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Rocks & Minerals
| Term | Definition |
|---|---|
| Texture | The look and feel of a rocks surface, determined by the size, shape, and pattern of a rocks grains. |
| Fine grain | Fine-grained textures generally indicate magmas that rapidly cooled at or near the Earth's surface |
| Coarse grain | Coarse grain varieties (with mineral grains large enough to see without a magnifying glass) are called phaneritic. |
| Porphyry | a hard igneous rock containing crystals, usually of feldspar, in a fine-grained, typically reddish ground mass. |
| Intrusive Igneous Rock | Intrusive igneous rocks form when magma cools slowly below the Earth's surface. |
| Extrusive Rock | Extrusive igneous rocks form when magma reaches the Earth's surface a volcano and cools quickly. |
| Compaction | Compaction refers to the process by which a sediment progressively loses its porosity due to the effects of loading. |
| Erosion | the process of eroding or being eroded by wind, water, or other natural agents. |
| Cementation | the binding together of particles or other things by cement. |
| Deposition | Deposition is the geological process in which sediments, soil and rocks are added to a land form or land mass. |
| Clastic Rocks | Clastic rocks are composed of fragments, or clasts, of pre-existing minerals and rock |
| Chemical Rock | Chemical sedimentary rocks form by precipitation of minerals from water |
| Sediment | Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice, and/or by the force of gravity acting on the particles. |
| Foliated |