MIDTERMS Flashcards

(35 cards)

1
Q

a vent, hill or mountain from which molten or hot rocks with gaseous materials are ejected

A

Volcano

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2
Q

can be craters, hills or mountains formed by removal of pre-existing material or by accumulation of ejected materials

A

Volcano

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3
Q

erupted w/in historical times (last 600 yrs); has written historical accounts or oral tradition

A

Active

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4
Q

landform is young-looking but w/ no records or proof of eruption

A

Potentially Active

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5
Q

long-period inactivity is evident from too much weathering & erosion of deep & long
gullies (valleys)

A

Inactive

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6
Q

one that hasn’t erupted in the past 10,000 BUT which is expected to erupt
again

A

Dormant

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7
Q

one that nobody expects to ever erupt again (note there have been eruptions
from “extinct” volcanoes

A

Extinct

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8
Q

ultravulcanianeruptionorsteam-blast eruption, occurs when magma heats ground or surface water.

A

Phreatic Eruption

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9
Q

Veryviolenteruptiongeneratedbytheexplosivecontactof erupting magma with water; Voluminous, slightly tall ash columns, laterally-projected pyroclastic currents (base surges) & blasts

A

Phreatomagmatic

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10
Q

Characterized by a dense cloud of ash-laden gas exploding from the crater and rising high above the peak.

A

Vulcanian

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11
Q

Highlyexplosive,with dense clouds of gas and tephra being propelled
upwards for many kilometres;

A

Plinian

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12
Q

What are the types of Eruption?

A

Phreatic Eruption
Phreatomagmatic
Vulcanian
Plinian

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13
Q

What are the Volcanic hazards?

A
Tephra Fall
Lava Flow
Pyroclastic flow
Lahars
Volcanic Gases
Ground Fissuring
Debris Avalanche
Volcanic Tsunami
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14
Q

Gravitational settling of volcanic ash & fragments from the umbrella clouds of tall eruption columns & ash clouds of pyroclastic flows

A

Tephra Fall

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15
Q

Incandescent rivers of hot molten rock (lava)

• Erupted from volcanic craters, fissures, during Hawaiian- Strombolian activity, lava dome eruptions

A

Lava Flow

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16
Q

Turbulent mass of ejected fragmented volcanic materials (ash & rocks) + hot gases that flow downslope at very high speeds (30-700 kph)

A

Pyroclastic Flow

17
Q

Rapidly flowing thick mixture of volcanic sediments and water
• Triggered by rainfall, melting of craterial icecaps, lake breakout or hydrothermal
“squeezing”

18
Q

It illustrates thickness variations within a tabular unit, layer or stratum. Isopachs are contour lines of equal thickness over an area

19
Q

Volcanic hazards zonation map

A

Show areas identified to be prone to a particular volcanic phenomena
• Tool to gauge the degree of susceptibility of a given area to a particular hazard
• Determine which areas should be evacuated and avoided during eruptions
• Provide guidelines for long-range land use planning around volcanoes that take
into account potential hazards from future eruption

20
Q

an individual particle ejected during a volcanic eruption; usually classified according to size

21
Q

pertaining to clastic rock material formed by explosion from a volcanic vent; also pertaining to rock texture of explosive origin; not synonymous with adjective “volcanic”

22
Q
  • any rock consisting of unreworked solid material of whatever size explosively or serially ejected from a volcanic vent
A

Pyroclastic Rock

23
Q

any volcanic material that is ejected into the air (ejecta).

A

Pyroclastic Materials

24
Q

(32 mm diameter) and are solid when ejected

25
32 mm diameter) and are liquid when ejected
Bombs
26
- rock fragments formed from ejected droplet of magma
Lapilli
27
4mm, usually glass, but sometimes contain mineral fragments
Ash
28
consolidated ash | (welded) is called
Tuff
29
Involve rapid release and decompression of gas which results simultaneously in fragmentation and ejection of magma and/or wall rocks
Explosive eruption
30
3 types/styles based on differences in the source of the gas and extent of direct involvement of magma
Explosive magmatic Phreatomagmatic Phreatic
31
How pyroclastics disperse?
1. Injection into the atmosphere followed eventually by fallout from suspension 2. Ground hugging, relatively high particle concentration pyroclastic flows; 3. Relatively low particle concentration pyroclastic surges;
32
groups of clasts, or clasts plus interstitial fluid (air, water, volcanic gas) move together and interact; mass flows vary widely in rheology and particle concentration
Mass flow transport
33
clasts are entrained in moving interstitial fluid (air, water, volcanic gas) and are free to behave independently
Traction transport
34
clasts are fully suspended in interstitial fluid (air, water, volcanic gas).
Suspension Transport
35
high buoyant plume carrying all except coarsest particles to heights of kilometers to tens of kilometers above the surface
Pyroclastic fall