
Discover sedimentary structures and textures, classify primary, secondary, inorganic, and organic types, and identify top, bottom, and within-bed features like ripple marks and desiccation cracks to infer deposition.
Explore sedimentary structures formed within beds, including mud cracks and desiccation features, model X and pseudo structures, cross-bedding types, lenticular bedding, and related stratification patterns.
Learn about bottom sedimentary structures, or sole marks, formed by erosional and depositional processes, and identify directional indicators like cross-bedding and curved marks that reveal flow direction.
Explore conglomerate types, including auto-conglomerates with glass in contact, open vs closed framework, and matrix vs glass-supported structures; assess transport distance, competence, and deduced transport mechanisms.
Learn how clastic rocks are classified by textural maturity, including sorting, roundness, and matrix, with compositional maturity, mineral stability, provenance and tectonic settings, and turbidites.
Explore diagenesis, lithification, and cementation, detailing burial processes—compaction, differential compaction, dissolution, precipitation, and replacement—and how cements shape porosity and permeability.
Explore shallow marine environments, carbonate production, reef types, and ramp forms on the continental shelf. Examine deep marine sedimentation driven by turbidity currents, debris flows, submarine canyons, and accommodation space.
Explore porosity and permeability in sedimentary rocks, covering primary and secondary porosity, granular and micro porosity, and dissolution or fracture porosity, plus total and effective porosity concepts.
Describe the Bouma sequence formed by turbidity currents on steep submarine slopes, showing coarser bottom to finer top sediments and related features like ripple laminations and flame structures.
Explore the classification of stylolites by bedding relation and geometry, detailing horizontal, inclined, vertical, cross-cutting and interconnected types, microsatellites, wispy and solution seams, amplitude, contact features, and sedimentary environments.
Analyze sedimentary basins through subduction geometry, margins, and arc settings, including back-arc and forearc scenarios. Integrate stratigraphy, subsidence, thermal history, and geophysical data to interpret basin evolution.
Understand Reynolds and Froude numbers, geometric and logarithmic grain size scales, and viscosity relations to distinguish laminar, transitional, and turbulent flow and associated sedimentary structures.
Learn to compute sediment particle sphericity and roundness using six times the particle volume over the sphere diameter, with cylinder, cube, and hemisphere numerical examples.
Explore lagoons as transitional coastal environments, their formation, types (coastal and atoll lagoons), and how sedimentary textures—grain size, sorting, and shape—reveal transgression, regression, and depositional history.
Explore transitional marine environments and deltas, including river-dominated bird-foot deltas, tidal-dominated deltas, and Gilbert-type deltas, along with sediment supply, river-mouth morphology, and tidal processes.
Explore dolomitisation processes, replacement and crystallization in carbonates, and compare mixing-zone, reflex, burial, and seawater models for dolomite formation.
Explore sandstone classification using ternary quartz–feldspar–lithic diagrams, assess matrix content, sorting, and textural maturity to identify clastic rock types.
Learn how sedimentary environments—from continental to deep marine—are controlled by sediment sources, transport processes, and accommodation space, with emphasis on shallow marine dynamics and storm-related structures.
Explore secondary chemical sedimentary structures, including concretions and skylights, formed by pressure solution and groundwater-driven mineral precipitation in limestones, with geometric classifications and porosity controls.
Sedimentology, scientific discipline that is concerned with the physical and chemical properties of sedimentary rocks and the processes involved in their formation, including the transportation, deposition, and lithification (transformation to rock) of sediments. The objective of much sedimentological research is the interpretation of ancient environmental conditions in sediment source areas and depositional sites. Sedimentologists study the constituents, textures, structures, and fossil content of the deposits laid down in different geographic environments. By these means they can differentiate between continental, littoral, and marine deposits of the geologic record. Importance of sedimentary rocks.
Sedimentary rocks provide a multitude of products which modern and ancient society has come to utilise.
Art: marble, although a metamorphosed limestone, is an example of the use of sedimentary rocks in the pursuit of aesthetics and art
Architectural uses: stone derived from sedimentary rocks is used for dimension stone and in architecture, notably slate, a meta-shale, for roofing, sandstone for load-bearing buttresses
Ceramics and industrial materials: clay for pottery and ceramics including bricks; cement and lime derived from limestone.
Economic geology: sedimentary rocks host large deposits of SEDEX ore deposits of lead-zinc-silver, large deposits of copper, deposits of gold, tungsten, Uranium, and many other precious minerals, gemstones and industrial minerals including heavy mineral sands ore deposits
Energy: petroleum geology relies on the capacity of sedimentary rocks to generate deposits of petroleum oils. Coal and oil shale are found in sedimentary rocks. A large proportion of the world's uranium energy resources are hosted within sedimentary successions.
Groundwater: sedimentary rocks contain a large proportion of the Earth's groundwater aquifers. Our understanding of the extent of these aquifers and how much water can be withdrawn from them depends critically on our knowledge of the rocks that hold them (the reservoir).