Depositional Coast
A coastline characterized by wide sandy beaches, stream deltas, and an overabundance of sediment.
| Term | Definition |
|---|---|
Depositional Coast | A coastline characterized by wide sandy beaches, stream deltas, and an overabundance of sediment. |
Erosional Coast | A coastline characterized by an irregular shape, narrow beaches, and eroding headlands. |
Wave-Cut Terrace | A flat platform formed by wave erosion when waves erode a notch in a cliff causing it to collapse undercutting. |
Fjord | A drowned U-shaped valley carved by glaciers and flooded by rising sea levels. |
Drowned Karst | Limestone topography formed by chemical weathering and dissolution, which has been flooded by sea-level rise. |
Delta | A shoreline protuberance where a river meets the ocean and sediment builds out onto the continental shelf. |
Estuary (Drowned River Valley) | An embayment created when a river valley is flooded by sea level rise, trapping muddy sediments. |
Spit | An alongshore extension of a coast formed by sand piling up where the coastline ends. |
Barrier Island | A sandy, shore-parallel island separated from the mainland coast by a lagoon or tidal flat. |
Jetties | Structures built perpendicular to the shoreline at rivers or inlets to keep navigation passages open. |
Groins | Structures built perpendicular to a beach to trap sand, causing sediment to accumulate on the updrift side. |
Seawalls | Structures built for shoreline armoring to protect landward development from coastal erosion. |
Breakwaters | Structures built offshore, parallel to the shore, to protect the beach from waves and encourage sediment deposition behind them. |
Atoll | A ring-shaped coral reef system surrounding a lagoon, formed as a volcanic island subsides and erodes below sea level. |
Sediment Sorting | A measure of how similar grain sizes are within a sediment or rock, reflecting changes in system energy. |
Graded Bedding | A layer of sediment where grain size changes vertically, being coarser at the bottom and progressively finer toward the top. |
Cross-Bedding | Inclined layers of sediment formed as sand avalanches down the lee slope of dunes or ripples, indicating flow direction. |
Symmetric Ripples (Wave-Oscillation Ripples) | Ripples formed by oscillatory wave motion in shallow water, featuring sharp crests and equal slopes on both sides. |
Asymmetric Ripples (Current Ripples) | Ripples formed by unidirectional wind or water currents, featuring a gentle stoss slope and a steep lee slope. |
Mudcracks | Polygonal patterns of cracks formed in very fine-grained sediment as it dries and contracts. |
Bioturbation | The disturbance of sediment layers by biological activity, such as animals or plants burrowing. |
Alluvial Fan | A fan-shaped deposit of poorly sorted, coarse sediment flowing out of mountains via high-energy floods or mudflows. |
Point Bar | An area of sediment deposition on the inside bend of a meandering river. |
Cutbank | An erosional bank located along the outside of a meandering river bend. |
Oxbow Lake | A U-shaped body of water formed when a meandering river takes a shortcut and cuts off a tight bend. |
Sediment Roundness | A measure of how sharp or smooth the corners and edges of a sediment grain are, with higher roundness indicating a longer transport distance. |
Sediment Sphericity | A measure of how closely a sediment particle approaches the geometric shape of a sphere. |
Sediment Maturity | A measure of sediment transport and weathering progress, characterized by stable minerals like quartz, well-rounded grains, and high sorting. |
Beach Slope Dynamics | The relationship where coarser sediment grains create steeper beach slopes due to high water infiltration, while finer grains result in flatter slopes due to increased backwash. |
Phaneritic Igneous Texture | An igneous rock texture characterized by large, mineral crystals that are easily visible to the naked eye, formed by slow cooling beneath Earth's surface. |