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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

chemical sedimentary rock

sedimentary rock consisting of material that was precipitated from water by either inorganic or organic means

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

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

graded bed

sediment layer characterized by a decrease in sediment size from bottom to top

strate (beds)

parallel layers of sedimentary rocks

classic texture

a sedimentary rock texture consisting of broken fragments of preexisting rock

crystalline texture aka nonclastic texture

a term for the texture of sedimentary rocks in which the minerals form a pattern of interlocking crystals

facies

a portion of a rock unit that possesses a distinctive set of characteristics that distinguishes it from other parts of the same unit

lithification

the process, generally involving cementation and/or compaction, of converting sediments to solid rock

salt flat

a white crust on the ground that is produced when water evaporates and leaves behind its dissolved materials

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

biochemical

a type of chemical that forms when material dissolved in water is evaporated by water-dwelling organisms.


exa. shells

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

diagensis

a collective for all the chemical, physical, and biological changes that take place after sediments are deposited and during and after lithification

fissility

the property of splitting easily into thin layers along closely spaced, parallel surfaces, such as bedding planes in shale

mud crack

a feature in some sedimentary rocks that forms when wet mud dries out, shrinks and cracks

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

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

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

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

evaporite

a sedimentary rock formed of material deposited from solution by evaporation of the water

fossil

the traces or remains of organisms preserved from the geologic past

ripple marks

small waves of sand that develop on the surface of a sediment layer by the action of moving water or air

sorting

the degree of similarity in particle size in sediment or sedimentary rock

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

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