates move away from each other

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11
Q

Describe what happens at a divergent plate margin

A

Convection currents diverge and cause a gap between plates
Magma rises up to fill the gap
New crust is generated as plates pull away from each other

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12
Q

What features does an oceanic plate have

A

High-density materials
Made of basaltic rock
Only 7-10km thick
Subduct under other plates

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13
Q

What features does a continental plate have

A

Thicker than oceanic (25-75km)
Less dense than oceanic
Made of granitic rock
Do not subduct

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14
Q

Define a hazard

A

A hazard is a natural/geophysical event that has the potential to threaten both life and infrastructure

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15
Q

How are hazards distributed

A

Unevenly

Some areas are at high risk and some are at low risk

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16
Q

Where do tectonic hazards (volcanoes, earthquakes, tsunamis) occur

A

At specific points that are usually associated with tectonic plate margins
Earthquakes also occur where the Indo-Australian plate collides with the Eurasian plate

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17
Q

Describe a hotspot

A

Where there is a hot mass of rising heat under a weakness in a plate
Magma rises to the surface through this weakness
Hawaiian islands formed as a result of a mid-Pacific hotspot

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18
Q

Describe intra-plate volcanoes

A

Mantle plumes rise towards the surface generating basaltic volcanoes
The plume remains stationary, although plate above moves over it
Continuing plate movement over time produces a chain of volcanic islands

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19
Q

Describe intra-plate earthquakes

A

Earthquakes can happen in mid-plate settings, usually associated ancient fault lines being re-activated by tectonic stresses
Zones of weaknesses are created as plates move and stress increases

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20
Q

Define gravitational sliding

A

Elevated altitudes of oceanic crust at ridges at divergent plate boundaries
Create a slope down which oceanic plate slides

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21
Q

What is sea floor spreading

A

Paleomagnetic signals from past reversals of the earths magnetic field prove that new crust is created by the process of sea floor spreading at mid-ocean ridges

22
Q

Describe Holmes’ hypothesis

A

Said the earths internal radioactive heat was the driving force of convection currents in the mantle that could move tectonic plates

23
Q

Describe slab pull

A

At convergent boundaries, ocean floor is dragged down by a downward gravitational force beneath the adjoining continental crust

24
Q

Describe Wegener’s continental drift hypothesis

A

Said that our now separate continents had once been joined together as supercontinents
Pangea

25
What is the focus
Where the pressure is released underground and where the energy radiates out from Place with the strongest waves that cause the most damage
26
What is the epicentre
The point directly above the centre of the earthquake on the earth’s surface
27
What are seismic waves
When energy is released from the focus in shock waves | Most damage occurs where the shock waves are strongest (closest to epicentre)
28
What causes earthquakes
Release of built up stress Plates are always moving so tensions build up between rocks Stress can suddenly be released when strain overcomes elasticity of the rock Energy is transferred to surface vertically then outwards from epicentre Energy transferred through seismic waves makes ground shake
29
What is a deep-focus earthquake
Those where the focus is 70-700km under the earths surface Caused by previously subducted crust moving towards the core, heating up or decomposing Generally less damaging as shock waves travel further so cause less shaking at surface
30
What is a shallow focus earthquake
Those where the focus is 0-70km under earths surface | Generally more damaging as waves don’t have as far to travel
31
What is an underwater earthquake
Move the seabed, which causes water to get displaced - can cause tsunamis Can be shall or deep focus Deeper the focus, bigger the tsunami Waves travel fast in deep water so tsunamis strike shores with little warning
32
What are P-waves
Primary waves Produced when tectonic stress energy is released Fastest waves but cause the least damage
33
What are L-waves
Love waves Create significant damage, including crustal fracturing Only travel across the surface and have a large amplitude
34
What are S-waves
Secondary waves | Produced by some earthquakes that make ground shake violently
35
What are 2 common primary hazards of earthquakes
Ground shaking | Crystal fracturing
36
Describe the duration and severity of ground shaking
Can range in duration and severity based on magnitude of earthquake and distance from epicentre
37
Describe crustal fracturing
Earth can visibly separate and deep fissures in the ground can be created
38
What are 3 common secondary hazards of earthquakes
Landslides Liquefaction Tsunamis
39
What is liquefaction
When earthquakes compact loose sediments of silts, sand and gravel that are waterlogged Compact ground forces water to rise to the surface and damage buildings and infrastructure
40
Name 4 primary hazards of volcanoes
Ash falls Volcanic gases Pyroclastic flows Lava flows
41
Describe ash falls
Also known as tephra Solid material of varying grain size ejected into the atmosphere Buildings often collapse under the weight Air becomes thick and is difficult to breathe in and can cause respiratory problems E.g. 2010 eruption of Mount Merapi in Indonesia
42
Describe volcanic gas
Can be poisonous e.g. carbon dioxide, carbon monoxide, sulphur dioxide E.g. 1986 eruption of Lake Nyos, Cameroon
43
Describe pyroclastic flows
Very hot (800°C), have a high velocity and are a mixture of gases and tephra Can destroy everything in their paths E.g. AD79 eruption of Mount Vesuvius, 1980 eruption of Mount St. Helens
44
Describe lava flows
Not usually a major threat when they are molten lava as slow moving Create extensive areas of solidified lava E.g. Hawaii and Southwest Iceland
45
Name 2 secondary hazards of volcanoes
Lahars | Jökulhlaup
46
Describe a lahar
Fast mudflows that happen when rain mobilises deposits of volcanic ash E.g. 1985 Armero tragedy took place when Nevado del Ruiz volcano erupted in Colombia, four lahars came towards town and around 20,000 people died
47
Describe jökulhlaups
Flooding that happens when glaciers or ice caps melt | Originates from Iceland where sun glacial outburst floods happen
48
What causes a tsunamis
Most generated by submarine earthquakes at subduction zones Sea bed is displaced vertically which displaced a large volume of water in the ocean column which moves outwards from the point of displacement
49
What are the characteristics of tsunamis
Long wavelength at sea - measured between 2 identical points of a wave, often over 100km long Short amplitude at sea - usually about 1m high and barely noticeable, height increases to over 25m when reach land Velocity - move quickly and reach speeds of 700kph in dee water Drawback - localised drop in sea level Wave-train - way a tsunami hits a coastline is like a series of waves
50
What is the Benioff Zone
Area where friction is created between colliding tectonic plates, resulting in intermediate and deep earthquakes