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27 Cards in this Set
- Front
- Back
bedding plane |
a nearly flat surface that separates two beds of sedimentary rock, each bedding plane marks the end of one deposit and the beginning of another having different characteristics |
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chemical sedimentary rock |
sedimentary rock consisting of material that was precipitated from water by either inorganic or organic means |
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detrital sedimentary rocks |
rocks that form from the accumulation of materials that originate and are transported as solid particles derived from both mechanical and chemical weathering |
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depositational environment aka sedimentary environment |
a geographic setting where sediment accumulates. each site is characterized by a particular combination of geologic processes and environmental conditions |
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graded bed |
sediment layer characterized by a decrease in sediment size from bottom to top |
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strate (beds) |
parallel layers of sedimentary rocks |
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classic texture |
a sedimentary rock texture consisting of broken fragments of preexisting rock |
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crystalline texture aka nonclastic texture |
a term for the texture of sedimentary rocks in which the minerals form a pattern of interlocking crystals |
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facies |
a portion of a rock unit that possesses a distinctive set of characteristics that distinguishes it from other parts of the same unit |
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lithification |
the process, generally involving cementation and/or compaction, of converting sediments to solid rock |
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salt flat |
a white crust on the ground that is produced when water evaporates and leaves behind its dissolved materials |
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turbidity curent |
a downslope movement of dense, sediment-laden water created when sand and mud on the continental shelf and slope are dislodged and thrown into suspension |
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biochemical |
a type of chemical that forms when material dissolved in water is evaporated by water-dwelling organisms. exa. shells |
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compaction |
a type of lithification in which the weight of overlying material compresses more deeply buried sediment. it is most important in the fine grained sedimentary rocks such as shale |
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diagensis |
a collective for all the chemical, physical, and biological changes that take place after sediments are deposited and during and after lithification |
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fissility |
the property of splitting easily into thin layers along closely spaced, parallel surfaces, such as bedding planes in shale |
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mud crack |
a feature in some sedimentary rocks that forms when wet mud dries out, shrinks and cracks |
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sediment |
unconsolidated particles created by the weathering and erosion of rock by chemical precipitation from solution in water or from the secretions of organisms and transported by water, wind and glaciers |
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bioturbation |
the reworking of soils and sediments by animals or plants. its effects include changing texture of sediments (diagenetic), bioirrigation and displacement of microorganisms and non-living particles |
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cementation |
one way in which sedimentary rocks are lithified. as material precipitates from water that percolates through the sediment, open spaces are filled and particles are joined into a solid mass |
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cross-bedding |
a structure in which relatively thin layers are inclined at an angle to the main bedding. formed by currents of wind or water |
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evaporite |
a sedimentary rock formed of material deposited from solution by evaporation of the water |
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fossil |
the traces or remains of organisms preserved from the geologic past |
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ripple marks |
small waves of sand that develop on the surface of a sediment layer by the action of moving water or air |
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sorting |
the degree of similarity in particle size in sediment or sedimentary rock |
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organic sedimentary rock |
sedimentary rock composed of organic carbon from the remains of plants that died and accumulated on the floor of a swamp exa. coal |
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organic reef |
sedimentary rock structure of significant dimensions erected by, and composed almost exclusively of the remains of corals, algae, bryozoans, sponges and other sedentary or colonial organisms |