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

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.

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

24
Q

Mafic magma typically cools into

A

Gabbro (intusive) or basalt (extrusive)

25
Intermediate magma usually cools into
Diorite (intrusive form) or | Andesite (extrusive form)
26
Felsic magma do not have to be so hot to maintain liquid form so they crystallize/harden at
lower temperatures
27
A felsic magam that cools starts at
Pyroxene and Plagioclase
28
Felsic magma commonly cools into
Granite (intrusive form) or | Rhyolite (extrusive form)
29
the _____ separates the ferromagnesian silicates on the upper right from the non-ferromagnesian silicates on the lower left.
red line
30
Mafic rocks tend to be darker than felsic rocks due to the
ferromagnesian silicates
31
• Mafic rocks can have _______ ferromagnesian silicates
50-100%
32
Intrusive rocks tend to be _______. This is because they ________under the ground, the crystals ______
rougher, cool slower, grow
33
crystallization of minerals in certain | sequence, and separation of the ones already formed.
Fractional Crystallization
34
settling of crystals already formed to the bottom | of a magma chamber
Crystal settling
35
have exposed area at the surface of more than 100 | km2
batholiths
36
a pluton that is sheet-like and is parallel to the existing | layering of the underground materials.
sill
37
similar to sill but perpendicular to the existing layering | of underground materials.
dyke
38
sill that has expanded and pushed the rock above it.
LACCOLITH
39
a “cylindrical” conduit (may have any cross-sectional shape) | that serves to allow movement of magma from one point to another.
PIPE