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when sediments become glued together, they form |
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physical and chemical processes that break rock into rock & mineral fragments are |
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the removal and transport of sediment |
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wind, moving water, gravity, and & glaciers |
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four main agents of erosion |
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when minerals in rock are dissolved or chemically changed |
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minerals remain chemically unchanged rock fragments break off the solid rock along fractures or grain boundaries |
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when sediments transported by water & wind deposit in layers with largest grains/particles in the bottom layer |
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when a mix of sediments is "dumped in a pile" by glaciers & landslides |
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the physical & chem processes that transform sediments into sedimentary rocks; begins with compaction |
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bends rock grains together |
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commonly found in spaces between sand grains in sedimentary rock |
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groundwater, oil, & natural gas |
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when new minerals grow between sediment grains & glues them together into solid rock |
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examples of minerals formed in cementation |
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horizontal layering that ranges in thickness from a few mm. to several meters |
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bedding that shows heavier/courser particles in bottom layers |
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bedding formed as inclined layers of sediment that are deposited across a horizontal surface |
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small-scale cross-bedding |
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formed by migrating sand dunes |
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large-scale cross-bedding |
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small ridges of sediment formed by wind or wave reaction or by a river current |
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contain gravel-sized rock & mineral fragments, form any kind of rocks |
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course-grained clastic rocks |
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classification of clastic sedimentary rocks |
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contain rounded gravel pieces because they have traveled farther |
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contain angular gravel pieces because they have been deposited closer to their source |
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contain sand-sized rock & mineral fragments |
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medium-grained clastic rocks |
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percentage of open spaces between rock's grains |
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sandstone's porosity makes it valuable as underground reservoirs of |
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oil, natural gas, & groundwater |
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formed from deposits of loose sediments on Earth's surface; most common sedimentary rocks |
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evaporates most commonly form in arid (dry) regions & in areas of low water flow |
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formed from remains of once-living organisms |
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biochemical sedimentary rocks |
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most abundant biochemical sedimentary rock |
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many types of limestone contain |
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lithifies into the biochemical sedimentary rock chert |
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process that produces clastic sediments |
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