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Chapter 3
Minerals
| Term | Definition |
|---|---|
| Silicates | Minerals that contain silicon and oxygen. |
| Nonsilicates | Minerals that do no contain silicon and oxygen, but may contain oxygen. |
| Reclamation | Returning the land back to an original state. |
| Mineral | Four must haves are solid, inorganic, made in nature and has a crystal structure. |
| Surface mines | Three examples are open pit, quarry and strip mining. |
| Subsurface mines | Three examples are slope, drift and shaft. |
| Ore | Mineral deposit large enough and pure enough to earn a profit. |
| Color | Not always reliable because of the effects of weathering and the atmosphere. |
| Luster | Reflection of light by a mineral. |
| Hardness | Measure of the resistance to being scratched. |
| Cleavage | Breaks along flat planes. |
| Fracture | Breaks along curved, messy surfaces. |
| Density | Ratio of mass to volume. |
| Fluorescence | Glowing under UV light. |
| Magnetism | Attracts Iron. |
| Radioactive | Waves emitted may be detected by a Geiger counter. |
| Chemical reaction | Fizzing may occur after contact with acids. |
| Optical | The ability to see double with a clean specimen. |
| Pegmitites | With enough time gemstones grow in these tear drop shaped objects. |
| Metamorphic | Heat and pressure can change the chemical make-up of minerals. |
| Non metallic Minerals | Used in construction, for example concrete, roads and bridges. |
| Metallic Minerals | Used in electronics, space craft, airplanes and more. |
| Recycle | Being mindful of natures resources, this helps extend the life of mineral sources. |
| Halite and Gypsum | Evaporating water leaves behind these minerals. |