2.2 notes a mineral is identified by its properties

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2.2 NOTES A Mineral is Identified by its Properties

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Page 1: 2.2 NOTES A Mineral is Identified by its Properties

2.2 NOTES

A Mineral is Identified by its Properties

Page 2: 2.2 NOTES A Mineral is Identified by its Properties

A MINERAL IS IDENTIFIED BY ITS PROPERTIES

The pictures to the right are all of the mineral Fluorite.

The pieces are different in color, size, and crystal shape, but they are all still Fluorite!

How is this possible?

Page 3: 2.2 NOTES A Mineral is Identified by its Properties

A MINERAL IS IDENTIFIED BY ITS PROPERTIES

As you can see, fluorite occurs in many colors, even colorless forms.

Its crystals can be well formed or poorly formed, smooth, or rough.

Page 4: 2.2 NOTES A Mineral is Identified by its Properties

A MINERAL IS IDENTIFIED BY ITS PROPERTIES

If you came across fluorite while hiking, would you know what it was just by looking at it? Probably not.

In this section we will learn how you could identify it.

Page 5: 2.2 NOTES A Mineral is Identified by its Properties

A MINERAL’S APPEARANCE HELPS IDENTIFY IT

To identify a mineral, you need to observe its properties-characteristic features that identify it.

Page 6: 2.2 NOTES A Mineral is Identified by its Properties

COLOR AND STREAK

Most minerals have a limited color range.

Page 7: 2.2 NOTES A Mineral is Identified by its Properties

COLOR AND STREAK

3 main factors cause minerals to be slightly different colors…

Page 8: 2.2 NOTES A Mineral is Identified by its Properties

COLOR AND STREAK

1. A mineral may get its color from tiny amounts of an element that is not part of its normal chemical makeup.

Page 9: 2.2 NOTES A Mineral is Identified by its Properties

COLOR AND STREAK

Example: Pure quartz is clear and colorless.

Tiny amounts of iron turn quartz purple. This is called amethyst.

Page 10: 2.2 NOTES A Mineral is Identified by its Properties

COLOR AND STREAK

2. A mineral’s color can change when it is at or near Earth’s surface and is in contact with the atmosphere or water.

Page 11: 2.2 NOTES A Mineral is Identified by its Properties

COLOR AND STREAK

3. Mineral crystals might have different shapes that change their color. Example: Hematite with small crystals looks dull.

Hematite with large crystals looks shiny.

Page 12: 2.2 NOTES A Mineral is Identified by its Properties

COLOR AND STREAK

Some minerals have a different color when they are ground into a fine powder than when they are left whole.

Page 13: 2.2 NOTES A Mineral is Identified by its Properties

COLOR AND STREAK

Streak is the color left behind when a mineral is scraped across a surface.

Page 14: 2.2 NOTES A Mineral is Identified by its Properties

COLOR AND STREAK

Scientists use a piece of porcelain, called a streak plate, to help identify minerals

Page 15: 2.2 NOTES A Mineral is Identified by its Properties

COLOR AND STREAK

Streak is a better clue to a mineral’s identity than surface color.

Page 16: 2.2 NOTES A Mineral is Identified by its Properties

COLOR AND STREAK

All samples of the same mineral have the same streak.

Page 17: 2.2 NOTES A Mineral is Identified by its Properties

LUSTER

Luster is the way in which light reflects from a mineral’s surface.

Page 18: 2.2 NOTES A Mineral is Identified by its Properties

LUSTER

Metallic luster makes a mineral look as if it were made of metal. For example, Pyrite (Fool’s Gold) has a metallic luster.

Page 19: 2.2 NOTES A Mineral is Identified by its Properties

LUSTER

Nonmetallic luster gives minerals a shiny look, but they do not appear to be made of metal.

Page 20: 2.2 NOTES A Mineral is Identified by its Properties

THE WAY A MINERAL BREAKS HELPS IDENTIFY IT

Each kind of mineral always breaks in the same way.

Page 21: 2.2 NOTES A Mineral is Identified by its Properties

THE WAY A MINERAL BREAKS HELPS IDENTIFY IT

Calcite breaks into tilted blocks.

Mica splits into thin, flat sheets.

Page 22: 2.2 NOTES A Mineral is Identified by its Properties

CLEAVAGE

Cleavage is the tendency of a mineral to break along flat surfaces.

Page 23: 2.2 NOTES A Mineral is Identified by its Properties

CLEAVAGE

The way in which a mineral breaks depends on how its atoms are bonded.

Minerals that have cleavage have weak bonds in the direction that the mineral breaks

Page 24: 2.2 NOTES A Mineral is Identified by its Properties

FRACTURE

Fracture is the tendency of a mineral to break into irregular pieces.

Page 25: 2.2 NOTES A Mineral is Identified by its Properties

FRACTURE

Minerals that have fracture have bonds that are equal in all directions.

This means the mineral will not break along flat surfaces. Example: Quartz breaks by

fracturing.

Page 26: 2.2 NOTES A Mineral is Identified by its Properties

A MINERAL’S DENSITY AND HARDNESS HELP IDENTIFY IT

A tennis ball is not as heavy or as hard as a baseball.

You would be able to tell the two apart even with your eyes closed.

Minerals can be identified in the same way.

Page 27: 2.2 NOTES A Mineral is Identified by its Properties

DENSITY

What weighs more, a pound of bricks or a pound of feathers?

Page 28: 2.2 NOTES A Mineral is Identified by its Properties

DENSITY

What takes up more room, a pound of bricks or a pound of feathers?

Page 29: 2.2 NOTES A Mineral is Identified by its Properties

DENSITY

The bricks are more dense; they have more density!

Page 30: 2.2 NOTES A Mineral is Identified by its Properties

DENSITY

Density is the amount of mass in a given volume of a substance.

Page 31: 2.2 NOTES A Mineral is Identified by its Properties

DENSITY

Example: 1 cm3 of pyrite has a mass of 5.1 grams.

Its density is 5.1 g/cm3

Page 32: 2.2 NOTES A Mineral is Identified by its Properties

DENSITY

Examining the density of minerals is a helpful way of identifying them.

Real gold is far more dense than pyrite (fool’s gold).

Page 33: 2.2 NOTES A Mineral is Identified by its Properties

HARDNESS

A mineral’s hardness is its resistance to being scratched.

Page 34: 2.2 NOTES A Mineral is Identified by its Properties

HARDNESS

The Mohs scale is often used to describe a mineral’s hardness.

On the Mohs scale, Talc is the softest with a value of 1 and Diamond is the hardest with a value of 10.

Page 35: 2.2 NOTES A Mineral is Identified by its Properties
Page 36: 2.2 NOTES A Mineral is Identified by its Properties

HARDNESS

You can test the hardness of various minerals by the items they are or are not able to scratch.

Page 37: 2.2 NOTES A Mineral is Identified by its Properties

SOME MINERALS HAVE SPECIAL PROPERTIES

Some, but not all, minerals have special properties that help to identify them.

Page 38: 2.2 NOTES A Mineral is Identified by its Properties

SOME MINERALS HAVE SPECIAL PROPERTIES

Minerals in the carbonate group react with acid.

Page 39: 2.2 NOTES A Mineral is Identified by its Properties

SOME MINERALS HAVE SPECIAL PROPERTIES

Fluorescent minerals glow when they are exposed to UV light.

Page 40: 2.2 NOTES A Mineral is Identified by its Properties

REVIEW

1. How is it possible for two different minerals to have the same chemical composition?

A. They have different chemical structures.

B. One is formed only by organisms.

C. Only one is a rock-forming mineral.

D.They have different appearances.

Page 41: 2.2 NOTES A Mineral is Identified by its Properties

REVIEW

2. Which of the following is the least reliable clue to a mineral’s identity?

A.Color

B.Density

C.Hardness

D.Luster

Page 42: 2.2 NOTES A Mineral is Identified by its Properties

REVIEW

3. Many properties of a mineral are related to the

A. Number of elements of which it is made.

B. Other types of minerals present as it formed.

C. Strength of bonds between its atoms

D.Speed at which it formed.