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Earth Science Unit 3
Rocks and Minerals Vocabulary
| Term | Definition |
|---|---|
| inorganic | A substance that does not form from living things (plants or animals). |
| solid | definite shape and volume particles are packed together tightly can hold its shape without a container |
| definite chemical composition | Minerals are made up of elements that are in definite proportions. Two or more elements chemically joined from a compound. Almost all minerals are compounds. |
| crystal structure | a repeating pattern of the mineral’s particles forming a solid has flat sides, called faces that meet at sharp edges and corners |
| Streak Test | Observed by rubbing the mineral against an unglazed tile revealing the color of its powder. |
| Luster | used to describe how a mineral reflects light from its surface Ex. Metallic or nonmetallic Quartz = glassy luster |
| cleavage | A mineral that splits easily along flat surfaces |
| fracture | Minerals that do not split easily |
| vesicular | |
| volcanic | |
| intrusive | rocks formed from magma hardened below Earth’s surface. Form larger crystals. granite is the most abundant of this type found in continental crust |
| extrusive | rocks formed from lava erupted onto Earth’s surface. Form smaller crystals. basalt from ocean crust, shield volcanoes and lava plateaus |
| Sedimentary rock | forms when particles of other rocks or remains of living things are pressed or cemented together. |
| clastic | rocks such as sandstone, shale, conglomerate, breccia form from fragments squeezed together |
| fragmental | Refers to rocks or sediments composed of broken pieces or fragments of pre-existing rocks or minerals, often formed through physical weathering or volcanic activity (e.g., volcanic breccia or clastic sedimentary rocks). |
| fossil | The preserved remains, impressions, or traces of ancient organisms found in rocks. Fossils can include bones, shells, imprints, or even evidence of activity like footprints. |
| precipitates | Substances that form when minerals crystallize out of a solution, often due to changes in temperature, pressure, or chemical composition. |
| evaporates | Sedimentary rocks formed from minerals left behind after the evaporation of water, usually in arid environments. Common evaporite minerals include halite (rock salt) and gypsum. |
| lithification | The process through which sediments are compacted and cemented together over time, transforming them into solid sedimentary rock. |
| foliated | grains are thin, flat layering or bands Example: shale (sedimentary) undergoes heat and pressure being changed into slate (metamorphic) |
| nonfoliated | grains are randomly arranged Example: sandstone (sedimentary) is changed into quartzite (metamorphic) |
| banding | The alternating layers of different minerals or compositions found in metamorphic rocks, often created by heat and pressure causing minerals to segregate into distinct bands. |
| mineral alignment | The arrangement of minerals in a rock, typically seen in metamorphic rocks, where mineral grains are oriented in a parallel or layered pattern due to pressure and temperature during metamorphism. |
| Igneous rock | forms from cooling magma either below the surface or on the surface. |
| Metamorphic rock | forms when altered by heat, pressure or chemical reactions deep below earth’s surface. |
| Metamorphism | The transition to one rock from another rock in the solid state under conditions unlike those which they originally formed. |