Week 6 Flashcards

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1
Q

What are shield volcanoes

A
  • Low aspect ratio due to the fluidity of lava
  • non-explosive eruptions are common
  • broad and gentle slopes
    e.g Mauna Loa
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2
Q

What is the magma type for shield volcanoes

A
  • lavas that erupt in Hawaii are basaltic and contain about 50% silica
  • They erupt at about 1200 degrees c
  • very fluid and pasty
  • effusive
  • low silica
  • low viscosity
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3
Q

What is the eruption type for shield volcanoes

A

Hawaiian type eruption

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4
Q

Hawaiian type eruption

A
  • Lava is very fluid and hot
    -Bubbles can expand and escape easily
  • relatively gentle
  • low energy eruption
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5
Q

What are stratovolcanoes

A
  • Higher aspect ratio because of lava viscosity
  • Explosive and non explosive eruptions
  • e.g Mt rainier: subduction zone volcano
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6
Q

What is the magma type for stratovolcanoes

A
  • most lavas that erupt on volcanoes like mt st helens are closer to rhyolitic and are about 65 to 75% silica
  • they erupt at about 900 degrees and are pretty stiff
  • high viscosity
  • high silica magma
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7
Q

What is the eruption type for stratovolcanoes

A

Plinian type eruption

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8
Q

Plinian type eruption

A
  • Lava is sticky and cooler
  • Bubbles can’t expand or escape easily
  • Explosive
  • starts with glowing pyroclastic flows
  • forms lava domes with steep sides
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9
Q

Characteristics of Plinian type eruptions

A
  • Ash and smoke column that can extend to stratosphere
  • large amounts of pumice
  • powerful gas blasts
  • large amounts of magma erupted
  • caldera formation possible
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10
Q

What are the three parts of a plinian column

A
  • lower kilometer or two is the gas thrust region
  • the next few kilometers is the convective region
  • the upper part is the umbrella region
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11
Q

What is calderas (ultra-plinian)

A
  • formed by very voluminous and explosive eruption
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12
Q

What are the key characteristics of calderas

A
  • caldera formation
  • large ejecta volumes
  • high energy release
  • massive plumes
  • magma is rhyolitic
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13
Q

What are cinder cones

A
  • smallest in size
  • e.g sunset crater, flagstaff , Arizona
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14
Q

Comparison of shield and stratovolcanoes

A

Shield volcanoes are far larger than stratovolcanoes

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15
Q

What are igneous rocks

A

-formed from the crystallization of magma
-extrusive: fine grained and quickly cooled
-intrusive: coarse grained and slowly cooled

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16
Q

Classification of Igneous rocks

A
  • mineral composition
  • grain size
  • texture
17
Q

Chemistry of silica

A
  • magmas range from about 50 to 75% silica
  • the more silica the stiffer the magma
  • the less silica, the more fluid the magma
    -“basalt” is lava that is about 50% silica
    -“rhyolite” is lava that is about 75% silica
18
Q

Chemistry of water

A
  • the more water, the more explosive especially for rhyolites
  • the effect of water on the stiffness of magma
  • high water content and high silica content makes magma erupt more explosively than a low water and low silica magma
19
Q

What are the three kinds of pyroclastic deposits

A
  1. Pyroclastic fall/ airfall
  2. Pyroclastic surges
  3. Pyroclastic flows
20
Q

Pyroclastic fall/airfall

A

fallout from the plinian column blankets the ground with a nearly uniform mantle of fine particles

21
Q

Pyroclastic surges

A

clouds of debris-laden gas jetting out of the volcano and racing over the countryside form layers of irregularly bedded ash and blocks

22
Q

Pyroclastic flow

A

dense slurries of debris racing down the slops of the volcano deposit, which concentrate in valleys