Volcanoes 2 Flashcards

1
Q

What is the most important factor that determines igneous texture (___)?

A

Cooling rate
(grain size)

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2
Q

Extrusive or volcanic rocks cool ___ and are ___ grained

A

fast (days-months)
fine

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3
Q

Intrusive or plutonic rocks cool ____ and are ____

A

slow (100+ years)
coarser

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4
Q

Example of extrusive rock

A
  • Basalt, lots of gas bubbles
  • rhyolite
  • andesite
  • dacite
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5
Q

Example of intrusive rock

A

granite

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6
Q

Felsic rocks examples and colour

A

light color
ex/ granite, rhyolite

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7
Q

Mafic rocks examples and colour

A

dark color
ex/ basalt, gabbro

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8
Q

rhyolite is an ___ ___ rock

A

extrusive felsic

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9
Q

basalt is an ____ ___ rock

A

extrusive mafic

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10
Q

granite is an ___ ___ rock

A

intrusive felsic

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11
Q

what is obsidian?

A

volcanic glass

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12
Q

define glass

A

a non-crystalline or amorphous solid formed by quenching a melt
-> cools so fast that regular crystal lattice cannot form

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13
Q

Temperature of mafic vs felsic rocks

A

mafic hot (1200-1400˚C)
felsic cool (600-900˚C)

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14
Q

Water content of mafic vs felsic rocks

A

mafic low
felsic high

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15
Q

viscosity of mafic vs felsic rocks

A

mafic low (runny)
felsic high (sticky)

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16
Q

Explosivity of mafic vs felsic rocks

A

mafic non explosive (lava)
felsic explosive (pyroclastic)

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17
Q

Silica content of mafic vs felsic rocks

A

mafic less (~50%)
felsic more (~70%)

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18
Q

Example of intermediate rocks (between mafic and felsic)

A

andesite
dacite

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19
Q

what are the two critical magma properties

A

density and viscosity

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20
Q

Magma density

A

== buoyancy

2.5 - 3.3 g/cm^3

21
Q

Magma melt travels up because

A

they are less dense

22
Q

define viscosity

A

resistance to flow
controls flow, deformation, eruption

23
Q

Viscosity is strongly dependent on ____

A

temperature

24
Q

magma viscosity depends on ____

A
  • temperature
  • gas content
  • crystal content
25
What composition affects viscosity the most?
H2O :D
26
in a magma chamber containing rhyolite on top of basalt, which erupts first?
rhyolite erupts first, then basalt then the basalt moves faster and overruns rhyolite (break thru)
27
high viscosity basalt lavas are called
A'a (blocky)
28
Cooling ___ melt viscosity, which increases ____
increases crystallization
29
Lowest viscosity basalt lavas are called
pahoehoe (flows)
30
A crystal rich lava will have ___ viscosity and ___ temperature than crystal poor lava of the same composition
higher viscosity lower temperature
31
the loss of dissolved volatiles ____ viscosity
increases volatiles include dissolved gasses, and when magma rises -> lower P -> less solubility -> bubbles!
32
Where do volcanoes occur?
plate boundaries hot spots
33
Example of a famous area of volcanism
pacific ring of fire also Hawaii is a hot spot
34
At which plate boundaries do volcanoes occur?
convergent and divergent
35
Continental volcanic arcs happen as a result of what type of volcanoes?
subduction volcanoes
36
Describe how continental volcanic arcs form
volatiles and partial melt from subducted ocean plate = mafic magma felsic magma as it is stored in continental crust felsic/intermediate as it is contaminated by stuff
37
plates involved in our local continental volcanic arc
Cascadia subduction zone Juan de fuca plate subducting under North American plate
38
Describe how oceanic volcanic arcs form
volatiles and melt rising from subducted ocean plate = mafic magma mafic/intermediate magmas and lavas
39
The most voluminous volcanism on earth are from
mid ocean ridges - not exposed at surface except in Iceland
40
Mafic magma from a plume of hot mantle: mantle plumes are ____ & ____
stationary and pulsatory
41
Volcanic settings: Divergent boundaries
continental crust : East African Rift Zone btwn oceanic plates: Mid-Atlantic Ridge
42
Volcanic Settings: Convergent boundaries
Oceanic-continental: Cascades Oceanic-oceanic: Aleutian islands
43
Volcanic Settings: Hot spots
under continental crust: Yellowstone under oceanic crust: Hawaii
44
Melting mechanisms: Divergent Boundaries
mantle stuff rises in a dike, pressure decrease - mafic magma may melt overlying crust
45
Melting mechanisms: Convergent Boundaries
hydration of mantle by subjecting plate - mafic magma melts overlying crust
46
Melting mechanisms: Hot Spots
mantle stuff rises in cylindrical plume, pressure decrease - mafic magma melts overlying crust
47
Type of magma associated with oceanic plates/crust
mafic
48
Type of magma associated with continental crust
mafic-int-felsic (mostly felsic)