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Chapter 3.1
| Term | Definition |
|---|---|
| Mineral | A naturally occurring, inorganic solid that has a crystal structure and a definite chemical composition. |
| Mohs Hardness Scale | A scale ranking ten minerals from softest to hardest, used in testing the hardness of minerals. |
| Crystal structure | A solid in which the atoms are arranged in a pattern that repeats again and again allowing crystallization to occur. |
| Cleavage | A mineral’s ability to split easily along flat surfaces. |
| Crystallization | The formation of crystals process-when atoms are arranged to form a material with a crystal structure. |
| Fracture | The way a mineral looks when it breaks apart in an irregular way, uneven edges. |
| Luster | The way light reflects off the surface of a mineral. |
| Inorganic | Not formed from living things or remains of living things. |
| Geode | A hollow rock inside which mineral crystals have grown. |
| Streak | The color of a mineral’s powder. |
| Solution | A mixture in which one substance is dissolved in another. |
| Vein | A narrow deposit of mineral that is very different from the surrounding rock. |
| Talc | The softest mineral, can be scratched by your fingernail. |
| Diamond | The hardest mineral, can only be scratched by itself. |
| Surface color | This is the least reliable test to identify a mineral and should be be used on its own. |
| Compound | Made of two or more elements that are chemically bonded. Most minerals are this type of substance. |
| Element | A substance that cannot be broken down, it is in its most pure form. Minerals such as gold, copper and silver are included. |
| Minerals from solutions | When elements and compounds that are dissolved in water leave a solution, crystallization occurs. |
| Slow cooling magma | Leads to large crystals |
| Rapid cooling magma | Leads to small crystals |
| Minerals from organic processes | Clams and shells are made of the mineral calcite. |
| Pyrite | The mineral that is nicknamed, "fools gold" and has cubic crystals. |
| Faces and Angles | Geologists measure a mineral's crystal pattern by its __________. |