Magma Flashcards

1
Q

Adiabatic process

A

A thermodynamic process in which no heat enters or leaves the system during expansion or compression

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2
Q

Adiabatic cooling

A

It occurs when crust or mantle rises, undergoes expansion and the temperature falls, with no loss or gain of thermal energy

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3
Q

Adiabatic heating

A

It occurs when crust or mantle material descends and temperature rises as it contracts, with no loss or gain in thermal energy

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4
Q

Divergent plate margin

A

They occur where two plates are moving apart and magma is rising up between them

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5
Q

Partial melting

A

It occurs where some of the minerals in a rock melt to form a magma

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6
Q

Hot spots

A

an area of high heat flow above a mantle plume

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7
Q

Convergent plate margins

A

Are where two plates are colliding and magma is formed above a subduction zone or deep in the crust

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8
Q

Decompression melting

A

Decompression of the ultramafic peridotite causes partial melting and produces mafic magmas

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9
Q

How is magma produced at a convergent plate boundary?

A

Two plates collide, one is forced down, the geothermal gradient increases and partial melting results

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10
Q

Describe the process of flux melting

A

An oceanic plate is subducted, water in the rocks is carried down into the hot mantle. As the descending plate heats up, the water is released into the mantle rock above the plate. The water lowers the melting point of the minerals in the mantle rock and partial melting produces magma.

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11
Q

How is basaltic magma produced at an oceanic-oceanic crust?

A

The magma is mafic to intermediate in composition, initially the magma has only thin oceanic crust to rise through. If the magma rises quickly at shallow depths then it will be basalt.

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12
Q

How is intermediate to silicic magma produced at a continental- oceanic plate?

A

Magma rises through thicker silicic crust and this may partially melt due to increasing temps. Rising mafic magma has temp of 1000+ and silicic material melts at just 800. The resulting mixing gives intermediate to silicic magma.

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13
Q

How is silicic magma produced at a continental-continental plate margin?

A

Neither plate is subducted. High pressures and the mass of sediment (formed fold mountains) combine to force the base crust down. Partial melting at base produces silicic magma.

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14
Q

Magma

A

Molten rock which is beneath the earth’s surface

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15
Q

What determines the density of magma?

A

composition, pressure and temperature

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16
Q

What is the effect of Composition on the density of magma?

A

Mafic magma is rich in iron compared to silicic magma and this makes it more dense

17
Q

What is the effect of Pressure on density of magma?

A

An increase in pressure causes the magma to compress, which increase its density making it less buoyant

18
Q

What is the effect of Temperature on the density of magma?

A

An increase in temperature cause the magma to expand, which decreases its density making it more buoyant

19
Q

What is the viscosity of magma determined by?

A

Composition- mafic magma low viscosity as silica content is low vies versa
Temperature- increase in temp reduces viscosity

20
Q

How can magma recharge be detected?

A

Microgravity- sensors detect local changes in subsurface density from magma movement
Seismometer- tracks migration of small earthquakes from depth towards surface
Ground water heated- increase in pressure can cause crustal deformation and release of gases can also be measured

21
Q

What factors can prevent magma mixing?

A

density contrast
viscosity contrast
thermal barrier

22
Q

How are geysers produced?

A

Groundwater is heated at depths. Convection causes the gas-rich, super heated water to rise. As it rises, the pressure decreases and ‘flash’ boiling into steam result. The column of cooler water above it is thrust up explosively. The water then drains back into the ground

23
Q

How can gases exsolve from magma?

A

As magma rises to the surface, the reduction in pressure allows dissolved gases to exsolve. This happens because there is less magma above it pressing down. Bubbles can also form in a magma due to recharge and mixing.

24
Q

What can provide the earliest indication of magma moving?

A

Earthquakes

25
Q

What types of earthquakes indicate magma movement?

A

Short period- caused by the fracturing of brittle rock as magma forces its way upwards
Long period- indicate increased gas pressure in the magma chamber
Harmonic tremors- sustained vibrations, 0.5-5 Hz the result of magma vibrating in the vent as it moves upwards

26
Q

What does ground movement indicate and how is it measured?

A

Magma is moving up under the volcano. Rate of swelling is measured using tiltmeters and GPS accurate to 1 millimetre and can measure vertical and horizontal movement.

27
Q

What do gas emissions indicate?

A

As magma nears the surface and the confining pressure decreases, gas escapes. Changes in its compositions e.g. increases SiO2 levels can indicate the magma is nearing the surface.

28
Q

What can changes in ground water indicate?

A

Increased gas pressure will cause water levels to rise and suddenly drop before an eruption and the increased heat flow can reduce flow in aquifers. (borehole and well measurements)

29
Q

Extrusion

A

The extrusion of magma onto the earth’s surface where it forms a lava flow