Magma and Lava Flashcards

1
Q

molten rock material generated by partial melting in the earth’s crust

A

magma

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2
Q

magma that rises and erupts onto the surface of the earth

A

lava

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3
Q

liquid portion of the magma

A

melt

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4
Q

gaseous portion of the magma

A

volatiles

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5
Q

solid portion of the magma

A

crystals

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6
Q

magma will move to areas with _ pressure

A

less

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7
Q

magma moves _

A

upward

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8
Q

magma is naturally _ than the surrounding rock

A

less dense

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9
Q

depending on its composition and temperature, magma _

A

evolves

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10
Q

gases in magma tend to be _ in the melt portion at depth due to high _

A

dissolved; pressures

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11
Q

as SiO2 becomes concentrated, magma becomes more

A

viscous

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12
Q

the process where magma and lava loses its heat and solidifies

A

crystallization

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13
Q

rocks that formed as a result if crytallization

A

igneous rocks

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14
Q

igneous rocks that formed beneath the earth’s surface

A

plutonic/intrusive igneous rocks

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15
Q

igneous rocks that solidified at the earth’s surface

A

volcanic/extrusive igneous rocks

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16
Q

will tend to have larger crystal sizes

A

intrusive igneous rocks

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17
Q

will tend to have smaller crystal sizes

A

extrusive igneous rocks

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18
Q

the process where pre-existing rock is heated to the point of partially melting

A

partial melting

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19
Q

partial melting within the earth’s crust

A

anatexis

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20
Q

factors determining the type of magma

A
  1. composition, temperature, and depth of source rock
  2. % partial melting of source rock
  3. source rock’s previous melting history
  4. diversification processes after partial melting
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21
Q

3 origins of magma

A
  1. temperature increase
  2. decompression melting
  3. addition of volatiles
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22
Q

magma is generated through heat transfer from a hot body until the melting point of the minerals present is reached

A

temperature increase

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23
Q

the increase of temperature with depth

A

geothermal gradient

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24
Q

the result of a decrease in pressure in the system

A

decompression/adiabatic melting

25
agents that reduce the melting point of rocks
flux
26
the presence of flux weakening the bonds between atoms, making it melt
addition of volatiles
27
crystallization along the walls of a magma chamber and crystals preferentially form and adhere to the edges
marginal accretion
28
fractionation processes that occur when crystals develop with significantly different densities than the magma
gravitational separation
29
dense minerals sink and accumulate at the bottom of the magma body
crystal settling
30
light minerals float and accumulate at the top of the magma body
crystal flotation
31
magma body is subjected to stress, squeezing out the melt and leaving behind crystals
filter pressing
32
liquids and crystals are segregated due to velocity, density, and temperature
convective flow segregation
33
two or more dissimilar magmas coexist but retain their distinctive characteristics
magma mingling
34
mixing of two or more magmas, with their individual characteristics no longer recognizable
magma mixing
35
development of more than one type of igneous rock from a parent magma
magmatic differentiation
36
the incorporation and digestion of foreign material into the magma body
magmatic assimilation
37
inclusions in magmatic bodies
xenolith
38
a body of magma
pluton
39
rocks that break away from the surrounding rock and assimilate into the pluton
stopes
40
one parent magma produces two distinct daughter magma
liquid fractionation
41
selective diffusion of ions in the magma due to compositional, thermal, or density gradients
differential diffusion
42
separation of magma into two or more liquid phases
liquid immiscibility/liquid-liquid fractionation
43
genetically related magmas that evolved from a parent magma
magma series/magma suite
44
decrease in Fe and Mg with increasing silica and alkali concentrations
calc-alkaline magma
45
where do calc-alkaline magmas occur
convergent margin environments with volcanic arcs and subduction zones
46
enrichment in Fe, low to moderate SiO2 concentrations, depleted MgO and CaO
tholeiitic magma
47
where do tholeiitic magmas occur?
extensional environments such as ocean ridges and continental rifts. also in intraplate settings with immature arcs and volcanic arc crusts
48
highly enriched in Na2O and/or K2O and contains extremely diverse SiO2 contents
alkaline magmas
49
high concentration of silicic and basic rocks, with little intermediate rocks
bimodal magma
50
bimodal magma suites
basic from mantle; silicic from crust
51
bivariate diagrams showing the relative relationship of oxide compounds
Harker Diagrams
52
as silica increases in a harker diagram
K2O and Na2O also increase
53
most abundant element in the earth’s crust
OSAICSPM
54
5 types of magma
1. ultramafic 2. mafic 3. intermediate 4. dacitic 5. felsic
55
magma that is <45% SiO2, >1,200°C, very fluid, very low gas content
ultramafic magma
56
magma that is 45-52% SiO2, 1,200-1,000°C, fluid, low gas content
mafic magma
57
magma that is 52-63% SiO2, 1,000-800°C, intermediate viscosity and gas content
intermediate magma
58
magma that is 63-68% SiO2
dacitic magma
59
magma that is 68-77% SiO2, 800°C-600°C, highly viscous, very gaseous
felsic magma