Tectonic Processes & Hazards - EQ1 - 1.2C Flashcards

1
Q

The processes which occur at the plate boundaries impact on the ….. of the eruption or earthquake

A
  • magnitude
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2
Q

The ………. of the magma have a crucial role on the ………… and …………….. of eruptions

A

The properties of the magma have a crucial role on the magnitude and frequency of eruptions

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3
Q

What are eruptions usually like at divergent boundaries

A
  • Eruptions tend to be small andeffusive
  • The eruptions are usually of basalt lava:
    • Low gas content
    • Lowviscosity
    • Higher temperature
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4
Q

What are earthquakes usually like at divergent boundaries

A
  • Earthquakes tend to be mild and shallow
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5
Q

What are earthquakes usually like at convergent boundaries

A
  • Friction and pressure build up in theBenioff zone(the area within the subduction zone where most friction and pressure build up occurs)
  • which causes strong earthquakes
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6
Q

What are eruptions usually like at convergent boundaries

A
  • Volcanic eruptions tend to be explosive as the magma is forcing its way to the surface
  • These eruptions are often rhyolite lava:
    • High gas content
    • High viscosity
    • Lower temperature
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7
Q

What is tectonic activity like at transform boundaries

A
  • Plates can stick causing a significant build up of pressure and powerful earthquakes
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8
Q

What are the 3 types of lava

A
  • basaltic lava
  • andesitic lava
  • rhyolitic lava
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9
Q

The higher the gas level in an erruption –> the more ….

A

destructive

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10
Q

What is the tectonic setting of basaltic lava

A
  • Oceanic Hot Spot - Hawaii
  • Constructive - Iceland
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11
Q

What is the temperature of basaltic lava

A
  • Hottest 1000-1200 degrees celcius
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12
Q

What are the main minerals in basaltic lava

A
  • low silica (50%), water, gases & aluminium
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13
Q

What are the gas content of basaltic lava

A
  • low 0.5-2%
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14
Q

How is basaltic lava formed

A
  • melting of upper mantle minerals mainly from upper zone
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15
Q

What are the flow characteristics of basaltic lava

A
  • thin & runny, low viscocity, gases escape
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16
Q

What is the erruption energy of basaltic lava

A
  • gentle, effusive
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17
Q

What are the hazards of basaltic lava

A
  • lava flow
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18
Q

What is the silica content % of basaltic lava

A

45-55%

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19
Q

Colour characteristics of basaltic lava

A
  • black to dark grey
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20
Q

What is the tectonic setting of andesitic lava

A
  • Destructive plate margin - Andes
  • Island arc margin - Montserrat
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21
Q

What is the temperature of andesitic lava

A
  • 800-1000 degrees celcius
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22
Q

What are the main minerals in andesitic lava

A
  • intermediate silica (60%), gas content, magnesium & iron
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23
Q

What are the gas content of andesitic lava

A
  • medium 3-4%
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24
Q

How is andesitic lava formed

A
  • subducted oceanic plate melts and mixes with seawater, lithospheric mantle and continental rocks
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25
Q

What are the flow characteristics of andesitic lava

A
  • show, intermediate viscocity and traps gases
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26
Q

What is the erruption energy of andesitic lava

A
  • violent, moderately explosive
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27
Q

What are the hazards of andesitic lava

A
  • lava flow
  • ash and tephra
  • pryroclastic flow
  • lahar
  • gas emission
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28
Q

What is the silica content % of andesitic lava

A

55-65%

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29
Q

Colour characteristics of andesitic lava

A
  • medium to dark grey
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30
Q

What is the tectonic setting of rhyolitic lava

A
  • Continental Hot Spot - Yellowstone
  • Continental Collision Zone - Himalayas
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31
Q

What is the temperature of rhyolitic lava

A
  • coolest 600-900 degrees celcius
32
Q

What are the main minerals in rhyolitic lava

A
  • high silica (70%),potassium, sodium, aluminium & gas content
33
Q

What are the gas content of rhyolitic lava

34
Q

How is rhyolitic lava formed

A
  • melting of lithospheric mantle & slabs of previously subducted plate
35
Q

What are the flow characteristics of rhyolitic lava

A
  • thick & stiff, high viscocity, diffult for gases to escape
36
Q

What is the erruption energy of rhyolitic lava

A
  • very violent, cataclysmic
37
Q

What are the hazards of rhyolitic lava

A
  • cataclysmic explosion
  • pryroclastic flow
38
Q

What is the silica content % of rhyolitic lava

39
Q

Colour characteristics of rhyolitic lava

A
  • light colour
40
Q

Where are the strongest sesimic waves (earthquakes) created

A
  • Where there is most friction and build-up of strain between two plates
  • This is greatest at destructive plate margins
41
Q

Where have the most intense earthquakes occurred

A
  • The five recorded earthquakes of 9 or higher on the Moment Magnitude Scale (MMS) have been on destructive plate boundaries (for example, Tohoku, Japan 2011)
  • Tsunamis are also more intense with this earthquake location
42
Q

Do transform faults have strong earthquakes

A
  • Transform faults also have earthquakes with a strong magnitude (for example, 7 on the MMS)
  • as plates are trying to slide past each other leading to friction and strain
43
Q

Where are volcanoes strongest & why?

A
  • Volcanoes are more explosive where the magma is viscous with a high silica and gas content;
  • these are found at destructive plate margins with subduction, where the subducted plate is melted, usually under a continental plate
44
Q

Volcanoes are landforms which develop around…….
They are closely asscoiated with…….

A

Volcanoes are landforms which develop around weaknesses in the earths crust where magma, gases & preexisting volcanic material are extracted
They are closely asscoiated with plate boundary activities

45
Q

What are the 3 types of volcano

A
  • active
  • dormant
  • extinct
46
Q

What are the 2 main types of volcanoes

A
  • shield & composite
47
Q

What is the plate boundary of shield volcanoes

A

constructive

48
Q

What is an example of a shield volcano

A

Muana Loa, Hawaii USA

49
Q

What is the lava type of shield volcanoes

A
  • thinner lava - travels a long way before it cools
50
Q

What is the structure of shield volcanoes

A
  • gentle sides
51
Q

What are the eruptions of shield volcanoes

A
  • more frequent but less violent
52
Q

What is the tectonic setting of basaltic lava

A
  • Oceanic Hot Spot - Hawaii
  • Constructive - Iceland
53
Q

What is the temperature of basaltic lava

A
  • Hottest 1000-1200 degrees celcius
54
Q

What are the main minerals in basaltic lava

A
  • low silica (50%), water, gases & aluminium
55
Q

What are the gas content of basaltic lava

A
  • low 0.5-2%
56
Q

How is basaltic lava formed

A
  • melting of upper mantle minerals mainly from upper zone
57
Q

What are the flow characteristics of basaltic lava

A
  • thin & runny, low viscocity, gases escape
58
Q

What is the erruption energy of basaltic lava

A
  • gentle, effusive
59
Q

What are the hazards of basaltic lava

60
Q

What is the silica content % of basaltic lava

61
Q

Colour characteristics of basaltic lava

A
  • black to dark grey
62
Q

What is the plate boundary of composite volcanoes

A

destructive

63
Q

What is an example of a composite volcano

A

Mount St. Helens, Washington USA

64
Q

What is the lava type of composite volcanoes

A
  • viscous magma, trap hot gas & large amounts of water
65
Q

What is the structure of composite volcanoes

A
  • coneshape, layered steep sides
66
Q

What are the eruptions of composite volcanoes

A
  • not frequent but very violent
67
Q

Explain how magma comes to be lava

A
  • Deep within the Earth it is so hot that some rocks slowly melt and become a thick flowing substance called magma
  • Since it is lighter than the solid rock around it, magma rises and collects in magma chambers
  • Eventually, some of the magma pushes through vents and fissures to the Earth’s surface
  • Magma that has erupted is called lava
68
Q

Non-violent eruptions

The explosivity of an eruption depends on the….

A

composition of the magma

69
Q

Non-violent eruptions

If magma is thin and runny,………………. easily from it.
When this type of magma erupts, it……
A good example is the eruptions at……..

A
  • gases can escape
  • flows out of the volcano
  • Hawaii’s volcanoes
70
Q

Non-violent eruptions

Lava flows rarely kill people because…

A
  • they move slowly enough for people to get out of their way
71
Q

How do violent erruptions occur

A
  • If magma is thick and sticky, gases cannot escape easily
  • Pressure builds up until the gases escape violently and explode
72
Q

What is a good example of violent eruptions

A
  • The eruption of Washington’s Mount St. Helens
73
Q

What is tephra

A
  • In violent eruptions (possibly of andestic lava), the magma blasts into the air and breaks apart into pieces called tephra
  • Tephra can range in size from tiny particles of ash to house-size boulders
74
Q

What is the VEI

A
  • The VEl is a relative measure of the explosiveness of a volcanic eruption,
  • the scale that enables explosive volcanic eruptions to be compared with one another
75
Q

What does VEI stand for

A

Volcanic explosiveness index

76
Q

Why is the VEI valuable

A
  • It is very valuable because it can be used for both:
  • recent eruptions that scientists have witnessed
  • & historic eruptions that happened thousands to millions of years ago
77
Q

What is the VEI based on

A
  • The volume of tephra (ash) produced during an eruption and uses the following factors to assign a number:
  • The amount of the volcanic material ejected (tephra and ash falls etc)
  • How long the eruption lasts
  • Height of eruption cloud
  • Qualitative descriptive terms (such as ‘gentle’, ‘explosive’, etc.)