Plate Boundaries And Igneous Processes Flashcards

1
Q

What creates the rheid asthenosphere?

A

Partial melting within the mantle. Not enough to classify it as a liquid. Pressure allows material to remain solid due to particle compaction

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

What is geothermal gradient?

A

The change in temperature with depth (C/Km)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

What are convection currents?

A

They help with rock movement within the mantle. Happens because of heat transfer from the core to the lower mantle.
Rock gets hotter, expands (less dense) and rises. Here it gets cooler, contracts (more dense) then sinks.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

What is adiabatic heating?

A

Areas become hotter, despite no change in energy.
Contraction = heat energy shared over smaller volume (no gained energy). So the rock appears hotter

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

What is adiabatic cooling?

A

Expansion = heat energy shared over larger volume (no energy loss). Rock appears to cool

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

What is an adiabatic system?

A

No heat energy enters or leaves the system.
Happens in the mantle.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

How does partial melting happen?

A

Rising magma experiences a decrease in pressure = expansion = reduction in temp with the loss of heat as energy used to move particles apart. Melting occurs because melting point decreases as pressure decreases

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

What are the 6 causes for magma formation at Earth’s surface?

A

Divergent boundary
Hotspots
Subduction zones
Oceanic-oceanic boundary
Continental-oceanic boundary
Continental-Continental boundary

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

How is magma formed at divergent plates boundaries?

A

Mainly seen as MORs (e.g. MAR).
Mainly due to decompression melting by pressure release. As it stretches and thins, asthenosphere upwell and pressure reduced (lower MP).
Partial melting of ultramafic peridotite produces mafic magma.
Basalts are produced, usually as pillow lava. Dolerite sills and dykes below

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

How is magma formed at hotspots?

A

Evidence of mantle plumes.
Magma rises from deep - decompression melting. Plumes carry heat upward in narrow rising columns of hot material, which spreads out when plume head reaches lithosphere.
Lower pressure = decompression + partial melting of mantle peridotite. Forming enormous volcanoes of basaltic lava

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

How is magma formed at subduction zones

A

Oceanic crust present.
Magma production here must occur under ocean. Some water dragged down during subduction. Presence of water lowers melting point of minerals. This called flux melting

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

How is magma formed at oceanic-oceanic boundaries?

A

Subduction causes volcanoes with usually mafic magma.
Partial melting of oceanic crust through ultramafic mantle

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

How is magma formed at a continental-oceanic boundary?

A

subduction causes volcanoes with intermediate magma.
Partial melting of oceanic crust through ultramafic mantle through silicic continental crust

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

How does magma form at continental-continental boundaries?

A

No subduction
Increased pressure = increased temps.
Some melting deep in mountains.
Silicic magma (viscous) in the base, so cools slowly (batholith).
Thickening on crust –> fold mountains

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

What controls the density of magma?

A

Composition. E.g. mafic > silicic (due to metals).
Temperatures. High temps = expansion if possible = reduction in density.
Pressure. Increase in pressure = increase density

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

What controls the viscosity of magma?

A

Composition.
Bonds. Silicic magma = more tetrahedra bonds = more viscous.
Temperature increase = reduced viscosity.
Increased pressure = increased viscosity.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
17
Q

What is magma recharging?

A

After an eruption, depleted magma chamber. More magma rises from deeper and ‘recharges’ the chamber

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
18
Q

What is the evidence of magma recharging?

A

Seismic tomography, release of gases.
New magma is hotter than any left over magma (deeper) and different composition.
Different composition could trigger eruption.
Old magma may have started to crystallise (floating crystals).
Sometimes zoned crystals.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
19
Q

What factors prevent magma mixing?

A

Different compositions: different densities. Tend to have one overlying the other (buoyant).

Different viscosities: more viscous = harder to mix

Different temps: where they meet, we get a thermal barrier

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
20
Q

What is a thermal barrier?

A

Where two magmas meet (different temps)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
21
Q

What does groundwater do for magma?

A

Groundwater percolates downwards –> becomes superheated if meets magma. Forms geysers and hot springs.
Flash boiling as pressure drops when water rises (release gases).
This then repeats

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
22
Q

What does exsolve mean?

A

To come out of solution

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
23
Q

What are volatiles?

A

Substances which are unstable at surface conditions

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
24
Q

What is the exsolution of volatiles in magma?

A

Magma rises –> pressure drops –> gases exsolve.

Formation of bubbles = more space (pressure).
Can trigger eruption

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
25
Q

What is an igneous intrusion?

A

Magma that has come up but never reached the surface, cooling below

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
26
Q

What is concordant?

A

Intrusions parallel to existing beds

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
27
Q

What is discordant?

A

Intrusions perpendicular to existing beds (cuts across)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
28
Q

What is country rock?

A

Rock that was already present before an intrusion

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
29
Q

What is a dyke? (basic description)

A

Discordant minor sheet-like intrusion

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
30
Q

What is a sill? (basic description)

A

Concordant minor sheet-like intrusion

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
31
Q

Sills and dykes are examples of what type of intrusion?

A

Minor igneous intrusions

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
32
Q

What are the two types of dyke which appear the same at first?

A

Ring dykes and cone sheets

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
33
Q

How are ring dykes formed?

A

Magma rises and pushes overlying rock into dome shape.
Magma retreats (pressure decrease), leaving void below the dome.
This then collapses and fractures the rock around it. Magma enters these circular fractures.
Then eroded to form a ring shape

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
34
Q

How are cone sheets formed?

A

Magma rises and pushes upwards, meeting a barrier –> accumulates and pressure builds. This means it moves upwards and outwards.
Forces its way upwards and out, forming a cone shape –> looking like a ring from the surface once eroded

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
35
Q

Ring dykes and cone sheets are often confused, why?

A

Both look circular in map view

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
36
Q

What is a volcanic plug?

A

A crystallised magma that fills the vent of a volcano.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
37
Q

What is a diapir?

A

Any blob of rising magma (no matter the size).
a.k.a
A body of low density material that pierces and rises up through overlying material of higher density

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
38
Q

What is meant by ‘contact’?

A

Where the igneous rock meets the country rock

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
39
Q

What is a baked margin?

A

Area of country rock that has been heated by the intrusion. It has undergone contact metamorphism as it has been altered by heat

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
40
Q

What is a chilled margin?

A

Part of an intrusion that cools rapidly due to contact with cold country rock. Has a finer crystal structure that remaining intrusion

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
41
Q

Plutons and batholiths are examples of what type of igneous intrusion?

A

Major igneous intrusions

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
42
Q

What is a pluton?

A

A large igneous intrusion. Smaller than batholiths

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
43
Q

What is a batholith?

A

A large igneous intrusion.
Bigger than plutons, may be an aggregate of plutons.
>100 km^2

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
44
Q

What are the features of a batholith?

A

Most are discordant.
Usually circular at surface and spherical underground.
Coarse crystals.
Usually granite, sometimes diorite

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
45
Q

What is the Cornubian batholith?

A

Batholith under Devon and Cornwall. Formed in Variscan orogen in late Paleozoic
235km long

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
46
Q

What is a metamorphic aureole?

A

A large area around a batholith where country rock has been metamorphosed.
Primary force is heat (contact)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
47
Q

How does a batholith affect shale country rock?

A

Large baked margin.
Close to intrusion = hornfels
Little further = Andalusite
Farthest = spotted rock

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
48
Q

Is hornfels a rock or a mineral?

49
Q

Is andalusite a rock or a mineral?

50
Q

How do granite magmas form?

A

Form at convergent plate boundaries. Deep in the core of mountains.

51
Q

How do granitic magmas form at continental-continental boundaries?

A

No subduction, high pressure causes some melting

52
Q

How do granitic magmas form at oceanic-continental boundaries?

A

Oceanic subduction melts. Melt rises.
Silicic minerals have lower melting point so rise first

53
Q

What is partial melting?

A

When only a portion of a rock is melted. Lower temperature minerals melt, e.g. quartz

54
Q

What is stoping?

A

The process that accommodates the magma as it moves upwards. Mechanical fracturing of the surrounding rock.

(Kinda like plucking in geography)

55
Q

What are xenoliths?

A

Clasts or blocks of pre-exiting rock contained within an igneous rock if it doesn’t melt

56
Q

What is assimilation?

A

The melting process that incorporates blocks of country rock, fed by stoping, into the magma

57
Q

What can assimilation do to a magma?

A

Change the overall composition of the magma.

58
Q

What are the three types of earthquakes caused by moving magma?

A

Short-period earthquakes.
Long-period earthquakes.
Harmonic tremors.

All small in comparison to large tectonic earthquakes

59
Q

What are short period earthquakes?

A

Short amount of ground movement. <1s.
Fracturing of brittle rocks as magma rises upwards (stoping)

60
Q

What are long period earthquakes?

A

Longer amount of ground movement. 1-5s
Caused by increased gas pressure in a magma chamber

61
Q

What are harmonic tremors?

A

Magma vibrating in the vent of the volcano as it moves upwards.
Longer rumblings, lasts a while

62
Q

What is a tiltmeter?

A

Designed to measure very small changes in vertical level

63
Q

What is GPS?

A

Global Positioning System.
The radio navigation system that allows determination of exact position

64
Q

What are fumaroles?

A

Openings in or near a volcano, through which hot gases emerge

65
Q

What is the evidence for the location of a magma chamber? (5)

A

Seismic tomography.
Ground movement.
Fumaroles.
Changes in water table.
Orientation of dykes

66
Q

How does seismic tomography provide evidence for the location of a magma chamber?

A

Both P+S waves. Intrusions result in low velocity zones.
Molten materials, no S waves.
P+S waves will travel faster around the chamber

67
Q

How does ground movement provide evidence for the location of a magma chamber?

A

Measures using tiltmeters and GPS that accurately measure both vertical and horizontal movements to the accuracy of 1mm.

68
Q

How do fumaroles provide evidence for the location of a magma chamber?

A

Fumaroles are gas emissions near the volcano. CO2 and SO2 produced

69
Q

How do changes in the water table provide evidence for the location of a magma chamber?

A

Water levels can be monitored using wells. If levels rise, it means more gases exsolved.
Sudden drop = imminent eruption

70
Q

How does the orientation of dykes provide evidence for the location of a magma chamber?

A

Dykes may change distance and position due to increased gas levels below the surface.
This can be used as an indicator of the stress field in volcanic areas and to identify volcanic centres

71
Q

What are rose diagrams also known as?

A

Circular graphs or stereonets

72
Q

For orientations on rose diagrams, how do we plot the data?

A

Tally up the data. Add up opposite tallies. Plot.

73
Q

For directions on rose diagrams, how do we plot the data?

A

Tally up the data. Plot.
No addition required

74
Q

What are the similarities between sills and lava flows? (3)

A

Igneous layers of rock between earlier rock.
May have xenoliths and phenocrysts.
Baked and chilled margin on lower contact

75
Q

What are the differences between sills and lava flows? (6)

A

Sill = 2 bakes margin. Lava flow = 1.
Lava flow may be uneven at top.
Sill = xenoliths top+bottom. Lava flow = xenoliths only bottom.
Lava flow = fine or glassy. Sill = fine or medium.
Lava flow = may have vesicles. Sill none.
Lava flow = reddened surface (oxidation of iron). Sill none.

76
Q

At a molecular level, why are silicic magmas more viscous than basaltic magmas?

A

More silica tetrahedra.
More bridging oxygens (bonds).
Form chains, double chains, sheets, and frameworks

77
Q

How does the temperature of lava impact its viscosity?

A

Increase temps = lower viscosity.
Energy breaks some of the bonds (depolymerisation).
Also the same the other way around.

78
Q

How does the pressure of lavas impact their viscosity?

A

Increase pressure = increase viscosity.
Atoms more able to form bonds (polymerisation)

79
Q

How does lava composition impact their viscosity?

A

Higher amount of silica tetrahedra bonds. More silica available = more bonds likely.
hence silicic more viscous

80
Q

How do volatiles (water) impact lava viscosity?

A

Presence of water = lower viscosity.
Water breaking bridging oxygen bonds (depolymerisation).
Instead hydrogen ions are reacting with bridging oxygens

81
Q

How do volatiles (CO2) impact lava viscosity?

A

Presence of CO2 = increased viscosity.
CO2 is a polymer, increases polymerisation.
CO2 connects to non-bridged oxygens and bridges to the next.
CO2 bridges them

82
Q

What is meant by the term ‘melt’?

A

The name given to magma or lava in the liquid phase

83
Q

What is aa?

A

Lava flows with a rough, blocky, jagged surface

84
Q

What is pahoehoe?

A

Lava flows with a smooth or ropy surface

85
Q

Which of aa or pahoehoe is more viscous?

86
Q

What is scoria?

A

A volcanic rock that is usually mafic but can be intermediate in composition

87
Q

What is a pyroclast?

A

An individual fragment ejected during an eruption

88
Q

What is a nuee ardente?

A

Gaseous pyroclastic cloud of magma droplets and ash

89
Q

When a nuee ardente deposit cools and solidifies, what rock does it become?

A

Ignimbrite rock

90
Q

What is a pyroclastic flow?

A

Hot mixture of pyroclastic material and has

91
Q

What is included in pyroclastic material?

A

bombs and blocks, lapilli, tuff, pumice, ash

92
Q

What is lapilli?

A

Particles between 2mm and 64 mm in size

93
Q

What rock does lapilli form?

A

Lapilli tuff

94
Q

What is ash?

A

Smallest particles less than 2 mm in size. form tuff

95
Q

What are volcanic bombs and blocks?

A

produced by the coarsest particles over 64 mm in size

96
Q

What pyroclastic rock is formed from volcanic bombs and blocks?

A

Agglomerate

97
Q

What are the features of shield volcanoes?

A

Gentle slope <10°
Almost entirely thin basalt.
Low viscosity.
Roughly circular
Little pyroclastic material
Frequent or constant eruption

98
Q

How many of Earth’s individual volcanoes are composite volcanoes?

99
Q

What are the features of a composite volcano?

A

Alternating strata (lava & pyroclastic deposits).
Typically conical.
Eruption can last hours, days or years.
Viscous.
Wide range of compositions (typically higher silica)

100
Q

What is the eruptive cycle of volcanoes?

A

Period of no activity. Magma builds, gas pressures.

Pressure builds, explodes. Gas rich pyroclastic material escapes.

Lava reaches surface and forms layer. gas pressure decreases

101
Q

What are the features of fissure eruptions?

A

Huge quantities of fluid lava spreads out over large area.
Lots of volcanic gas (SO2).
Elongated breaks in the crust

102
Q

What is columnar jointing?

A

Hexagonal columns formed from large lava flows cooling

103
Q

How does columnar jointing form?

A

Lava flows >3mm thick.
Inside cools slowly (weeks, months)
Outside cools in hours or days.
Cooling at centres in all directions.
Contraction causes tension cracks (hexagonal)

104
Q

What is the other name for submarine eruptions?

A

Pillow lavas

105
Q

How do pillow lavas form?

A

Lava erupts underwater, outer skin cools rapidly while inside is molten.
Pressure of more lava causes breaks to form new pillows.

106
Q

How can pillow lavas be identified?

A

Rounded shape.
Vesicles may be present towards outer upper edge of pillows.
Spaces between pillows may be filled with fine, glassy materials

107
Q

What are the features of a caldera?

A

Large 1-20km crater circular. caused by violent eruptions, followed by the collapse of the top of the volcanic cone

108
Q

What are the three stages of formation of calderas?

A

1) series of violent eruptions of pyro flows, ash, pumice. Removes large volumes of magma.

2) Magma chamber starts to empty. top starts to collapse down. This compresses magma, making eruptions more violent.

3) Entire cone collapses.

109
Q

What other hazard might the collapse of the cone of a caldera cause?

A

Tsunamis if the volcano is coastal, e.g. Krakatoa

110
Q

What kind of gases do volcanoes release/exsolve?

A

CO2 (12%)
SO2 (7%)
N (7%)
^add to 25%
H2O vapour (70%)

111
Q

What are the potential hazards caused by eruptions?

A

Pyroclastic flow,
lahars (mudflows)
Tephra (ash,bombs)
Lava
Earthquakes, tsunamis
Floods

112
Q

What is meant by ‘effusive’?

A

Describes the fluid, non-explosive, basaltic lava. Often constant eruptions

113
Q

What is the Volcanic explosivity index?

A

A measure of the explosiveness of eruptions. Allows volcanoes to be compared. 0-8 scale

114
Q

What are hawaiian eruptions?

A

Large amounts of fluid basaltic lava from which gases escape, but few pyroclasts

115
Q

What are strombolian eruptions?

A

More explosive with less fluid lava. Regular explosions of gas and pyroclastic material

116
Q

What are vulcanian eruptions?

A

Violent with viscous andesitic lava and large quantities of pyroclastic material from large explosions

117
Q

What are plinian eruptions?

A

Extremely explosive with viscous gas filled andesitic and rhyolitic lava and high volumes of pyroclastic material blasted out

118
Q

What is isopachyte?

A

A line joining points of equal thickness of a deposit such as ash. The maps may be called isopach maps