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Page 1: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths
Page 2: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

Chapter: Rocks and Minerals

Table of ContentsTable of Contents

Section 3: Metamorphic Rocks and the Rock Cycle

Section 1: Minerals—Earth’s Jewels

Section 2: Igneous and Sedimentary Rocks

Page 3: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Minerals are inorganic, solid materials found in nature. Inorganic means they usually are not formed by plants or animals.

• X-ray patterns of a mineral show an orderly arrangement of atoms that looks something like a garden trellis.

What is a mineral?— Minerals Defined

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Page 4: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• The particular chemical makeup and arrangement of the atoms in the crystal is unique to each mineral.

• Rocks usually are made up of two or more minerals.

What is a mineral?— Minerals Defined

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• Each mineral has unique characteristics you can use to identify it.

Page 5: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Minerals form in several ways. One way is from melted rock material inside Earth called magma.

• As magma cools, atoms combine in orderly patterns to form minerals.

How do minerals form?

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Page 6: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Evaporation can form minerals.

• Just as salt crystals appear when seawater evaporates, other dissolved minerals, such as gypsum, can crystallize.

How do minerals form?

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Page 7: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• A process called precipitation (prih sih puh TAY shun) can form minerals, too.

• Water can hold only so much dissolved material. Any extra separates and falls out as a solid.

How do minerals form?

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Page 8: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Large mineral grains that fit together like a puzzle seem to show up in rocks formed from slow-cooling magma.

Formation Clues

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Page 9: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• If you see large, perfectly formed crystals, it means the mineral had plenty of space in which to grow.

Formation Clues

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• This is a sign they may have formed in open pockets within the rock.

Page 10: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Each mineral has a set of physical properties that can be used to identify it.

• Most common minerals can be identified with items you have around the house and can carry in your pocket, such as a penny or a steel file.

Properties of Minerals

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Page 11: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• All minerals have an orderly pattern of atoms.

• The atoms making up the mineral are arranged in a repeating pattern.

Crystals

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• Solid materials that have such a pattern of atoms are called crystals.

Page 12: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Minerals that split into pieces with smooth, regular planes that reflect light are said to have cleavage (KLEE vihj).

Cleavage and Fracture

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• Cleavage is caused by weaknesses within the arrangement of atoms that make up the mineral.

Page 13: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Not all minerals have cleavage. Some break into pieces with jagged or rough edges.

Cleavage and Fracture

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• Materials that break this way, such as quartz, have what is called fracture (FRAK chur).

Page 14: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Sometimes a mineral’s color can help you figure out what it is. But color also can fool you.

Color

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• The common mineral pyrite (PI rite) has a shiny, gold color similar to real gold.

• Because of this, pyrite also is called fool’s gold.

Page 15: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Scraping a mineral sample across an unglazed, white tile, called a streak plate, produces a streak of color.

Streak and Luster

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Page 16: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

Streak and Luster

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• The streak is not necessarily the same color as the mineral itself. This streak of powdered mineral is more useful for identification than the mineral’s color.

Page 17: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Luster describes how light reflects from a mineral’s surface.

Streak and Luster

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• If it shines like a metal, the mineral has metallic (muh TA lihk) luster.

• Nonmetallic minerals can be described as having pearly, glassy, dull, or earthy luster.

Page 18: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Friedrich Mohs developed a way to classify minerals by their hardness.

Hardness

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• The Mohs scale classifies minerals from 1 (softest) to 10 (hardest).

Page 19: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

Hardness

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• You can determine hardness by trying to scratch one mineral with another to see which is harder.

Page 20: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Specific gravity compares the weight of a mineral with the weight of an equal volume of water.

Specific Gravity

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• Pyrite—or fool’s gold—is about five times heavier than water. Pure gold is more than 19 times heavier than water.

• Measuring specific gravity is another way you can identify minerals.

Page 21: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• The mineral magnetite will attract a magnet.

Other Properties

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• The mineral calcite has two unusual properties. It will fizz when it comes into contact with an acid like dilute HCl.

• Also, if you look through a clear calcite crystal, you will see a double image.

Page 22: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Only a small number of the more than 4,000 minerals make up most rocks.

Common Minerals

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• Most of the rock-forming mineralsare silicates (SIH luh kaytz), which contain the elements silicon and oxygen.

Page 23: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

Common Minerals

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• More than half of the minerals in Earth’s crust are types of a silicate mineral called feldspar.

Page 24: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Other important rock-forming minerals are carbonates.

Common Minerals

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• The carbonate mineral calcite makes up most of the common rock limestone.

Page 25: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• Gems are minerals that are rare and can be cut and polished, giving them a beautiful appearance.

Gems

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• To be gem quality, most minerals must be clear with few or no blemishes or cracks.

• A gem also must have a beautiful luster or color.

Page 26: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• One reason why gems are so rare is that they are formed under special conditions.

The Making of a Gem

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• Diamond, for instance, is a form of the element carbon.

• Scientists suggest that diamond forms deep in Earth’s mantle. It takes a certain kind of volcanic eruption to bring a diamond close to Earth’s surface, where miners can find it.

Page 27: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• A mineral is called an ore if it contains enough of a useful substance that it can be sold for a profit.

Ores

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• The iron used to make steel comes from the mineral hematite, lead for batteries is produced from galena, and the magnesium used in vitamins comes from dolomite.

• Ores of these useful metals must be extracted from Earth in a process called mining.

Page 28: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

• After an ore has been mined, it must be processed to extract the desired mineral or element.

Ore Processing

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• Smelting melts the ore and thenseparates and removes most of the unwanted materials.

Page 29: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

Ore Processing

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• After this smelting process, it can be refined, which means that it is purified.

Page 30: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

Section CheckSection Check

11Question 1

What does inorganic mean?

Answer

Inorganic means not formed by plants or animals.

Page 31: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

Section CheckSection Check

11Question 2

List some places you might find minerals in your home.

Answer

You can find minerals in salt shakers, pencils, glasses, and ceramic dishes.

Page 32: Chapter: Rocks and Minerals Table of Contents Section 3: Metamorphic Rocks and the Rock CycleMetamorphic Rocks and the Rock Cycle Section 1: MineralsEarths

Section CheckSection Check

11Question 3

Explain the difference between a rock and a gem.

Answer

Gems are rare minerals that can be cut and polished. They have a beautiful color and lack cracks or blemishes. Rocks are often cloudy and when they are cut, they crack.