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A set of vocabulary flashcards covering fluvial systems, sediment transport, coastal dynamics, and geologic climate proxies based on the lecture material.
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Laminar Flow
A type of flow where water moves in parallel, non-crossing streamlines, which is rarely found in open channels.
Turbulent Flow
Water flow characterized by chaotic, crossing streamlines and continuous mixing, which is highly efficient at eroding channels and keeping sediment in suspension.
Bed (Traction) Load
Coarse particles like boulders and gravel that roll or slide along the river bottom without leaving the substrate.
Saltating Load
Sand-sized grains that move by bouncing or hopping along the stream bed.
Suspended Load
Fine silt and clay particles that are kept aloft by turbulent eddies within the water column.
Dissolved Load
Soluble ions carried in chemical solution within a stream.
Competence
A metric measuring the maximum particle size a stream can carry, which is determined by the stream's velocity.
Capacity
A metric measuring the total volume of sediment a stream can transport, determined by the stream's discharge.
The Thalweg
The path of fastest water velocity within a channel, which swings to the outside of river bends and dictates where erosion occurs.
Cut Banks
The outer bank of a river loop where dynamic erosion occurs due to high water velocity.
Point Bars
The inner loop of a river bend where deposition occurs because the water slows down.
Oxbow Lakes
Crescent-shaped lakes that form when the neck of a meander is breached and then abandoned.
Graded Stream
A river system in dynamic equilibrium where sediment delivered=sediment removed, characterized by a concave-up profile.
Base Level
The lowest elevation to which a stream can erode, typically represented by sea level.
Stream Terraces
Stranded, incised former floodplains left behind after a river adjusts to profile disruptions.
Alluvial Fans
Fan-shaped aprons of coarse sediment dropped by ephemeral streams exiting steep mountain fronts onto flat plains.
Deltas
Tri-part sedimentary wedges formed where a river drops its sediment load as it enters a standing body of water like an ocean or lake.
Wave Base
The depth below which orbital wave motion vanishes, roughly equal to 21 the horizontal wavelength.
Refraction
The bending of wavefronts as they slow down in shallow water, focusing energy onto headlands and dissipating it in bays.
Longshore Drift
The shore-parallel transport of sand caused by waves striking the beach at an angle, involving incoming swash and gravity-driven backwash.
Spring Tides
Extreme tidal ranges that occur during full or new moons when the gravitational forces of the Moon and Sun reinforce each other.
Tsunamis
Long-period waves generated by sudden sea floor displacements, such as megathrust earthquakes, which grow into high-amplitude walls of water in shallow areas.
Thermohaline Circulation
A global "ocean conveyor belt" driven by density differences resulting from water temperature (thermo) and salinity (haline) variations.
Recurrence Interval (R)
The statistical average time elapsed between floods of a given size, such as a "100-year flood" having a 1% annual chance.
Greenhouse Effect
The process where greenhouse gases like H2O, CO2, and CH4 capture and reflect longwave, infrared radiation back to Earth, warming the lower atmosphere.
Benthic Foraminifera
Deep-sea organisms that build calcium carbonate CaCO3 shells using oxygen from seawater, providing climate proxies through 18O/16O ratios.
Eccentricity
A Milankovitch cycle lasting approximately 100,000 years where the shape of Earth's orbit alternates between nearly circular and mildly elliptical.
Obliquity (Tilt)
A Milankovitch cycle lasting approximately 41,000 years involving the tilt angle of Earth's axis, ranging from 21.5∘ to 24.5∘.
Precession
A Milankovitch cycle lasting approximately 23,000 years involving the wobble of Earth's axis, which changes the seasonal timing of perihelion and aphelion.