Volcanoes Flashcards

1
Q

What is a volcano?

A
  • Any landform (on land or beneath the ocean) that releases lava, gas, or ashes, or has done so in the past
  • Most occur at divergent or convergent plate boundaries
  • Anomalous volcanism can sometimes occur in the middle of a plate (intraplate volcanism)
  • Anomalous volcanoes may be the result of: hot magma rising from the core-mantle boundary or asteroid impacts
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2
Q

Good evidence that Hawaii is situated over a:

A

hotspot (islands in a row b/c plate is moving making holes as it moves = islands, tells us plate motion)

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3
Q

Magma (and lava) can be:

A

felsic, intermediate, or mafic

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4
Q

How does magma chemistry influence the nature of volcanic eruptions?

A
  • Fewer covalent bonds between tetrahedra = thin, runny magma (mafic, low silica)
  • More covalent bonds b/w tetrahedra = thick magma (felsic, high silica)
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5
Q

Mafic (basaltic) lava flows easily and erupts gently

A
  • Low silica content
  • Low viscosity (good at off-gassing (releasing gas) due to low viscosity)
  • Low gas
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6
Q

Mafic (basaltic) lava flows easily and erupts gently

A
  • Low silica content
  • Low viscosity (good at off-gassing (releasing gas) due to low viscosity)
  • Low gas
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7
Q

Mafic lava textures

A

Aa - rough, fragmented lava blocked called “clinker”

Pahoehoe - smooth, shiny, and ropy surface

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8
Q

Felsic magma tends to erupt catastrophically

A
  • High silica content
  • More viscous (resistant to flowing)
  • High gas content (trapped between silica tetrahedra/crystals)
  • Expanding gases fragment magma and rock, producing pyroclastic debris or tephra
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9
Q

Intermediate magma eruptions are less

A

explosive

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10
Q

Types of pyroclastic debris

A
  • Ash
  • Lapilli (tiny pieces of rock)
  • Volcanic bombs (rocks size of fist)
  • Volcanic block (house/car size)
  • Welded tuff (compacted tiny rocks into rock)
  • Pumice (vesicular)
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11
Q

H2O, CO2, SO2 are the most

A

abundant gases released during an explosion

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12
Q

What happens to the SO2 gas released during an explosion?

A

Sulphuric acid = acid rain

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13
Q

Volcanoes can be classified into 2 groups:

A
  1. Central vent volcanoes: central vent, summit crater

2. Large-scale volcanic terrains: no central vent, network of source material, extend over a large area

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14
Q

Types of central vent volcanoes

A
  • Shield Volcanoes
  • Stratovolcanoes
  • Rhyolite Caldera Complexes
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15
Q

What is a shield volcano?

A

low silica, low gas magma originates in mantle, low viscosity creates broad gentle slopes

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16
Q

What is a stratovolcano?

A

Alternating layers of mafic to intermediate lava flows with layers of intermediate to felsic explosively ejected pyroclastic fragments, explosive eruptions are common due to buildup of gases

17
Q

What is a Rhyolite Caldera Complex volcano?

A

High silica, high gas magmas, massive explosions (most explosive of all types), withdrawal of magma from the magma chamber causes collapse, produces an “inverse volcano” or caldera

18
Q

Large-scale volcanic terrains

A
  • Mid-ocean ridges develop at divergent boundaries, basaltic flow creates a global network of interconnected seafloor ridges
19
Q

Volcanoes are highly variable in terms of:

A

size

20
Q

Volcano type is related to:

A

kind of magma

21
Q

Divergent boundary: mafic

A

lava flows

22
Q

Oceanic hot spot:

A

mafic lava flows, shield volcanoes

23
Q

Continental hotspot:

A

felsic to mafic lava flows, can be any type

24
Q

Oceanic-continental subduction zones:

A

felsic to mafic

25
Q

Ocean-oceanic:

A

intermediate to mafic lava flow, shield or stratovolcanoes, volcanoes form an island arc