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Rocks and Minerals
| Term | Definition |
|---|---|
| Mineral | A naturally occurring, inorganic solid that has a crystal structure and a definite chemical composition. |
| Crystal Structure | A definite pattern in the way that particles in a substance are arranged. |
| Moh's Hardness Scale | German scientist, Friedrich Mohs developed this scale to help people study the hardness of rocks. |
| Luster | How a mineral reflects light from it's surface. |
| Hardness | A way to describe how hard it is to scratch a mineral. |
| Cleavage | The tendency of a mineral to break along a flat surface where layers of atoms are attached weakly to each other. |
| Fracture | The tendency of a mineral to break in a way that is not along a flat surface. |
| Streak | The color of a mineral in it's powdered form. |
| Crystalization | The process by which atoms are arranged to form a material with a crystal structure. |
| Solution | A mixture in which one substance is dissolved into another. |
| Vein | A narrow channel or slab of a mineral that i different from the surrounding rock. |
| Geode | A rounded hollowed rock that is often lined with mineral crystals that are often perfectly formed. |
| Element | A substance that cannot be broken down into other substances. |
| Compound | A substance made of two or more elements that have been chemically combined. |
| Inorganic | A characteristic of a mineral, that means a mineral cannot form from materials that were once apart of a living thing. |
| Fluoresence | Minerals that glow under ultraviolet light. |
| Sediment | Small, solid pieces of material that come from rocks or living things. |
| Compaction | The process that presses sediments together. |
| Erosion | This occurs when running water, wind, or ice loosen and carry away fragment of rock. |
| Cementation | The process in which dissolved minerals crystallize and glue particles of sediment together. |
| Depositon | The process by which sediment settles out of the water or wind carrying it. |
| Clastic Rock | A sedimentary rock that forms when rock fragments are squeezed together. |
| Chemical Rock | This type of rock forms when minerals that are dissolved in a solution crystallize. |
| Organic Rock | This type of rock forms when the remains of plants and animals are deposited in thick layers. |
| Foliated | Metamorphic rock with grains arranged in parallel layers or bands. |
| Non-Foliated | The opposite of foliated |