Week 8: Volcanic Hazards Flashcards

(46 cards)

1
Q

It is an opening in the earth’s
crust where lava, pyroclastics and
gases are ejected onto the surface during eruptions.

A

Volcano

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2
Q

This part of the volcano is a steeped-wall depression at the peak of the volcano and the volcanic vent.

A

Crater

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3
Q

This part of the volcano a very large crater that can exceed for about 1 km in diameter; they are formed when the summit of the volcano collapses during violent or explosive eruptions.

A

Caldera

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4
Q

This part of the volcano is the most prominent part of a volcano.

A

Cone

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5
Q

This part of the volcano formed by the mountainous accumulation of volcanic materials

A

Cone

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6
Q

This kind of volcano has a recent history of eruptions (within the last 10,000 years); they are also likely to erupt again.

A

Active volcano

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7
Q

Identify the different parts of a volcano.

A
  1. Ash cloud
  2. Main/Primary vent
  3. Magma chamber
  4. Crater
  5. Lava flow
  6. Conduit
  7. Cone
  8. Dome
  9. Secondary vent
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8
Q

This kind of volcano have not erupted in a long time but are expected to erupt again in the future (has not erupted in the past 10,000 years).

A

Dormant/Inactive Volcano

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9
Q

This kind of volcano are not expected or are unlikely to erupt again (30,000-40,000 years of no eruption).

A

Extinct volcano

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10
Q

Occurs when lava is ejected to the surface through an opening in the earth’s crust.

A

Volcanic eruption

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11
Q

This type of eruption is non-explosive or quiet. It is dominated by flow of lava and formation of fountains and lakes.

A

Effusive eruption

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12
Q

This type of eruption is also called violent or Plinian eruption. It ejects ash and larger fragments of broken up pyroclastic materials, forming ash clouds that eventually collapse and cover the slope of the volcano.

A

Explosive eruption

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13
Q

Identify if it is effusive or explosive eruption: Less Silica/Higher Temperature/More Gas/Less Viscous

A

Effusive eruption

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14
Q

Identify if it is effusive or explosive eruption: More Silica/Lower Temperature/Less Gas/More Viscous

A

Explosive eruption

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15
Q

This type of eruption is magma-driven.

A

Magmatic eruption

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16
Q

This type of eruption is steam-driven; it is due to the heating of surface or groundwater near a magma chamber.

A

Phreatic eruption

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17
Q

This type of eruption involves the interaction of magma and water.

A

Phreatomagmatic eruption

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18
Q

This phreatomagmatic eruption involves volcanic eruptions of volcanoes on shallow waters.

A

Surtseyan eruption

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19
Q

This phreatomagmatic eruption involves volcanic eruptions of volcanoes under the water.

A

Submarine eruption

20
Q

This phreatomagmatic eruption involves volcanic eruptions of ice-covered volcanoes.

A

Subglacial eruption

21
Q

This magmatic eruption type is effusive, with streams of molten basaltic lava that flow from long, parallel fissures. These often build lava plateaus.

A

Icelandic eruption

22
Q

This magmatic eruption type is also effusive. However, fluid lava flows from a volcano’s summit and radial fissures to form shield volcanoes, which are quite large and have gentle slopes.

A

Hawaiian eruption

23
Q

This magmatic eruption type involve moderate bursts of expanding gases that eject clots of incandescent lava in cyclical or nearly continuous small eruptions.

A

Strombolian eruption

24
Q

This magmatic eruption type is characterized by moderate explosions of gas laden with volcanic ash–which together form dark, turbulent, rapidly ascending eruption clouds.

A

Vulcanian eruption

25
This magmatic eruption type is noted for its explosive outburstst that produce pyroclastic flows, dense mixtures of hot volcanic fragments and gas that roll down slopes at high speeds.
Pelean
26
This magmatic eruption type is an intensely violent in which the uprushing gases and volcanic fragments resemble a gigantic rocket blast directed vertically upward.
Plinian eruption
27
This volcanic shape has a narrow base and a steep slope. It is made up of loose fragments called cinders (pyroclasts and tephra).
Cinder cone volcano
28
This volcano shape is formed from explosive eruption
Cinder cone volcano
29
This volcanic shape has a wide base with gently sloping sides. It is made up purely of solidified lava.
Shield cone volcano
30
This volcanic shape is formed from effusive eruption.
Shield cone volcano
31
This volcanic shape is composed of alternating layers of lava and cinders.
Composite volcano
32
This volcanic shape is formed when volcanic eruptions vary between quiet and violent and explosive.
Composite Volcano
33
This volcanic hazard refers to hot dry masses of fragmented volcanic materials that move along the slope and in contact with ground surface. This includes: pumice flow, ash flow, block-and-ash flow, nuee ardente and glowing avalanche.
Pyroclastic flow
34
This volcanic hazard is a glowing eruption cloud characterized by extreme heat (about 500 °C or higher).
Nuee ardente
35
This volcanic hazard is a highly elongated mass of molten rock materials cascading downslope from an erupting vent. The lava flow being extruded has low silica and low water contents.
Lava flow
36
This volcanic hazard involves rocks that an erupting volcano sends into the air. The rocks can vary in size and density– some can be as small as ash, others are as big as boulders. Examples are lapilli, cinders, blocks and bombs.
Ballistic projectile
37
This volcanic hazard is dangerous due to their temperature and toxicity. This contains water vapor, carbon monoxide, carbon dioxide, hydrogen sulfide, hydrogen chloride, hydrogen fluoride and helium.
Volcanic gases
38
When this gases mix with water, they form an acidic solution.
Volcanic gases
39
It is made of small jagged pieces of rocks, minerals, volcanic glass less than 2 mm in diameter (about the size of sand)
Ash fall
40
This volcanic hazard involves fine, silica-rich particles that are extremely abrasive, mildly corrosive, conducts electricity when wet and does not dissolve in water.
Volcanic ashfall
41
This volcanic hazard is sometimes called mudflows or volcanic debris flows; are flowing mixtures of volcanic debris and water.
Lahar
42
Lahar that is associated directly with volcanic eruption.
Primary or hot lahar
43
Lahar that is caused by heavy rainfall.
Secondary or cold lahar
44
TRUE OR FLASE: Lahar in tropical areas can be produced by: * sudden draining of a crater lake, caused by either an explosive eruption or collapse of a crater fall (e.g. Agua, Kelut, Ruapehu) * movement of a pyroclastic flow into a river or lake, displacing and mixing with water * avalanche of water-sustained rock debris, where water can be from heavy rain, hydrothermal activity or other sources
TRUE
45
TRUE OR FLASE: Lahar in tropical areas can be produced by: * torrential rainfall on unconsolidated deposits on slope of a volcano (e.g. Pinatubo) * collapse of a temporary dam, where recent volcanic deposits have blocked a steam channel (e.g. Asama, Pinatubo
TRUE
46
Earthquake is caused by the movement of magma beneath the surface of the Earth.
Volcanic earthquake