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Rocks & Minerals NOTES Pages ©Mark Place,

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Presentation on theme: "Rocks & Minerals NOTES Pages ©Mark Place,"— Presentation transcript:

1 Rocks & Minerals NOTES Pages 1 - 3 ©Mark Place, 2009-2010

2 ESRT Mineral Chart Click Here
Frayer Model Box #1 What is a mineral? naturally occurring inorganic It is a definite chemical composition substance which has a What would be the opposite of this? man-made Organic (Living) mixture ESRT Mineral Chart Click Here

3 Graphite (pencil lead)
Frayer Model box #2 Minerals can be made of the same elements But have different physical properties because of the way their atoms are arranged. Two examples of common minerals Click Here Graphite (pencil lead) & Diamonds (Jewelry)

4 The Least Useful Physical Property Used to Identify Minerals
Frayer Model Box #3 The Least Useful Physical Property Used to Identify Minerals Color a poor indicator minerals can be multiple colors many minerals are the same color

5 The Most Useful Physical Properties Used to Identify Minerals
Frayer Model Box # 4 The Most Useful Physical Properties Used to Identify Minerals 1. Streak 2. Luster 3. Hardness 4. Fracture 5. Cleavage 6. Magnetism

6 The Main Physical Properties Used to Identify Minerals
#1. Streak The mark left when a mineral is rubbed on a tile. more reliable than color the powder form of a mineral

7 The Main Physical Properties Used to Identify Minerals
#2. Luster how light reflects(bounces) off a mineral. metallic non-metallic looks like a metal looks earthy, waxy, greasy ,dull,pearly,silky

8 The Main Physical Properties Used to Identify Minerals
#3. Hardness resistance to being scratched It is NOT the same as breaking! For example: You can break glass easily with steel. However, steel will not scratch glass.

9 The Main Physical Properties Used to Identify Minerals
Hardness Continued Fingernail- 2.5 copper coin 3 and 4 Iron nail- 5 tile-6.5 MOH’S SCALE OF HARDNESS Hardness Mineral 1 (softest) 6 2 7 3 8 4 9 5 10 (hardest) TALC ORTHOCLASE GYPSUM QUARTZ CALCITE TOPAZ FLUORITE CORUNDUM APATITE DIAMOND

10 The Main Physical Properties Used to Identify Minerals
#4. Fracture The mineral breaks randomly and unevenly because of the arrangement of atoms.

11 The Main Physical Properties Used to Identify Minerals
5. Cleavage The mineral breaks in a predictable pattern because of its arrangement of atoms. Some minerals break into smooth flat sheets.

12 Examples of Cleavage

13 Examples of Cleavage

14 Examples of Cleavage

15 Examples of Cleavage

16 Examples of Cleavage

17 Examples of Cleavage

18 Examples of Cleavage

19 One Mineral, Many Colors

20 Different Minerals Same Color


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