Lesson 4.2 Flashcards

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1
Q

are formed from
solidification of magma or lava
which flows out from depth.

A

Igneous rocks

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2
Q

are the components of almost
all types of igneous rocks.

A

Minerals such as quartz, feldspar,
pyroxene, olivine, amphibole, and
mica

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3
Q

Igneous rocks are
characterized by

A

intergrowth of crystals and/or
volcanic glass.

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4
Q

Crystal size is _
proportional to the cooling
rate of magma.

A

directly

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5
Q

are formed
deep underground,

A

Big crystals

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6
Q

are formed
near the surface.

A

smaller crystals

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7
Q

forms
when magma or volcanic fragments
erupt and solidify on Earth’s surface
which results in very fine-grained
rock with very small crystals that
could not be seen through naked
eye.

also known as a volcanic rock

A

extrusive igneous rock

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8
Q

forms when magma
crystallizes within the crust
and is composed of
medium to coarse grains. It
is also known as a plutonic
rock.

A

intrusive igneous rock

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9
Q

Igneous rocks can be named using the binary system which
is mainly based on its

A

texture
composition

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10
Q

It is directly proportional to the cooling rate of magma. This means that when the crystals are big, it denotes that the rock is formed deep underground
since the magma has a longer trip to the surface giving it longer time to cool down
at a very slow rate. On the other hand, magma cools quickly (fast cooling) near the
surface that causes formation of smaller crystals since it is given few time to form.

A
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11
Q

Crystals form when magma are cooled. A general model is created to show the
progression of silicate crystallization at specific temperature. It is called

A

Bowen’s
reaction series

which is developed by petrologist Norman L. Bowen

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12
Q

2 branchs of bowen’s reaction series

A

discontinuous branch
continuous branch

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13
Q

discontinuous branch

A

olivine
pyroxene
amphibole
biotite mica

old people are boring

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14
Q

continuous branch

A

calcium rich plagioclase feldspar

to sodium rich plagioclase feldspar

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15
Q

3 textures of extrusive igneous rock

A

smooth
full of holes
wit hlarge crystals embedded in a fine ground mass

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16
Q

examples of extrusive igneous

A

obsidian
pumice
andesite

17
Q

two types of intrusive bodies

A

concordant and discordant

18
Q

When the pre-existing rock bed is cut across by an intrusive body

A

concordant

19
Q

while if it runs parallel to the bedrock, igneous rock bodies are called

A

discordant

20
Q

sills

A

concordant

21
Q

dikes and laccolith

A

discordant

22
Q

are large intrusive bodies formed deep within Earth

A

Batholiths

23
Q

textures of igneous rocks

A

aphaneitic
phaneritic
pegmatitic
vesicular
porphyritic
amygdaloidal
pyroclastic

24
Q

has crystals that are too fine-grained to be seen by the naked
eye or even with the help of a hand lens

A

Aphanitic

25
Q

has grains that are coarse enough to be visible to the eye

A

Phaneritic

26
Q

has crystals are greater than 3 cm due to very slow cooling

A

Pegmatitic

27
Q

contains tiny holes called vesicles due to gas bubbles in the
lava or magma

A

Vesicular

28
Q

are rocks where larger crystals are embedded in smaller crystals

A

Porphyritic

29
Q

is when vesicles are filled by low-temperature minerals after
the solidification of magma

A

Amygdaloidal

30
Q

is formed from the consolidation of individual rock fragments
that are ejected during a volcanic eruption.

A

Pyroclastic

31
Q

igneous rock is usually light colored and contains large amounts of
quartz, potassium feldspar, and plagioclase.

is also called granitic igneous
rock

A

Felsic

32
Q

igneous rock is medium gray or medium green and consists
of major minerals like amphibole, plagioclase, and feldspar

A

Intermediate

33
Q

igneous rock is dark gray to black-colored and composed largely of
plagioclase and amphibole with small amounts of olivine.

is also called as
basaltic igneous rock.

A

Mafic

34
Q

igneous rock has a very dark green to black shade and consists
largely of olivine and pyroxene.

A

Ultramafic

35
Q

Types of Igneous Rocks Based on Mineral Composition

A

Felsic
Intermediate
Mafic
Ultramafic