Rivers Flashcards
abrasion (corrasion)
When rocks and silt carried along by the river wear down the river bed and bank
hydraulic action
When the motion of water against the rock produces gradual mechanical weathering of the river bed and banks
attrition
When rocks which are transported by the river smash together and break into smaller, smoother and rounder particles
solution (corrosion)
When small, soluble particles are dissolved into the river
traction
When the force of the water rolls large boulders along the riverbed (a river usually only has this much force in times of flooding)
saltation
When small pebbles and stones bounce along the riverbed as the river picks them up then drops them as they are too heavy to keep afloat
suspension
When fine light material (which can be kept afloat) is carried along with the water
solution
When minerals are dissolved in the water and carried along in solution (eg. salts)
pot holes & eddy currents
Boulders broken off by erosion sit on the river bed creating eddy currents as the water flows past since the river current is too weak to move the boulders by traction. The boulders swirl by the eddy currents, grinding a hole into the riverbed by abrasion.
alluvium
Alluvium is an extremely fertile soil that is very use full for planting crops, and in general farming. The alluvium is created from the river’s silt when it is piled layer upon layer during floods. This takes thousands of floods depositing the silt.
Angel Falls
Venezuela, 979 meters (19 times the height of the Niagara Falls!), highest waterfall in the world, source: upper tributary of Rio Caroni
aquifer
An underground layer of permeable rock, sediment or soil that provides water. The best aquifers are sandstones, unconsolidated gravels and permeable limestones. They can be a few square kilometers to thousands of square kilometers in size.
braiding
Braided channels are features that occur in the lower course of a river. The braids in the channel occur because of piles of sediment deposit that block the river from going in its natural course (shallow water). Therefore, because water chooses the path of least resistance, it goes around the pile of sediment and then rejoins the channel, thus the braiding. This forms islands in the river called eyots.
condensation nuclei
When tiny particles invisible to the human eye such as dust and dirt provide surfaces on which water molecules can condense and gather into water droplets.
condensation
The process by which water vapor in the air is changed into liquid water. Condensation is crucial to the water cycle because it is responsible for the formation of clouds. These clouds may produce precipitation, which is the primary route for water to return to the Earth’s surface within the water cycle. Condensation is the opposite of evaporation.
confluence
Where a smaller stream or river meets and joins a larger river.
Dams and reservoirs
A dam is any barrier that holds back water; dams are primarily used to save, manage, and/or prevent the flow of excess water into specific regions. In addition, some dams are used to generate hydropower. A reservoir is a man-made lake that is primarily used for storing water. They can also be defined as the specific bodies of water formed by the construction of a dam.
Deforestation
Deforestation is a term used to describe the removal of trees for many uses such as wood or open space for example. Deforestation can cause a very big problem when it comes to flooding. This is because if you don’t have trees, it is very hard for the water to be absorbed because there is nothing to absorb it. When there is no trees and a flood is present, the ground just has a lot of surface run-off.
Deltas
A land form at the mouth of a river, where the river flows into an ocean, sea or lake. Deltas are formed from the deposition of sediment carried by the river as it leaves the mouth of the river.
Deposition
Deposition is when a river that is containing things such as; rocks, sand, mud, etc drops the things it is carrying, when the speed of the river slows down, or if the volume of the river decreases. Deposition majorly occurs in floods, which then makes the land after the flood better for farming because the land is more fertile. The heavier objects deposit from the river first, and then the smaller object deposit after.
Dew point
The temperature at which water vapour in a specific volume of humid air condenses into liquid water, forming in this case precipitation such as rain and, after more cooling, snow.
Discharge
Discharge is the volume of water to flow at a give point on a stream bank per unit of time. It is usually expressed in cubic meters of water per second (m3/s). This is the volume rate of water flow which could include things such as dissolved chemical species, biological material and suspended solids (such as sediment). It is calculated by the equation: area of river cross section (calculated by adding up area of subsections (depth * width)) multiplied by the velocity
distributary
A branch of river that flow off from the main channel and does not rejoin it.
drainage basin
The area of land drained by a river.
dredging
When sand and gravel is removed from the coastline or seabed. It is a type of flood management, because now more water can go into the river, lake or sea because there is a smaller seabed.
evaporation
The change of state from water as a liquid into water vapour (a gas)
flood plain
The area around a river that is covered in times of flood. A floodplain is a very fertile area due to the rich alluvium deposited by floodwaters. This makes floodplains a good place for agriculture.
flood relief channels
A channel which redirects water away from the river during a flood to avoid there having civilian problems.
gorge
A narrow valley, with steep rocky walls, typically created by a waterfall receding back upstream when the soft rock is eroded, and carving deeper into the ridge above it.
groundwater flow
The sideways movement of water through the bedrock, which is typically an aquifer
through flow
The horizontal movement of water through the soil zone.
hydrological cycle
The process by which water moves through the landscape
impermeable rock
If river is in an area of impermeable rock, water can’t percolate into rocks so flows as surface runoff, increases discharge rapidly
infiltration
The movement of water into the soil layers
interception
Trees and other vegetation, which prevent moisture from reaching the ground directly
interlocking spurs
Water will always erode downwards and it will find the easiest way to get where it needs to go. This is how interlocking spurs are formed. The spurs themselves are the more resistant rock, so the water will erode around them into the softer rock creating winding passage ways called interlocking spurs. This feature is normally found in a V-shape valley.
land use planning
When you map out the flood plain. You then build cities further away from the river so that if a flood were to occur, then it wouldn’t do much damage. You would then put the farming fields up close to the river so that the land would pretty much always be fertile for growing crops. This concept is when you have a plan before you build so that you avoid more consequences than you would do if you didn’t plan out the region.
long profile
A diagram depicting the river in 3 stages: Upper course, middle course and lower course.