Igneous rock formation Flashcards

2.1-2.4 (74 cards)

1
Q

igneous rocks are formed from

A

the solidification of a melt

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2
Q

a melt is

A

molten rock

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3
Q

what’s the difference between lava and magma

A

magma below ground lava above ground

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4
Q

extrusive is

A

above ground

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5
Q

intrusive is

A

below ground

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6
Q

the crust and athenosphere are mostly in what state

A

solid

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7
Q

melts occur in what areas

A

localized

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8
Q

the earth has been cooling by

A

radiating heat out to space

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9
Q

the uppermost layer of the earth froze to form

A

the crust

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10
Q

how thick is the mantle

A

2800 km

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11
Q

temp increases or decreases with depth

A

increases

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12
Q

almost all solid rock is

A

peridotite

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13
Q

lithosphere thickness

A

100-150km

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14
Q

lithosphere is the

A

crust and upper mantle

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15
Q

athenosphere thickness

A

100-350km

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16
Q

athenosphere is a part of the

A

mantle

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17
Q

melts occur because of

A

decrease in pressure (decompression)

introduction of volatiles’ (flux)

heat transfer (heat transfer)

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18
Q

what happens in decompression melting

A

P decreases but T remains constant

temperature is high enough to melt rock at surface but pressure keeps them solid

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19
Q

how does pressure decrease to allow decompression melting

A

a volume of hot asthenosphere rises by a mantle plume or divergent plate boundaries

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20
Q

decompression melting creates M/F material

A

mafic

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21
Q

what kind of melt created hawaii

A

decompression

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22
Q

what happens in flux melting

A

volatiles help break chemical bonds, creating a melt

h2o or co2 mi with hot dry rock and help break the chemical bonds

this lowers the melting point of the rock

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23
Q

where does flux melting happen

A

subduction zones

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24
Q

flux melting creates M/F material

A

Felsic

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25
Heat transfer melting happens when
heat from magma melts adjacent rocks hot mantle rises up and brings heat with it this melts existing crustal rock that has a lower melting point
26
volcanic ars along plate boundaries come from what type of melting
heat transfer melting
27
melt composition is defined by
the proportion of different oxides SILICA SiO2 IRON OXIDE FeO and Fe2O3 MAGNESIUM OXIDE MgO
28
a dry melt has
no volatiles
29
a wet melt has
volatiles
30
What are the four major compositional groups of magma
felsic (silicic). 67-76% silica intermediate. 53-66% silica mafic. 46-52% silica ultramafic. 38-45% silica
31
felsic magma is what percent silica
67-76%
32
intermediate magma is what percent silica
53-66%
33
mafic magma is what percent silica
46-52%
34
ultramafic magma is what percent silica
38-45%
35
the four major compositional groups of magma is the percent
magma weight that is silica
36
the four major compositional groups of solid rock
are dependent on the proportion of silica relative to the combination of magnesium and iron oxide
37
diorite is _ I/S/M and _ F/M
igneous intermediate
38
rhyolite I/S/M and F/M
felsic igneous
39
gabbro I/S/M F/M
igneous mafic
40
why do melts vary
source rock dictates the initial melt composition
41
what is magma mixing
different magmas from different source rocks mix in the magma chamber changing the magma composition
42
what is assimilation / contamination
heat provided by magma partially melts wall rock the new magma the mixes with the original magma blocks of wall rock can dissolve in the original magma and that wall rock may chemically react with the magma changes the melts composition
43
what is partial melting
only a fraction of a source rock will melt at an achievable P and T some minerals melt at lower temps than others
44
in partial melting liquid magma
migrates away from the source rock before the entire rock can melt
45
partial melting produces a rock with
higher silica content
46
how does molten rock flow
melts migrate toward the surface due to their relatively low density
47
viscosity of molten rock depends on
temperature, volatile content, and silica percent content
48
Low viscosity magma is
Hotter more mafic has less volatiles
49
high viscosity magma is
cooler more felsic has more volatiles
50
mafic melts are ___ viscous than felsic melts. why
less more silica tetrahedra in felsic magma. they link together and don’t like to flow
51
how does a melt become a rock
it freezes migrates towards the surface loses heat to surrounding rock or erupts onto surface looses volatiles
52
the time a melt takes to cool depends on how
well insulated it is
53
wall rock is a ____insulator than water or air
better
54
melts cool ___ at the surface than underground
faster
55
the deeper magma is the hotter
the wall rock will be
56
a larger intrusion will cool _____ than a small intrusion at the same depth
slower
57
interaction with ground water can cool a melt _____ as water
faster as water can carry away heat but also introduce volatiles
58
thing lava flows cool ____ than thick ones
faster
59
lava immersed in water cools _____ than water immersed in air
faster
60
what is fractional crystallization
when a melt cools some minerals form earlier than others due to their melting points this results in sequential crystal formation
61
fractional crystallization creates a more
felsic melt
62
in crystal fractionalization the material that solidifies out is
more mafic olivine and calcium rich plagioclase
63
In bowens reaction series Low temperature corresponds to
last minerals to crystallize felsic materials
64
in bowens reaction series high the first minerals to crystallize
do so at high temperatures are ultramafic
65
What are tabular intrusions
Sills and Dikes underground solidified melts
66
Dikes are ___ to rock layers
perpendicular
67
Sills are ___ to rock layers
parralell
68
most sills result in a
change in land elevation of the surface
69
dikes spread in what way
sideways
70
what is a lacolith
when magma that cannot spread accumulates in a blister shaped intrusion
71
what is a pluton
a solid igneous intrusion
72
what is a batholith
a large solid igneous intrusion larger than 100km^2
73
what is a xenolith
a piece of rock in an igneous rock that is not derived from the original magma that showed up from elsewhere
74
what is unroofing
when intrusive igneous features are exposed over a long period of time