Volcanic Hazards Flashcards

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1
Q

formation of a volcano

A

plates subducts
friction causes plate to melt into magma
this is less dense so rises
breaks through crust to form volcano

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2
Q

types of volcanic hazard

A

primary
- lava flow
- gas
- ash fallout
- pyroclastic flow
- tephra

secondary
- lahars
- acid rain

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3
Q

pyroclastic flow

A

explosion of ash, has and volcanic rock that flow down side of volcano

  • high speeds - 200m/s
  • long way - up to 15km
  • little warning

eg Mount Pelee

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4
Q

lava flow

A

flow of Laval from vets
distance depends on
- viscosity
- steepness of volcano

often slower so people can evacuate
but very destructive, cause fires

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5
Q

volcanic gases

A

releases CO2 and sulphur dioxide
into atmosphere

can be harmful to humans and animals if inhaled

eg Mammouth Lakes, California
CO2 released causing suffocation

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6
Q

ash fallout

A

tephra and material ejected in eruptions fall back down
large pieces fall closer

larger can damage buildings and people
smaller particles can travel thousands of kilometres, damage agriculture and hinders transport

eg Eyjafjalllajokull

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7
Q

nuees ardentes

A

dense, rapid moving clouds of hot gases, ash
a type of pyroclastic flow
- denser so doesn’t move as far

eg Mount Pelee

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8
Q

tephra

A

solid material ejected in an eruption
larger pieces fall closer

eg Pompeii

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9
Q

lahars

A

when volcanic material mixes with water from rainfall or ice melt
- moves fast, over 80km/h
- travel far, tens of km

bury or destroy habitats and infrastructure

eg Nevado del Ruiz, Colombia

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10
Q

acid rain

A

volcanic gases can react with water vapour
fall as acid rain
damages ecosystems and can erode metal

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11
Q

primary impacts

A

social
- death
- collapse of infrastructure

environmental
- ecosystems damaged

economic
- businesses destroyed
- agriculture damaged

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12
Q

secondary impacts

A

fires caused by lava
- destroy ecosystems and buildings

lahars
- bury buildings and ecosystems

flooding from ice melts

food shortages due to damage

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13
Q

short term responses

A

evacuation
emergency food supplies

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14
Q

long term responses

A

designed to reduce impacts for future

monitoring
reconstruction - buildings strengthened
barriers to divert flow
preparation

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15
Q

volcanic form on constructive margins

A

plates moving apart

  • basaltic lava
  • runny, less viscous, lower in silica
  • less violent eruptions
  • more frequent
  • mainly lava
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16
Q

volcanic form on destructive margins

A

plates moving towards

  • acidic lava
  • vicious, higher in silica
  • potentially explosive
  • less frequent
  • tephra and pyroclastic flow
17
Q

adaptation

A

buildings strengthened
- reduce risk of collapse under ash

capitalise on opportunities
- farming on fertile soils
- tourism

18
Q

prevention

A

not possible
but risk can be reduced

  • evacuation, using prediction
  • land use zoning, not developing in at risk areas
19
Q

mitigation

A

reduce severity

monitoring
- allows prediction and evacuation

emergency shelters and supplies
- save lives

barriers to divert flows away from populated areas
eg Iceland, 4m walls

20
Q

preparedness

A

monitoring systems
- allow prediction
- monitor gases and seismic activity

evacuation plans

emergency shelters and supplies

21
Q

distribution

A

90% as plate boundaries
other caused by magma plumes
- vertical commons or extra hot magma
- rises and breaks through crust

22
Q

magnitude

A

measured on VEI scale
1-8 on destruction

Criticised, Only measures tephra

23
Q

frequency

A

depends of type of margin

constructive - more frequent, can be continuous

destructive - less frequent

24
Q

predictability

A

monitored
gases and seismic activity measured

can be predicted
- allows of evacuation

eg Iceland, 30 minute warning

25
Q

regularity

A

unpredictable

can erupt regularly
or can be dormant or many years

26
Q

Primary vs secondary impacts

A

Pyroclastic flow worse primary - hardest to avoid, move fast and far

Secondary worse
Lahars
- Nevada Del Ruiz

Flooding
Tsunamis

Effect climate
- Mount Pinatubo eruption reduced global temperatures by 1c