Lab Exercise - Mineral Properties Uses and Identification 2
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School
California State University, Long Beach *
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Course
104
Subject
Geology
Date
Apr 3, 2024
Type
Pages
9
Uploaded by DoctorEchidna6113
Geology Lab 1 Lab Exercise - Mineral Properties, Uses and Identification Name: Date: Part #1 1.
List five characteristics that describe a mineral: 2.
Luster –
How a mineral reflects light. Include whether it is metallic or nonmetallic and whether the mineral is shiny/glassy or dull. a.
Indicate whether the luster of each of the following materials is metallic (M) of nonmetallic (NM): a brick: magnet: ice: sharpen pencil lead: frying pan: a mirror: b.
From your tray of minerals, how many of your specimens can be grouped into each of the following luster types? Metallic: Nonmetallic: 3.
Light transmission –
Ability of light to penetrate a mineral. If opaque,
no light penetrates; if translucent,
some light penetrates; if transparent,
most light penetrates through a mineral. a.
From your tray of minerals, how many of your specimens are transparent and how many are opaque and how many are translucent? Transparent: Opaque: Translucent: 4.
Color –
Combination of wavelengths of light absorbed and refracted from a mineral. Some minerals will always have the same color, but other minerals can have a variety of colors based on impurities within the minerals
’
crystalline structures. This is especially true for the “
colorless
”
minerals like quartz and calcite. a.
From your tray of minerals, select two of your mineral specimens and describe those that appear to be the same mineral but with variable colors: Mineral Name: Color Color Mineral Name: Kaylee
Cruz
10/03/23
Naturally
occuring
solid
I
generally
Inorganic
define
chemical
composition
orderly
crystalline
structure
NM
M
NM
M
M
NM
S
10
kompletely
3
10
I
kinda
clears
(not
clear)
clear)
feldspar
red
white
R
black
Geology Lab 2 5.
Streak –
Color of powdered mineral on a porcelain streak plate. Metallic minerals always have a bold streak that is easy to see. 6.
Hardness –
Resistance of a mineral to being scratched by another substance. Geologist use Mohs Hardness Scale. Use the Mohs Hardness Scale (below) to answer questions #7 and #8: 7.
A mineral can be scratched by a masonry nail or knife blade but cannot be scratched by a wire (iron) nail: a)
Is this mineral hard or soft? b)
What is the hardness number of this mineral on Mohs Scale? c)
What mineral is this? 8.
A mineral can scratch calcite and the same mineral can be scratched by a wire (iron) nail: a)
What is the hardness number of this mineral on Mohs Scale? b)
What mineral on Mohs Scale has this hardness? 9.
Crystal Form –
External appearance of a mineral determined by the bonding arrangements of the atoms in a mineral. For example, quartz has a hexagonal (six sided) form. But, when quartz is broken, this form will no longer be present because the shape does not exist on the inside of this mineral. 10.
Breakage –
How a mineral break. If breakage is random and uneven, then the mineral fractures
. If the mineral breaks along pre-existing planes of weakness, called cleavage planes, then the breakage is called cleavage
. Note that some mineral only fracture when they break, like quartz. Some minerals only cleave when they break, like halite. And some mineral cleave and fracture, like feldspar. soft
S
apalite
4
flowrite
Geology Lab 3 Use the figure above, common cleavage directions of minerals to answer question #11 and # a.
From your tray of minerals, name two minerals you identified that have good cleavage. Describe the cleavage of each mineral. Specimen #1 Mineral Name Cleavage Specimen #2 b.
From your tray of minerals, name two minerals you identified that have no cleavage, they fracture. Specimen #3 Mineral Name Cleavage Specimen #4 11.
Specific Gravity –
Density per unit of volume of a mineral. Metallic minerals tend to be very heavy for their size, so they have a high specific gravity (Sp.Gr.), a 4 or 5 on the Sp.Gr. scale. 12.
Magnetism –
Attraction of iron rich minerals to magnetic field. This is especially true of the mineral magnetite
.
13.
Reaction to hydrochloric acid (HCl) –
Bonds holding carbonate minerals together are ready broken when they contact HCl, causing bubbling or fizzing. 14.
Tenacity –
The brittleness of a mineral. The mineral hematite will scratch glass, but when you rub it with your thumb, it will flake off onto your skin. Hematite has a low tenacity –
it is very brittle. 15.
“
Feel
”
–
Weakly bonded minerals often have a very low tenacity, giving them a greasy or soapy feel, such as with the mineral Talc
. calcite
in
three
directions
galena
in
three
directions
quarte
prismic
smooth
hemanize
absent
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Geology Lab 4 Part #2 16.
"Rocks are minerals and minerals are rocks". Why is this statement incorrect? Part #3 17.
Obtain a set of minerals as directed by your instructor. Using the physical properties described in Part #1 identify the mineral hand samples and then fill in the mineral
’
s information on the Mineral Hand Sample Lab Identification sheet. This
statement
is
incorrect
because
most
of
the
time
,
rocks
S
will
contain
minerals
,
while
minerals
always
contain
atoms
.
N
ame:
Date:
Name
(formula)
Place mineral in square
Luster:
Metallic or Nonmetallic
Hardness
Color
Streak
Cleavage: Perfect, Good or Absent
Other Properties
Plagioclase feldspar
(
Na or Ca+AlSiO
3
O
8
)
Place mineral here
Potassium-Feldspar
(
KAlSi
3
O
8
)
Place mineral here
Muscovite mica
(
K, OH, Al silicate
)
Place mineral here
Minerial Identification
Stamp:
page 1
Kaylee
Cruz
10/03/23
colorless
;
may
have
white
,
iridescent
Play
of
NM
6
gray
or
white
good
color
from
S
black
within
orange
,
forms
brown
,
translucent
white
,
NM
6
green
or
white
perfect
prisms
/
pink
colorless
,
can
be
yellow
,
5
lit
into
NM
2
-
2
.
5
brown
white
perfect
thin
flexible
or
transparent
red
Sheets
brown
Biotite mica
(
K, Mg, Fe, Al silicate
)
Place mineral here
Augite
(
Ca, Mg, Fe, Al silicate
)
Place mineral here
Hornblende
(
Ca, Na, Mg, Fe, OH, Al silicate
)
Place mineral here
Olivine
(
(Mg, Fe)
2
SiO
4
)
Place mineral here
page 2
black
,
green
gray-
2
.
5
-
3
black
,
or
brown
creates
NM
brown
-
perfect
flexible
black
sheets
dark
white
to
forms
+O
green
pale
gray
good
Short
NM
S
.
5-6
gray
dark
gray
to
white
NM
S
.
S
black
to
good
brittle
pale
gray
pale
Or
conchiodal
dark
ol=
fracture
NM
I
ine
green
white
abset
t
I
or
brown
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Quartz (
SiO
2
)
Place mineral here
Calcite (
CaCO
3
)
Place mineral here
Gypsum (
CaSO
4
+2H
2
0
)
Place mineral here
Halite (
NaCl
)
Place mineral here
page 3
usually
transparent
colorless
Ho
NM
7
white
absent
translucent
usually
forms
NM
3
colorless
white
perfect
prisms
colorless
;
forms
white
or
tabular
NM
2
gray
white
good
crystals
colorless
;
white
,
y-
forms
ellow
,
blue
,
Ni
2
.
S
brown
,
white
perfect
cures
Or
red
Limonite
(
Fe
2
O
3
+H
2
O
)
Place mineral here
Magnetite
(
Fe
3
O
4
)
Place mineral here
Hematite
(
Fe
2
O
3
)
Place mineral here
Pyrite
(
FeS
2
)
Place mineral here
page 4
Mor
yellow
tarnishes
brocon
to
yelloco
NM
1
-
5
.
5
brown
absent
yellow
dark
t
brown
brown
silvery
tarnishes
M
6-6
.
S
sy
dark
absent
gray
b
lack
grey
MON
silvery
gray
,
red
to
I
reddish
/
NM
1
-
6
silver
,
brown
absent
opaque
black
,
or
brick
red
silver
y
tarnishes
gold
M
6-6
.
5
dark
absent
brown
grey
Fluorite (
CaF
2
)
Place mineral here
Talc (
Mg silicate
)
Place mineral here
Graphite
(
C
)
Place mineral here
page 5
colorless
;
crystals
purple
,
usually
NM
4
blue
,
white
perfect
cubes
gray
,
green
,
or
yellow
white
3
feels
gray
,
greasy
NM
I
Pale
white
absent
or
soapy
green
,
or
broron
dark
dark
greasy
silvery
feel
M
I
gray
to
gray
perfect
black
tarnishes
I
bright
gray
to
dark
Galena
M
2
.
S
silve
ry
dark
good
gray
gray
gray
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