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Bellringer: Sort these items into minerals and not minerals: Wood

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Presentation on theme: "Bellringer: Sort these items into minerals and not minerals: Wood"— Presentation transcript:

1 Bellringer: Sort these items into minerals and not minerals: Wood
Sulfur Feldspar Fossil Granite Gold Copper Halite Ice Water Talc Topaz Dirt Smoke Sun

2 What is a Mineral?

3 What is a mineral? Properties:
Solid Cannot be a liquid or a gas Naturally Occurring Found in nature, not man-made Inorganic Is not alive and never was, non-living Fixed composition Has a chemical formula, most are formed from compounds of two or more elements, some minerals consist of one element ex. Au Crystal Form A definite structure in which atoms are arranged

4 What is a mineral? Definition:
A mineral is a naturally formed, inorganic solid that has a definite crystalline structure. -Questions to ask yourself when determining if an item is a mineral or not: Is it non-living material? Is it a solid? Is it formed in nature? Does it have a crystalline structure?

5 Minerals are identified by their key characteristics
hardness crystal shape (form) luster color Streak Density (specific gravity) Cleavage/fracture special properties --reaction to acid --fluorescence --salty taste --magnetism

6 Hardness Refers to "scratchability" or resistance to being scratched. Harder minerals will scratch softer minerals. Geologists rank minerals according to hardness using the Moh's scale Moh's Hardness Scale 1.0     TALC 2.0    GYPSUM FINGERNAIL 3.0    CALCITE 3.5    COPPER PENNY 4.0    FLUORITE 5.0    APATITE 5.5    STEEL KNIFE/GLASS PLATE 6.0    FELDSPAR 7.0    QUARTZ 8.0     TOPAZ 9.0     CORUNDUM (RUBY) DIAMOND

7 Crystal Shape (Form) External structure due to internal arrangement of the atoms

8

9 Luster Describes how light reflects off the surface
Main categories are “metallic” and “non- metallic” Non-metallic includes “dull,” glassy,” waxy,” “pearly,” and others

10 Non-metallic mineral Metallic mineral

11 Cleavage and Fracture -Cleavage refers to the pattern of very smooth, flat, or reflective surfaces that a mineral “cleaves” or breaks into. -These special breakage surfaces correspond to zones of weak bonding in the crystal structure. -Other minerals break unevenly along rough or curved surfaces--this is called fracture NO cleavage

12 Color -Color results from ability to absorb some wavelengths and reflect others -some minerals have characteristic color while others vary due to chemical differences or impurities (rust, other mineral, etc.) e.x. quartz -VERY unreliable.

13 Streak Color of the powder when rubbed on a “streak plate” (unglazed porcelain) Always the same unlike color.

14 Density (Specific Gravity)
density (mass /volume) Specific Gravity is the density of the mineral compared with density of water

15 Special Characteristics-- Fluorescence
Some minerals will glow when placed under ultraviolet light Carbonates react with dilute HCl and other acids by fizzing or bubbling (releasing CO2 gas) The “Acid Test”

16 Special Characteristics-- Salty Taste
DO NOT TASTE MOST MINERALS! Halite is the exception--it will taste salty

17 Special Characteristics-- Magnetism
Many iron minerals will produce an invisible magnetic force field


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