Lesson 5: Magma Generation and Igneous Rocks Flashcards

1
Q

Igneous rocks form when:

A

a melt solidifies at or below the Earth’s surface

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2
Q

The molten rock beneath the Earth’s surface is called ____.

A

Magma

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3
Q

The greatest amount of magma is created at

A

Divergent plate boundaries

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4
Q

How is magma generated at subduction zones?

A

Addition of volatiles

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5
Q

What type of magma contains the lowest amount of silica?

a. Felsic
b. Intermediate
c. Mafic
d. All magmas contain the same amount of silica

A

c. Mafic

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6
Q

_______ is a mafic extrusive igneous rock.

A

Basalt

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7
Q

A _________ is a concordant igneous rock body which runs parallel to pre-existing bedrock.

A

Sill

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8
Q

Magma rises toward the Earth’s surface because:

A

it is less dense than the surrounding rocks

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9
Q

Why are intrusive igneous rocks from a batholith generally coarser-grained than those from volcanic vents?

A

They cooled more slowly and thus had more time to grow

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10
Q

A _______ texture indicates two stages of cooling.

A

Porphyritic

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11
Q

Magma

A

molten/partially molten material found beneath the surface of the Earth

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12
Q

Lava

A

What we call magma that reaches the Earth’s surface.

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13
Q

Where does magma form in terms of plate tectonics?

A

Mostly at divergent plate boundaries
- mid-ocean ridges
- Continental rifts
Few at convergent plate boundaries
- subduction zones

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14
Q

What are the three ways to generate magma

A
  1. Decompression melting
  2. Addition of volatiles
  3. Addition of heat
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15
Q

What is decompression melting?

A

a rapid decrease in pressure that can cause the mantle to melt without an increase in temperature.

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16
Q

Where do we see decompression melting in terms of plate tectonics?

A

Divergent plate boundaries

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17
Q

What is addition of volatiles?

A

flux melting that occur due to chemical compounds (water) lowering the melting temperature of the rock

18
Q

Where do we see addition of volatiles in terms of plate tectonics?

A

Subduction zones

19
Q

What is addition of heat?

A

Inducing melting if temperature exceeds melting temperature

20
Q

Where do we see addition of heat in terms of plate tectonics?

A

Mantle plumes/hotspots

21
Q

How does magma evolve?

A
  1. Fractionation
  2. Assimilation
  3. Magma mixing
22
Q

What is fractionation?

A

The composition of magmas change as the magma cools

23
Q

What is assimilation?

A

The chemical evolution of magma is influenced by its reaction with, and digestion of the wall rock that it encounters during its ascent.

24
Q

What is magma mixing?

A

during the ascent of two chemically different magma bodies, the more buoyant mass may overtake the slower-rising body.

25
Compare intrusive and extrusive igneous rocks.
Intrusive: below the surface of the earth; slow cooling of magma Extrusive: on the surface of the earth; rapid cooling
26
What are the results of intrusive enviornments? (5)
1. Dike 2. Sill 3. Lacccolith 4. Plutons 5. Batholiths
27
What is the difference between a dike and a sill?
Dike is a vertical intrusion and cuts across sills Sill is a horizontal intrusion that form parallel to existing features instead of cutting through it
28
Describe laccoliths.
A mushroom-shaped intrusive body that has intruded between layers of sedimentary rock. Rising magma forces the overlying layers to rise into a dome
29
Describe plutons.
A blob-like igneous intrusion
30
Describe batholiths.
A huge blob-like igneous intrusion , formed as composite of many plutons
31
What are the different compositions of magma (igneous rocks)?
1. Felsic 2. Intermediate 3. Mafic
32
Describe the composition of felsic rocks
High in silica Low in iron and magnesium Lighter in color
33
Describe the composition of intermediate rocks
Lighter than felsics Average silica, iron, and magnesium
34
Describe the composition of mafic rocks
Low in silica High in iron and magnesium Darker in color than intermediate and felsic rocks.
35
What are the textures of igneous rocks?
1. Aphantic - fine-grained 2. Phaneritic- course-grained 3. Porphyritic - 2 sizes of crystals 4. Glassy 5. Pyroclastic - various fragments 6. Pegmatitic - exceptionally coarse-grained 7. Vesicular - bubbles
36
How are aphanitic textures characterized? (3)
No visible grains to the naked eye Rapid cooling of lava/magma May contain vesicles
37
How are phaneritic textures characterized? (3)
Crystals large enough to see with the naked eye Slow cooling of magma Intrusive origin
38
How are porphyritic textures characterized? (3)
Two distinct sizes of crystals (large and small) Minerals form at different temperatures and rates Usually indicates two stages of cooling Larger crystals are phenocrysts Finer crystals are ground-pass
39
How are glassy textures characterized?
Very rapid cooling of molten rock Extrusive origin
40
How are pyroclastic textures characterized? (2)
various fragments Extrusive origin Tuff if the largest fragments are less than 2.5 inches Volcanic breccia if fragments are larger than 2.5 inches
41
How are pegmatitic textures characterized?
Exceptionally coarse-grained Forms in the late stages of crystallization of granitic magmas
42
How is vesicular texture characterized?
Gas bubbles trapped in colling lava Extrusive origin