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Unit 3 – Minerals and Rocks Do Now – Number the pages (there should be 40) HW – You may clean out your folders.

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Presentation on theme: "Unit 3 – Minerals and Rocks Do Now – Number the pages (there should be 40) HW – You may clean out your folders."— Presentation transcript:

1 Unit 3 – Minerals and Rocks Do Now – Number the pages (there should be 40) HW – You may clean out your folders

2 Minerals are: Important Vocabulary Today’s Objective: What is a Mineral? Naturally occurring – Forms by natural geologic processes. Solid substance

3 Inorganic – not living Calcite primarily comes from the remains of shells from living organisms Definite chemical composition – most are made up of two or more elements.

4 Orderly crystalline structure – atoms are arranged in an orderly and repetitive manner. Crystals – A solid body having a visually symmetrical pattern to it’s atomic arrangement

5 Example - Crystalline Structures Silicon and Oxygen combine to form a structure called the Silicon-Oxygen Tetrahedron. Sand (SiO 4 ) is a common silicate

6 Because the atoms are arranged differently. Diamond Graphite The following minerals are both made of pure Carbon, why do they look different?

7 How are minerals formed? Precipitates Minerals are left behind from a body of water when it evaporates Example - Rock Candy As the water evaporates the sugar is left behind

8 Heat and Pressure Changes minerals into new minerals Crystallize Minerals that form out of cooling magma

9 Hydrothermal Super heated water causes chemical reactions that change minerals into new ones.

10 A mineral’s properties are caused by its internal arrangement of atoms.

11 Color (NOT reliable) -Many minerals have the same color OR one mineral can have many colors -Small amounts of different elements can give the same mineral different colors. Properties of Minerals

12 Streak - Streak is the color of a mineral in its powdered form. - Streak is obtained by rubbing a mineral across a streak plate (a piece of porcelain.)

13 Hardness -Hardness is a measure of the resistance of a mineral to being scratched on glass. -The Mohs scale consists of 10 minerals arranged from 10 (hardest) to 1 (softest). - Glass has a hardness of about 5.5

14 Other - Few minerals bubble in the presence of an acid (Calcite and Dolomite)

15 Cleavage - Cleavage is the tendency of a mineral to cleave, or break, along flat, even surfaces. Fracture - Fracture is the uneven breakage of a mineral.

16 Luster - Luster is used to describe how light is reflected from the surface of a mineral. Metallic vs. Non-Metallic

17 Watch the video and take the REVIEW quiz rvcschools


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