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Flashcards about River Environments
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Upper Course
The section of a river that begins as narrow tributaries converging to form a V-shaped valley, characterized by steep gradients, rapid water flow, and significant vertical erosion.
Rapids and Waterfalls
Common features in the upper course of a river due to steep topography.
Middle Course
The section of a river where the channel becomes deeper and rounder, leading to increased erosion, widening of the channel, and development of floodplains.
Lower Course
The section of a river that carries the most substantial volume of water within a wide, deep channel, featuring levees and a shallower gradient.
Vertical Erosion
The process that deepens the riverbed, particularly in steep sections.
Lateral Erosion
The process that widens the riverbanks, creating more expansive channels.
Abrasion
The erosional process where rock fragments carried by the water scrape against the river channel.
Attrition
The erosional process involving colliding rocks and pebbles being broken down into smaller, smoother particles.
Hydraulic Action
The erosional process where the force of high-pressure water fractures and collapses riverbank material.
Corrosion (Solution)
The erosional process where certain minerals in rocks dissolve into river water, especially in acidic environments.
Solution (Transportation)
The transportation process where chemicals are fully dissolved in water and transported invisibly.
Suspension
The transportation process where tiny solid particles are held within the water and transported, often resulting in cloudy water.
Saltation
The transportation process involving larger pebbles that bounce along the riverbed.
Traction
The transportation process where large rocks and boulders are rolled along the riverbed.
River Deposition
The process that occurs when river water loses energy and velocity, leading to the dropping of its load.
Interlocking Spurs
Formations in the upper course where the river is forced around harder, resistant rocks, creating a zigzag pattern.
Waterfalls
Formations where there is a sudden change in rock resistance, causing water to cascade dramatically over ledges.
Gorge
A narrow valley with steep, rocky walls formed by the gradual erosion and retreat of a waterfall.
Meanders
Pronounced bends in a river, formed through lateral erosion on the outer bends and deposition of sand on the inner bends.
River Cliff
The outer bend of a meander where faster water flow leads to erosion.
Slip-off Slope
The inner bend of a meander where slower water allows sediment to accumulate.
Thalweg
The path of the fastest water flow in a river, providing insights into erosion and deposition patterns.
Ox-Bow Lakes
Crescent-shaped lakes formed when river meanders become severely eroded and sediment blocks the former bend.
Floodplains
Fertile areas that develop from sediment deposition during floods, making them suitable for agriculture.
Levees
Raised banks that protect against flooding, formed by sediment accumulation when the river overflows.
Estuaries
Depositional environments formed at river mouths where freshwater mixes with saltwater, creating diverse ecosystems.
Storm Hydrographs
Graphs that depict how river discharge changes over time in response to precipitation.
Peak Precipitation
The highest amount of rainfall recorded during a storm event.
Rising Limb
The phase where river discharge increases following rainfall.
Peak Flow
The maximum discharge measured after the peak rainfall.
Lag Time
The duration between peak rainfall and peak river discharge.
Falling Limb
The period during which discharge levels decrease as rain ceases.
Base Flow
The return to normal discharge levels post-rainfall.
Flash Floods
Floods that occur suddenly with little warning, associated with intense rainfall or rapid snowmelt.
Subdued Floods
Gradual floods resulting from prolonged rainfall events, allowing for more effective management.
Hard Engineering Solutions
Flood control strategies involving the construction of artificial structures like dams and levees.