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Cards 1 – 14 → Sediment Transport & Formation Weathering, erosion, deposition, lithification, sorting, rounding, and grain size as energy indicators. Cards 15 – 20 → Sedimentary Structures Cross-bedding, ripple marks, graded bedding, mud cracks, and bioturbation — all clues to past flow and environmental conditions. Cards 21 – 28 → Environments & Processes Fluvial, deltaic, beach, and marine settings; turbidity currents and evaporites. Cards 29 – 35 → Composition & Identification Descriptions of clastic, chemical, and organic rocks — conglomerate, breccia, sandstone, shale, limestone, chert, coal. Cards 36 – 45 → Practice Quiz (Sedimentary Focus) Covers lithification, cross-bedding, energy levels, mud cracks, biological rocks, and identifying depositional structures.
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Sediment – Definition
Loose particles of rock, minerals, or biological material that are transported and deposited by wind, water, or ice.
Sedimentary Rock – Definition
Rock formed from the lithification of sediments through compaction and cementation.
Weathering – Definition
The physical and chemical breakdown of preexisting rocks into smaller particles or dissolved ions.
The removal and transport of sediments by wind, water, or ice.
The process where transported sediments settle out of the transporting medium.
The transformation of loose sediment into solid rock through compaction and cementation.
Process where sediment grains are pressed together under pressure, reducing pore space.
Minerals precipitate from groundwater and bind sediment grains together.
Form from the accumulation of fragments of preexisting rocks (detritus).
Form by precipitation of minerals from solution (e.g., limestone, halite).
Form from the accumulation of biological material such as plant remains (e.g., coal).
Describes the uniformity of grain sizes in sediment; well-sorted = consistent sizes, poorly sorted = mixed sizes.
Degree to which sediment particles have smooth edges; increases with transport distance.
Indicates energy of the depositional environment; coarse grains = high energy, fine grains = low energy.
Features that form during or shortly after deposition, providing information about past environments.
Inclined layers within a bed formed by wind or water currents; indicates direction of flow.
Small ridges formed by moving water or wind on a sediment surface.
Layer showing a vertical change in particle size from coarse at the bottom to fine at the top.
Polygonal cracks that form when muddy sediments dry and shrink.
Disruption of sediments by organisms such as worms or roots.
River and stream settings where sediments are transported and deposited by running water.
Where a river meets a standing body of water; sediments form deltas with layered deposits.
Wave-dominated setting where sand-sized sediments accumulate along shorelines.
Fine-grained clay and planktonic material settle slowly; often forms shale or ooze.
A dense, fast-moving underwater current carrying sediments down continental slopes.
A graded bed formed by turbidity currents, coarse at base, fine at top.
Mix of clastic and chemical sediments in shallow marine environments.
Chemical sedimentary rock formed by evaporation of water, leaving mineral deposits like halite or gypsum.
Clastic sedimentary rock with rounded gravel-sized clasts; indicates high-energy environments like rivers.
Clastic sedimentary rock with angular gravel-sized clasts; indicates deposition near source area.
Medium-grained clastic rock made of sand-sized particles; indicates moderate energy environments.
Fine-grained clastic rock formed from mud or clay; deposited in low-energy settings like deep water or floodplains.
Chemical or biological sedimentary rock composed mainly of calcite (CaCO₃).
Microcrystalline quartz formed by chemical precipitation or replacement; often found with limestone.
Organic sedimentary rock formed from compressed plant material in swampy environments.
Compaction and cementation (lithification).
Desert dunes or river channels.
Coarse-grained, poorly sorted sediments.
Periodic drying of wet environments, such as tidal flats.
Coal or some limestones.
Cross-bedding or ripple marks.
Larger grains = higher energy, smaller grains = lower energy.
Halite or limestone.
Shale.
Graded bedding (turbidites).