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Geology
Kehir - Rocks and Minerals
Term | Definition |
---|---|
absolute age | Age, in years, of a rock or other object; can be determined by using properties of the atoms that make up materials. |
alloy | mixture of two or more minerals, with at least one being metallic |
basaltic | Describes dense, dark-colored igneous rock formed from magma rich in magnesium and iron and poor in silica. |
carbon film | Thin film of carbon residue preserved as a fossil. |
cast | A type of body fossil that forms when crystals fill a mold or sediments wash into a mold and harden into rock. |
cementation | Sedimentary rock-forming process in which sediment grains are held together by natural cements that are produced when water moves through rock and soil. |
cleavage | A mineral's ability to split easily along flat surfaces. |
compaction | Process that forms sedimentary rocks when layers of sediments are compressed by the weight of the layers above them. |
coral reef | A structure of calcite skeletons built up by coral animals in warm, shallow ocean water. |
crystal | A solid in which the atoms are arranged in a pattern that repeats again and again. |
crystallization | The process by which atoms are arranged to form a material with a crystal structure. |
deposition | Process in which sediment is laid down in new locations. |
erosion | A process in which the materials of Earth's surface are loosened, dissolved or worn away and transported from one place to another by a natural agent, such as wind, water, ice or gravity. |
extrusive | Describes fine-grained igneous rock that forms when magma cools quickly at or near Earth's surface. |
foliated | Describes metamorphic rock, such as slate and gneiss, whose mineral grains line up in parallel layers. |
fossil | Physical evidence of an organism that lived long ago that scientists use to study the past; evidence may appear in rocks, amber, or ice. |
fracture | The way a mineral looks when it breaks apart in an irregular way. |
geode | A hollow rock inside which mineral crystals have formed. |
granitic | Describes generally light-colored, silica-rich igneous rock that is less dense than basaltic rock. |
half-life | Time it takes for half the atoms of an isotope to decay. |
igneous rock | Rock formed when magma or lava cools and hardens. |
index fossils | Remains of species that existed on Earth for a relatively short period of time, were abundant and widespread geographically, and can be used by geologists to assign the ages of rock layers. |
inorganic | A substance not having the structure or organization characteristic of living bodies. |
intrusive | Describes a type of igneous rock that generally contains large crystals and forms when magma cools slowly beneath Earth's surface. |
lava | Liquid magma that reaches the surface; also, the rock formed when liquid lava hardens. |
luster | The way a mineral reflects light from its surface. |
magma | The molten mixture of rock-forming substances, gases, and water from the mantle. |
metamorphic rock | Forms when heat, pressure, or fluids act on igneous, sedimentary, or other metamorphic rock to change its form, composition, or both |
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. |
mold | A type of body fossil that forms in rock when an organism with hard parts is buried, decays, or dissolves and leaves a cavity in the rock |
non foliated | Describes metamorphic rock, such as quartzsite or marble, whose mineral grains grow and rearrange but generally do not form layers. |
ore minerals | valuable minerals that are economically worthwhile to extract |
permineralized remains | Fossils in which the spaces inside are filled with minerals from groundwater. |
placer deposits | surface deposits of minerals created by weather and erosion of rocks |
placer mining | method used to extract minerals from stream bends and along coasts |
principle of superposition | States that in undisturbed rock layers, the oldest rocks are on the bottom and the rocks become progressively younger toward the top. |
radioactivity decay | Process in which some isotopes break down into other isotopes and particles. |
radiometric dating | Process used to calculate the absolute age of rock by measuring the ratio of parent isotope to daughter product in a mineral and knowing the half-life of the parent. |
reclamation | the process of restoring a mine that is no longer used for mineral extraction |
relative age | The age of something compared with other things. |
rock | A naturally occurring solid mixture of one or more minerals or organic matter. |
rock cycle | The series of geologic processes in which a rock forms, changes from one type to another, is destroyed, and forms again. |
sediment | Small, solid pieces of material that come from rocks or organisms; earth materials deposited by erosion. |
sedimentary rock | Forms when sediments are compacted and cemented together or when minerals form from solutions. |
solution | A mixture in which one substance is dissolved in another. |
streak | The color of a mineral's powder. |
subsurface mining | tunneling method used to extract ores when they are located at least 50 meters below the surface |
surface mining | method used to remove ores from surface deposits |
texture | The quality of a rock that is based on the sizes, shapes, and positions of the rock's grains. |
unconformoity | Gap in the rock layer that is due to erosion or periods without any deposition |
uniformitarianism | Principle stating that Earth processes occurring today are similar to those that occurred in the past. |
valley fills | earthen dams created with waste rock from surface mining |
vein | A narrow deposit of a mineral that is sharply different from the surrounding rock. |
gem | Beautiful, rare, highly prized mineral that can be worn in jewelry. |
ore | Deposit in which a mineral exists in large enough amounts to be mined at a profit. |
composition | The chemical makeup of a rock; describes either the minerals or other materials in the rock |