Volcanic Hazards - Formation Of Volcanoes Flashcards

- process of formation

1
Q

Volcanoes are vents (openings) in the Earth’s crust through which lava,

A

tephra (ash, dust and fragments of material are produced in a volcanic eruption) and gases erupt.

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2
Q

Molten rock beneath the surface is called magma, but

A

When it is ejected to the surface it is called lava.

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3
Q

Magma, in addition to molten rock, may also contain suspended

A

Crystals and dissolved gases and sometimes gas bubbles. Magma often collects in magma chambers that may feel a volcano turn into a pluton.

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4
Q

Underground, the enormous pressure exerted by overlying rocks

A

Keep the rocks in a semi-detatched state.

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5
Q

Fissures and fragments in the crust create area of low pressure that

A

Allow some of the rocks to become molten and rise.

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6
Q

If these molten rock reach the surface

A

They are said to be extrusive.

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7
Q

If they are injected into the crust,

A

Without reaching the surface they are called intrusive.

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8
Q

Active volcanoes

A

Have erupted within living memory - present

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9
Q

Dormant volcanoes

A

Have erupted within historical record - past

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10
Q

Extinct volcanoes

A

Will never erupt again - never

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11
Q

Pyroclasts - origin

A

In all explosive eruptions

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12
Q

Pyroclasts - characteristics

A

Has broken fragments of rock ejected with velocity

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13
Q

Pyroclasts - harmful effects

A

Large rocks which impact on landing

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14
Q

Tephra - origin

A

In all explosive volcanoes

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15
Q

Tephra - characteristics

A

Collective term 4 airborne pyroclasts (including solidifying magma)

  • bombs
  • Laphilli
  • Ash
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16
Q

Tephra - harmful effects

A
  • may spread over distances
  • 1500 km
  • causes minor/major damage
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17
Q

Pyroclastic flow - origin

A
  • explosive eruptions

- caused by eruption collumn

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18
Q

Pyrochlastic flow - characteristics

A
  • Hot
  • Gas charged
  • High velocity flows of Tephra
  • Composed of mixture of bombs, lapilli, ash, extremely hot gases - high deposits of pumice
19
Q

Pyroclastic flows - harmful effects

A
  • may extend many kilometres
  • high velocity
  • lethal mix of bombs, ash, laphilli + hot gases
20
Q

Atmospheric effects- origin

A
  • Eruption collumns which may extend a few collumns into the atmosphere
  • allows ash to be carried by high level winds - pressure of heat drives this
21
Q

Atmospheric effects - Characteristic

A
  • ash + dust particles (including aerosols) - leads to unusual optical effects
22
Q

Atmospheric effects - harmful effects

A
  • clouding blocks sun from reaching Earths surface
  • cools troposphere
  • but gases are released, contributing to troposphere warming
23
Q

Troposphere

A

the lowest region of the atmosphere, extending from the earth’s surface to a height of about 6–10 km (the lower boundary of the stratosphere)

24
Q

Landslides - origin

A

Dislocation of level and rocks by magmatic pressure

25
Q

Landslides - characterictics

A
  • huge flows of rocks
  • mud
  • tephra
26
Q

Landslides - harmful effects

A

Destruction of property and land

27
Q

Lahars - origin

A

Rain water or meltwater loosen tephra

28
Q

Lahars - characteristics

A
  • volcanic mudflow
  • move downhill
  • movement is dependent on topography - almost
  • perpenducular (as it is steep) = faster
  • gentle slope = slow movement
29
Q

Lahars - harmful effects

A
  • extensive destruction of property
  • loss of life
  • e.g. Navado Del Ruiz, Colombia 1985
    Mount Pintubo
30
Q

Lava flows - origin

A
  • any eruptions
31
Q

Lava flows - characteristics

A
  • the rate of flow depends on temperature
  • increased temperature = fast
  • decreased temperature = slow
  • as lava cools viscosity ☝️and speed 👇 till less than walking speed.
  • as it cools a solidified surface is produced
  • volume + range are variable - may extend up to 100 km from source
32
Q

Lava flows - harmful effects

A
  • ignition of fires + burial of land + built environment
  • relatively slow rate
  • little risk to life
33
Q

Poisonous gas - origin

A

Any eruption

34
Q

Poinsonous gas - characteristics

A
  • ash laden gases

- carbon monoxide, co2, hydrochloric acid, hydrofluric acid, sulfur dioxide

35
Q

Poisonous gases - harmful effects

A
  • toxic
  • contributes to acid rain
  • 1700 people suffered from asphyxiation by co2 in 1968 eruption at Lake Monoun Cameroon
  • may cause long term starvation and wodespread diseases
36
Q

Flooding - origin

A

Submarine explosions = displaced large volumes of rock and hence water
- blockage of river by lahars or lava flows

37
Q

Characteristics of flooding

A

Flood of fresh/salt water.

Either gradual or rapid.

38
Q

Harmful effects of flooding

A
  • dramatic changes in erosion + deposition pattern

- destruction of properties and agricultural land

39
Q

Beneficial effects of volcanism (BEV)

A
  • Tourism
  • Soil
  • Volcanic ash
  • Industrial materials + chemicals
  • Geothermal water
40
Q

BEV - TOURISM

A

Scenic landscapes

Increases potential for tourism

41
Q

BEV - SOIL

A

Driven from basic/balsaltic lava = fertile

42
Q

BEV - VOLCANIC ASH

A
  • Rich in K
  • phosphorus - rich in natural fertilisers
    THIS explains POPULARITY 4 SETTLING around these areas
43
Q

BEV - INDUSTRIAL MATERIALS + CHEMICALS

A
  • sulfur
  • pumice
  • boric acid
  • ammonia
  • silica - cosmetics, hair care etc
44
Q

BEV - GEOTHERMAL WATER

A

As water reaches the surface it proves as useful = harnessed for energy
Homes heated by this method
E.g. Italy, US, Mexico, New Zealand and former USSR - naturally occuring heat is used to produce electricity.