Lesson 4: Igneous Rocks Flashcards

1
Q

Formed by cooling and crystallization of magma

A

Igneous Rock

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

Molten rock underground

A

Magma

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

forms within crust/blow ground

surface; takes centuries – millions of years to form

A

Intrusive Igneous Rock

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

forms above ground surface;

takes seconds to years to form

A

Extrusive Igneous Rock

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

Molten rock above ground surface

A

Lava

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

Volcanic Rocks

A

Extrusive

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

Plutonic Rocks

A

Intrusive

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

Magma from _____melting is the source of nearly all Igneous rocks

A

Partial

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

Only certain parts of the rock melt (not all of

it) due to each component of a rock having different melting points

A

Partial Melting

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

determines how far the

reaction process reaches (based on available silica) and what kind of rock it will harden into.

A

Magma Composition

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

has the most SiO2

A

Felsic

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

45%-55% SiO2

A

Mafic

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

SiO2 < 45%

A

Ultramafic

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

result to mafic rocks

A

Mafic magma

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

mafic rocks will have different names depending on

where it ________

A

Crystallized

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

Has low viscosity associated with (relatively) calmer

volcanic eruptions

A

Mafic magma

17
Q

fluid’s resistance to flow

A

viscosity

18
Q

show how minerals are formed as magma

cools and becomes igneous rocks.

A

Bowen’s reaction series

19
Q

branches of Bowen’s reaction series

A

Discontinuous, continuous

20
Q

Plagioclase Feldspar will have calcium rich core

and then covered with more sodium-rich Plagioclase Feldspar shell/cover.

A

Zoning

21
Q

magma formed at ~750-800°C (assuming there are still silica left)

A

Quartz, Potassium feldspar, muscovite mica

22
Q

Large part of the remaining Silica goes into

A

calcium-rich Plagioclase

23
Q

Remaining part of Silica (if there are any) transforms Olivine to

A

Pyroxene

24
Q

Mafic magma typically cools into

A

Gabbro (intusive) or basalt (extrusive)

25
Q

Intermediate magma usually cools into

A

Diorite (intrusive form) or

Andesite (extrusive form)

26
Q

Felsic magma do not have to be so hot to maintain liquid form so they crystallize/harden at

A

lower temperatures

27
Q

A felsic magam that cools starts at

A

Pyroxene and Plagioclase

28
Q

Felsic magma commonly cools into

A

Granite (intrusive form) or

Rhyolite (extrusive form)

29
Q

the _____ separates the ferromagnesian silicates on the upper right
from the non-ferromagnesian silicates on the lower left.

A

red line

30
Q

Mafic rocks tend to be darker than felsic rocks due to the

A

ferromagnesian silicates

31
Q

• Mafic rocks can have _______ ferromagnesian silicates

A

50-100%

32
Q

Intrusive rocks tend to be _______. This is because they ________under the ground, the crystals ______

A

rougher, cool slower, grow

33
Q

crystallization of minerals in certain

sequence, and separation of the ones already formed.

A

Fractional Crystallization

34
Q

settling of crystals already formed to the bottom

of a magma chamber

A

Crystal settling

35
Q

have exposed area at the surface of more than 100

km2

A

batholiths

36
Q

a pluton that is sheet-like and is parallel to the existing

layering of the underground materials.

A

sill

37
Q

similar to sill but perpendicular to the existing layering

of underground materials.

A

dyke

38
Q

sill that has expanded and pushed the rock above it.

A

LACCOLITH

39
Q

a “cylindrical” conduit (may have any cross-sectional shape)

that serves to allow movement of magma from one point to another.

A

PIPE