New clastic coasts
Clastic Coasts Part 2
Overview
Focuses on various coastal and sedimentary systems.
Emphasizes deposition processes and coastal morphologies.
Deposition Systems
Definition
Depositional system: Collection of process-related sedimentary facies assemblages, informed by geography.
Examples: Nearshore, deep marine, glacial, and fluvial depositional systems.
Importance: Modern systems help in interpreting ancient sedimentary records.
Marine Depositional Systems
Types
Wave-dominated coasts
Tide-dominated coasts
Fluvial-dominated coasts (deltas)
Carbonate reefs
Clastic shelves & platforms
Carbonate shelves & platforms
Deepwater fans
Pelagic abyssal plains
Clastic Depositional Systems
Types
Terrestrial
Transitional
Marine
Characteristics: Dominated by sedimentary structures like graded beds and facies represented by highstand, lowstand, etc.
Shows the interface between land and sea in dynamic environments.
Coastal Types
Coastal Morphology
Increasing tidal and wave power influences coastal types: strand plains, barrier islands, and deltaic formations.
Types defined by sediment supply and wave/tide influence.
Beach Systems
Characteristics
Sediments coarsen upward from marine shales.
Linear sand bodies formed by waves and tidal currents.
Various facies identified: well-sorted quartz arenites, offshore hummocky bedding, cut and fill structures.
Faunal distribution: marine at the base, terrestrial at the crest.
Vertical Stacking in Shoreline Sediments
Prograding Coastal Plain
Holistic view of sediment integration over time.
Influence of sea level changes on sedimentation patterns.
Coastal Systems and Features
Types
Coastal plain, sandstone, and mudstone formations.
Characteristics: burrows, planar beds indicative of environmental conditions, foreshore & delta front structures.
Combinations of terrestrial and marine influences observed in sequence.
Deltaic Systems
Characteristics
Form where rivers meet standing water, offering large sediment influx.
Features: mix of fluvial, tidal currents, and storm influences.
Typical delta types based on tidal range, wave climate, and basin characteristics.
Processes in Deltaic Systems
Key Influences
Inertia, friction and buoyancy determined by water density and sediment interaction.
Different deltaic forms arise based on the dominance of these processes leading to various depositional traits.
Lake Systems
Characteristics
Lakes as sediment traps influenced by terrestrial input, internal morphology, and climatic conditions.
Lake sediments typically show a varying character from clastics & organics to evaporites.
Glacial Systems
Features
Glacial systems indicate climatic extremes with clear sedimentological signatures.
Glacial deposits like till and stratified sequences reveal evidence of historical ice coverage and melting trends.
Aeolian Systems
Characteristics
Presence in deserts with notable dust, loess deposits, and dune formations.
Role of wind in the transport of sediments, shaping the landscape through processes of erosion and deposition.
Conclusion
Understanding sedimentary systems is crucial for reconstructing past environments and predicting geological behavior under varying climatic conditions.