rocks and minerals

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{ Rocks and Minerals Lecture Part I: Minerals

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Rocks and Minerals. Lecture Part I: Minerals. Five Properties of Minerals. Crystal Structure. Naturally occurring. Solid. Definite Chemical Composition. Definite volume and shape. Formed by processes in natural world. mineral. Inorganic. Did not come from something living. - PowerPoint PPT Presentation

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Page 1: Rocks and Minerals

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Rocks and Minerals

Lecture Part I: Minerals

Page 2: Rocks and Minerals

mineral

Definite Chemical

Composition

Inorganic

Crystal Structure

Naturally occurring

Solid

Five Properties of Minerals

Did not come from something living

Repeating pattern

Always contains the same elements

Definite volume and shape

Formed by processes in natural world

Page 3: Rocks and Minerals

Over 4,000 minerals exist!

Scientists use 8 different properties to identify

minerals.

Page 4: Rocks and Minerals

color streak luster

density hardness

Crystal type cleavage or fracture

special properties

How do we identify minerals?

Page 5: Rocks and Minerals

1. Color - easily observed but many minerals have the same color.

Which one is the mineral, gold?

Pyrite Gold Chalcopyrite

Page 6: Rocks and Minerals

2. Streak – the color of a mineral’s powder.

Try it: hematite #19 & galena #14

Page 7: Rocks and Minerals

3. Luster – how light reflects on the surface of the mineral.

Metallic Glassy Waxy, Greasy

Dull Silky Earthy

Page 8: Rocks and Minerals

4. DensityThe mass in a given space – how much “stuff” is in the mineral.

The density does not change based on size.

Density = Mass / Volume

Page 9: Rocks and Minerals

5. Hardness – one of the best clues to identify a mineral.

Mohs Hardness Scale (1812) – ranks ten minerals from hard to soft.

A scratch test is used to determine hardness.

Page 10: Rocks and Minerals

6. Crystal Systems – atoms in a mineral grow in a pattern.

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7. Cleavage & Fracture

A mineral that splits evenly along flat

surfaces.

A mineral that does not split apart

evenly.

mica talc

Page 12: Rocks and Minerals

8. Special Properties

Some minerals have fluorescence, magnetism,

reactivity to acids, and optical properties.

Page 13: Rocks and Minerals

Minerals are INORGANIC and naturally occurring.

Minerals have a crystal structure with a definite chemical composition.

They are identified by their color, streak, luster, density, hardness, cleavage or fracture, and special properties.

IN SUMMARY…

Page 14: Rocks and Minerals

HOW MINERALS FORM

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Pop Quiz

1. What is the difference between a rock & a mineral?2. What are the five characteristics of ALL minerals?3. What are 8 properties used to identify minerals?4. How do you calculate density?5. What is the difference between cleavage & fracture?6. What is the difference between color & streak?7. What is the Mohs Hardness Scale?

Page 16: Rocks and Minerals

The process by which atoms are arranged to form a material with a crystal structure.

geode

Crystallization

Page 17: Rocks and Minerals

Two Ways Minerals Form

1) crystallization of lava or magma, 2) crystallization of materials in

solutions.

Page 18: Rocks and Minerals

Minerals From Magma & Lava

When these liquids cool to a solid state, they form crystals.

Page 19: Rocks and Minerals

Minerals From Solutions

Solution - A mixture in which one substance is dissolved in another.

Page 20: Rocks and Minerals

Minerals Formed by Evaporation

When ancient seas slowly evaporated, minerals formed (halite, gypsum, calcite).

HALITE

Page 21: Rocks and Minerals

Minerals from Hot Water Solutions

Elements that form minerals dissolve in hot water underground; when the solution cools, the elements

crystallize as minerals.

These iron-rich minerals formed at an undersea vent

Page 22: Rocks and Minerals

Pure Metal VeinsA narrow channel of a mineral that is different

from the surrounding rock; usually pure metals.

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The Size of CrystalsDepends on the rate at which the magma/lava

cools or the solution evaporates.

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Slow Cooling Crystals

Slow cooling leads to the formation of large crystals.

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Rapid Cooling Crystals

Magma closer to the surface loses heat energy much faster than magma deep below ground.

Rapid cooling leaves no time for large crystals. Crystals are small.

Page 26: Rocks and Minerals

Minerals form from magma and lava when the hot magma cools inside the crust or the lava hardens on the surface.

Minerals form when elements and compounds are dissolved in water and they leave a solution which eventually crystallizes.

Minerals form when solutions evaporate (Example: halite from the ancient seas and gypsum)

IN SUMMARY…

Page 27: Rocks and Minerals

Preview “minerals an their uses”

Mineral identification using samples. Name of mineral 3 words to DESCRIBE it.

Mineral poster – front side Title: Your mineral In the center draw/print/glue a picture of something that contains your mineral 5 bubbles around the picture in the center that describe the PROPERTIES of

that mineral Minerals Lab Part I: DENSITY (review identification

properties) Analysis: explain the other ways to identify minerals. Make crystals with kit Make your own sugar crystals