A | B |
Chemical Sedimentary Rock | Sedimentary rocks that are created from the dissolved substances and they precipitate back into the soil. |
Coarse-grained texture | Has crystals that are large and easy to see, most crystals are roughly the same size. These are usually formed underneath the Earth’s surface. |
Contact Metamorphism | Results when rocks form near large plums of magma that increases the heat applied to each rock. |
Crystallization | The process where magma cools and solidifies, either below or at a volcanic eruption at the surface. |
Detrital Sedimentary Rocks | Sedimentary rocks that are formed for the weathering of different rocks and then reformed. |
Disseminated Deposit | A deposit of metallic ions that are distributed in minute masses throughout an entire rock mass. |
Evaporate Deposit | Formed from the evaporation of water leaving minerals that solidify into different minerals. |
Extrusive (volcanic) | Igneous rocks that are formed because of a volcanic explosion. |
Fine-grained Texture | Has crystals that cannot be seen with out the unaided eye usually cooled quickly. |
Foliated Texture | Metamorphic rock that contains rock layers that are banded. |
Glassy Texture | The result of very rapid cooling of magma. |
Hydrothermal Solution | Created when hot, metal rich fluids containing metallic ions settle near the top of a magma chamber. |
Igneous Rock | Result from the crystallization of magma beneath the earths surface or in volcanic eruptions. |
Intrusive (plutonic) | Igneous rocks that are formed below the Earth’s surface and are can be seen as overlying layers are striped away. |
Lava | Magma that has reached the surface and lost its gaseous components. |
Lithification | Term meaning “conversion into rock.” |
Magma | Molten material that forms inside Earth. |
Metamorphic Rock | Rocks that created after being buried deep into the Earth’s surface and have intense heats and pressures applied. |
Non-Foliated | Metamorphic rocks that contain all of one mineral and are essentially a single crystal. |
Porphyritic Texture | Have some crystals which are much larger while other are much smaller and fine grain. |
Regional Metamorphism | Usually the result of mountain building where there are high scale deformations and high heat applied. |
Rock Cycle | Allow s us to view many of the interrelationships among different parts of the Earth’s system. |
Sediment | The deposition of rock materials that are weathered in either ocean, swamps, floodplains, or rivers. |
Sedimentary Rock | Created when sediment layers are compacted because of weight above and minerals fill in the pores spaces between with minerals. |
Strata (beds) | Different layers of sediment that are laid down on top of one another. |
Texture | Describes the overall appearance of an igneous rock, based on the size and arrangement of its interlocking crystals. |
Vein Deposits | Where fluids of rocks move between small cracks and leave behind metallic ions. |
Weathering | The day to day forces that decompose rocks into their constituent parts. |