Volcanic Hazards - Formation Of Volcanoes Flashcards

- process of formation (44 cards)

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
Landslides - characterictics
- huge flows of rocks - mud - tephra
26
Landslides - harmful effects
Destruction of property and land
27
Lahars - origin
Rain water or meltwater loosen tephra
28
Lahars - characteristics
- volcanic mudflow - move downhill - movement is dependent on topography - almost - perpenducular (as it is steep) = faster - gentle slope = slow movement
29
Lahars - harmful effects
- extensive destruction of property - loss of life - e.g. Navado Del Ruiz, Colombia 1985 Mount Pintubo
30
Lava flows - origin
- any eruptions
31
Lava flows - characteristics
- 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
Lava flows - harmful effects
- ignition of fires + burial of land + built environment - relatively slow rate - little risk to life
33
Poisonous gas - origin
Any eruption
34
Poinsonous gas - characteristics
- ash laden gases | - carbon monoxide, co2, hydrochloric acid, hydrofluric acid, sulfur dioxide
35
Poisonous gases - harmful effects
- 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
Flooding - origin
Submarine explosions = displaced large volumes of rock and hence water - blockage of river by lahars or lava flows
37
Characteristics of flooding
Flood of fresh/salt water. | Either gradual or rapid.
38
Harmful effects of flooding
- dramatic changes in erosion + deposition pattern | - destruction of properties and agricultural land
39
Beneficial effects of volcanism (BEV)
- Tourism - Soil - Volcanic ash - Industrial materials + chemicals - Geothermal water
40
BEV - TOURISM
Scenic landscapes | Increases potential for tourism
41
BEV - SOIL
Driven from basic/balsaltic lava = fertile
42
BEV - VOLCANIC ASH
- Rich in K - phosphorus - rich in natural fertilisers THIS explains POPULARITY 4 SETTLING around these areas
43
BEV - INDUSTRIAL MATERIALS + CHEMICALS
- sulfur - pumice - boric acid - ammonia - silica - cosmetics, hair care etc
44
BEV - GEOTHERMAL WATER
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.