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Minerals Chapter 3 Sec. 1 & 2.

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Presentation on theme: "Minerals Chapter 3 Sec. 1 & 2."— Presentation transcript:

1 Minerals Chapter 3 Sec. 1 & 2

2 What Is a Mineral? A mineral is a naturally formed, inorganic solid that has a definite crystalline structure. All minerals contain one or more of the 92 naturally occurring elements.

3 What is a Mineral? Answer four questions. If any answer is “no” – NOT a mineral!

4 What is a Mineral? 1) Is it nonliving material? 2) Is it a solid?
3) Is it formed in nature? 4) Does it have a crystalline structure?

5 What Are Crystals? Crystals are solid, geometric forms of minerals
Repeating pattern of atoms or molecules creates the crystals A crystal’s shape is determined by the arrangement of the atoms or molecules within the crystal.

6 Crystal Structures

7 Two Groups of Minerals Silicate vs. Nonsilicate
Silicate Minerals: Minerals that contain a combination of silicon and oxygen molecules. These minerals make up more than 90% of Earth’s crust. Examples: Quartz, Feldspar, and Mica.


9 Nonsilicate Minerals: Minerals that do not contain a combination of the elements silicon and oxygen. They are made up of carbon, oxygen (without silicon), fluorine, and sulfur. Examples; Copper, Calcite, Fluorite, and Gypsum


11 There are seven ways to determine the identity of minerals.
Identifying Minerals There are seven ways to determine the identity of minerals.

12 Color Not usually the best way to identify a mineral; for reasons such as impurities.

13 Luster The way a surface reflects light; usually described as shiny or dull Shiny = metallic luster Dull = submetallic, nonmetallic Observe samples


15 Streak The color of a mineral in powdered form.
A mineral’s streak can be found rubbing the mineral against a piece of unglazed porcelain called a streak plate.


17 Cleavage and Fracture Cleavage: the tendency of some minerals to break along smooth, flat surfaces. Fracture: the tendency of some minerals to break unevenly along curved or irregular surfaces.


19 This sample of quartz shows a curved fracture pattern called conchoidal fracture.

20 Hardness A mineral’s resistance to being scratched.
Scientists use Mohs hardness scale to determine the hardness of minerals. ***The greater a mineral’s resistance to being scratched is, the higher the mineral’s rating is.

21 Moh's Hardness Scale

22 Density The measure of how much matter is in a given amount of space.

23 Special Properties Some minerals can be identified by special properties they have, such as taste (NEVER taste in science class!), magnetism, fluorescence, radioactivity, chemical reaction, and optical properties.

24 Special Properties

25 What are Rocks? Rocks are a combination of one or more minerals.

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