2 a and b landforms, landscapes and hazards Created By Volcanic Eruptions Flashcards

1
Q

Type of eruption at a convergent boundary

A

Explosive

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2
Q

Explosive eruptions material ejected

A

Gases (direct and indirect greenhouse gases)
Ash
Pumice
Pyroclastic flow
Rhyolitic lava

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3
Q

Explosive eruptions characteristics

A

Convergent boundary
Viscous rhyolitic lava
900°C
High silica content
Plinian eruption

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4
Q

Effusive eruption plate boundary

A

Divergent

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5
Q

Effusive eruption material ejected

A

Little gas
Basaltic (runny lava)

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6
Q

Effusive eruption characteristics

A

Basaltic lava
Low silica content
1160°C lava
Icelandic and Hawaiian
Erupts over a long period of time
E.g. Erta Ale (EARV)

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7
Q

Basaltic lava

A

48-52% silica (v low)
1160°C ( v hot)
Viscous lava

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8
Q

Andenistic lava

A

52-63% silica
Somewhat viscous

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9
Q

Rhyolitic lava

A

900°C (cool)
Viscous
68-77% silica

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10
Q

3 ways magma is generated

A

1) increasing temperature causing rock to melt
2) decreasing pressure (decompression melting) as rocks ascend to lower pressure levels
3) introduction of volatiles ( principally water) lowers the melting point of rocks

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11
Q

Hotspot definition

A

An area of intense volcanic activity where a mantle plume reaches the earth’s surface causing eruptions

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12
Q

Are hotspots located on plate boundaries?

A

No

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13
Q

What is the Hawaiian hotspot?

A

Pacific plate moves NW 10cm/year
Created basalt volcano peaks
As the plate moves volcanoes lose their source of magma and become extinct
Eroded and submerged

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14
Q

Height of Muana Loa on Hawaii

A

400m above sea level

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15
Q

Processes occurring at a hotspot

A

Localised source of heat energy that sustains a volcanism
The weight of the volcano bends the plate down
Isostatic change and later rebound
Thermal plume moves through dike

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16
Q

East African Hotspot

A

Crust stretched under tension for 30 million years
Rifting has allowed magma to reach the surface creating a line of active volcanoes
Mount Kilimanjaro was formed this way

17
Q

Example of a hotspot volcano which is not shield

A

El Teide, Tenerife
Stratovolacano

18
Q

How much material is ejected by a supervolcano

A

1000km3 in a single eruption event

19
Q

Size of calderas

A

75km in diameter in Yellowstone
Huge

20
Q

Frequency of supervolcanic eruption

A

Infrequent
Last supervolcanic eruption was 27000 years ago in New Zealand

21
Q

Shot term impact of SV ash cloud

A

1000km3 material
Tephra falls into crops
Dust block stomata and cuticle, no photosynthesis, crop failure
Ashcloud prevents short wave solar radiation from entering the atmosphere, temperature drops
Famine and ecological deviation

22
Q

How many mass extinctions have been caused by volcanos

A

2

23
Q

Long term impacts of SV eruption

A

Direct GHG (CO2 H2O)
Indirect GHG (SO2 CO)
GHG effect
Global warming, sea level rise and extreme weather

24
Q

Magnitude of volcanic eruption definition

A

Amount of material erupted

25
Q

Intensity of volcanic eruption definition

A

Speed at which material is erupted

26
Q

The four factors measured for VEI

A

Magnitude
Intensity
Height ejected material
Duration of eruption

27
Q

Scale for VEI

A

0-8 (logarithmic)

28
Q

Evaluation of VEI

A

Less useful for effusive eruptions but is useful in determining relative impacts volcano might have on different geographic scales

29
Q

Jökulhlaups

A

glacial outburst flood
They occur when a lake (fed by glacial meltwater) breaches its dam and drains catastrophically
these floods are extremely powerful and high volume causing significant damage to surrounding land

30
Q

lava bomb

A

a mass of partially molten rock (tephra)
larger than 64 mm in diameter
formed when a volcano ejects viscous fragments of lava during an eruption.
Because volcanic bombs cool after they leave the volcano, they are extrusive igneous rocks.

31
Q

pyroclastic flow

A

hot gas , ash and rock fragments
up to 100kmph
highly destructive
localised effect
follow the topography
inhaling causes instant death
can cause pyroclastic dam from blocked river (delayed onset)

32
Q

lahar

A

mud flows combined with ash- warm
very destructive
follows topography
50kmph
can be formed due to melting glacier
monsoon can dislodge unconsolidated ash (delayed onset)