Chapter 5 Flashcards

1
Q

igneous rock

A

begins in the lower crust or upper mantle melts to form magma, which rises up through the crust

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2
Q

extrusive igneous rock

A

forms from solidified lava or ash

it comes out onto the surface

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3
Q

intrusive igneous rock

A

magma that never reaches the surface and solidifies underground

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4
Q

shapes of intrusive igneous rock

A

plutons: massive blobs
batholiths: the largest of the plutons
dikes: thin sheet cutting across layering in the wall rock
sills: form parallel to the layers of wall rock

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5
Q

determining igneous rock types

A

grain size
color
specific gravity

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6
Q

texture

A

the size, shape, and arrangement of its grain

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7
Q

crystalline

A

specimens composed of interlocking grains

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8
Q

glasses

A

rocks that are shiny and contain no grains

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9
Q

porous

A

rocks that have sponge-like masses

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10
Q

fragmented

A

rocks that appear to have pieces cemented together

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11
Q

cooling rate

A

most important factor controlling grain size - the slower a magma cools, the more ions have to migrate to crystal seeds; the faster it cools the less time there is and the smaller the grains will be

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12
Q

viscosity

A

resistance of material to flow

the less viscous the more fluid the easier it is for ions to migrate and larger crystals can become

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13
Q

Four Major Compositional groups of Igneous Rocks

A
  1. ) Felsic
  2. ) Intermediate
  3. ) Mafic
  4. ) Ultramfic
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14
Q

Felsic

A

ex: feldspar and silica and quartz
have the most silica and the least iron and magnesium
light colored and have low specific gravities

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15
Q

Intermediate

A

chemical compositions, colors, specific gravities, and mineral assemblages between those of felsic and mafic rocks

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16
Q

Mafic

A

have much less silica, potassium, and sodium than felsic rocks but much more calcium, iron, and magnesium
dark green or black and have higher specific gravities

17
Q

Ultramafic

A

least amount and the most iron and magnesium but very little aluminum, potassium, sodium, or calcium
very dark and have highest specific gravities of igneous rocks

18
Q

Decompression melting

A

stretching of the lithosphere at a divergent plate boundary (ocean ridge) or continental rift lowers the confining pressure on the asthenosphere and allows the heat in the rocks to overcome the bonds and cause melting
requires no additional input of heat

19
Q

Flux melting

A

water and other volatiles are released from these minerals when the subducted plate reaches critical depth and risse into the asthenosphere where they help melt it
no additional heat required

20
Q

shield volcanoes

A

made mostly of highly fluid lava
broad structures with gentle slopes
largest types of volcanoes

21
Q

Lava domes

A

much smaller than shield volcanoes with extremely viscous lava
steeper slopes than shield volcanoes

22
Q

Cinder cones

A

made mostly from relatively fine-grained pyroclastic material and form above
smaller than shield volcanoes and moderate slopes

23
Q

stratovolcanoes

A

made of large amounts of both lava and pyroclastic material
have the steepest slopes
commonly found in subduction zones
explosive eruptions

24
Q

lahars

A

mudslides made of volcanic ash, water, and debris