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Minerals of the Earth's Crust

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Minerals of the

Earth’s Crust







Chapter 9

Mineral: a naturally occurring

substance formed in the Earth

• Inorganic

• Always a

crystalline

solid

• Definite

chemical composition

Over 2,000

are known!

Identifying Minerals:

Color

• Most easily

observed

property

• Yet, least

useful

property

Identifying Minerals: Color

Why it is the least useful

property…

• Different minerals have the same color

• One mineral can have different colors

• Impurities can alter color

• Some change color when exposed to air

• Way a mineral shines in reflected light

distorts color

Identifying Minerals:

Luster

•Way a

mineral

shines in

reflected

light

Identifying Minerals: Luster



Metallic:

shines like polished metal



Pyrite

“Fool’s

Gold”

Identifying Minerals: Luster



Nonmetallic:

does not shine like metal

Identifying Minerals: Luster



Pearly

like a

pearl

Talc

Identifying Minerals: Luster



Greasy





Turquoise

Identifying Minerals: Luster



Vitreous

like

shining

glass

Amethyst

Identifying Minerals: Luster



Resinous

like wax

Identifying Minerals: Luster



Dull or

Earthy







Bauxite

Identifying Minerals:

Crystal Shape

•The shape of a crystal

results from the way

the atoms of a mineral

come together as the

mineral forms

Identifying Minerals:

Streak Test

• Color of a mineral’s

powder form

• Usually, streak is not the

same color as the mineral

• Streak doesn’t vary

Identifying Minerals:

Streak Test

• Metallic mineral has

dark streak

• Nonmetallic – colorless

or light streak

Identifying Minerals:

Cleavage

• The splitting of a mineral

along certain flat surfaces

• Related to the types of

bonds in the internal

structure of the mineral

Identifying Minerals:

Cleavage

Identifying Minerals:

Fracture



• the way a mineral

tends to break

Identifying Minerals:

Fracture







Splintery jagged

Identifying Minerals:

Hardness

•Resistance to being

scratched

•Moh’s hardness scale

• Mohs Scale, • 1. Talc

identified • 2. Gypsum

• 3. Calcite

numerically

• 4. Fluorite

by standard • 5. Apatite

minerals, • 6. Orthoclase

from 1 • 7. Quartz

(softest) to • 8. Topaz

10 (hardest): • 9. Corundum

• 10. Diamond

To remember the Mohs scale

try remembering this phrase:



The Geologist Can Find

An Ordinary Quartz,

(that) Tourists Call

Diamond!

Tools for Testing

Hardness

• You typically do not carry

around a supply of the 10

minerals on the hardness

scale. However, you can use

the following items to help

estimate the hardness of a

mineral:

Tools for Testing

Hardness

• finger nail (H = 2.5)

• penny (H = 3.5)

• common nail (H = 4.5)

• glass plate (H = 5.5)

Identifying Minerals:

Special Properties

•Acid

test

http://www.westhamptonbe

ach.k12.ny.us/Teachers/Co

hen/sciweb/earthscience/s

edimentary/Mvc-327w.mpg

Identifying Minerals:

Special Properties



•Magnetic

test

Identifying Minerals:

Special Properties

•Taste test



Some minerals have a distinct

taste. Never do this test

after the acid test!

Quartz

Feldspar









Mica

Talc









Amphiboles

Galena









Halite

Biotite









Calcite

Hematite









Pyrite

Magnitie









Olivine

Garnets



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