Geomorphology Flashcards
Abrasion
Particles of sand and silt that are carried by the river scratch an wear aqua the bed and sides of the channel
Abstraction
Process whereby the watershed becomes lower and its position shifts
Aerated zone
Part of crust above the water table where there are open air spaces
Alluvium
fertile silt deposited by a river
Attrition
Small particles bump against one another and become smaller, rounder and smother
Antecedent drainage pattern
After the river formed, folding and faulting occurred, but the river maintained is pattern, cutting a gorge/ poort/ gap through the land that has been uplifted
Baseflow
Ground water that seeps into a river
Braided streaks
Rivers that have multiple channels and islands of alluvial sediment in between those channels
Captive stream
Less energetic river that was captured by the captor river
Captor stream
More energetic river that eroded through the watershed and captured another river
Catchment areas
The are that feeds water into a river system
Channel flow
Water flowing in a river channel
Confluence
Point where one river in the network joins another
Corrosion
Acids in the water can dissolve the rock particles
Delta
Depositions feature that forms when a river enters the sea or a still body of water
Direct runoff
Water flowing over earth in river channels
Discharge
Amount of water flowing in a river channel past a point in a given time
Drainage basin
And area drained by a river and its tributaries
Drainage density
The total length of all the streams and rivers in at raise drainage basin (KM) divided by the total area of the drainage basin (KM squared)
Elbow of capture
Point where capture occurred; The captive changes direction and flows into the captor
Entrenched or incised meanders
A meander that has cut (vertically) deep into the crust
Episodic rivers
Rivers that hardly ever flow because they are in low rainfall areas and the water table is always a load of riverbed
Erosion
The wearing away and removal of weathered rock material from the river channel
Exotic rivers
Rivers found in low rainfall areas but flow all year round because they are fed by tributaries in high rainfall areas
Floodplain
Flat valley floor
Gorge
Deep-steep sided valley
Graded river
A river that has just enough energy to carry it to load; neither erosion nor deposition is taking place resulting in a smooth, concave longitudinal profile
Groundwater
Underground water
Groundwater flow
Water flowing through underground rocks
Headward erosion
A river lengthens itself by cutting back towards it source
Hydraulic action
The force of water hitting the side and the bed off the river will break pieces off
Impermeable rock
Rock which does not allow water to pass through it
Indirect runoff
Water feeding into rivers through base with
Ingrown meanders
A meander that cuts sideways into the bank so that there is slight overhang above the stream
Interfluves
Ridges of high ground between individual channel
Knickpoint
Sharp change in gradients along the course of the river located at the old sea level after isostatic uplift or a drop in sealevel has occurred
Knickpoint waterfall
A waterfall created by a sharp change in gradient
Lag time
The period between maximum precipitation and peak discharge
Laminar flow
Water flowing smoothly in sheets with no vertical mixing
Lateral erosion
Horizontal erosion (of the sise) of a river channel making it wider
Load
Broken rock particles and other materials carried by a river
Levees
Raised banks of the river
Longitudinals profile
A visual representation of the gradient down which a river flows
Meanders
Bends in the river channel
Meander scars
Dried up ox-bow lakes
Misfit/beheaded stream
part of the river that have lost it head waters
Mouth
Point at which the river flows into the sea
Non-porous rock
Rocks that does not have pore spaces, therefore water cannot seep into the rock
Over graded rivers
Reverse that have Excess energy and therefore erode their channels
Oxbow lakes
A meander that is cut off when the river takes a new course across the neck off a meander loop
Periodic river/ non-perennial
Rivers that only flow during the rainy season when the water table is higher
Permanent base level
Sea level, the lowest level to which a river will erode the land
Permanent rivers/ perennial
Rivers that flow all year because the river bed is deeper than the water table all year
Permeable roadie
Rocks that allow water to pass through it
Porous
A rock which has pore spaces into which water can seep
Rapids
A resistant layer of rock causes slight changes in gradient and turbulent flow within a river
Rejuvenated river
A river receives additional energy and begins to erode vertically
Riparian zone
Area alongside a river
River capture
A process of one river capturing water from another stream
River cliff
Steep river bank, due to erosion, in the outside Bend of a meander
River network/system
A river and all its tributaries that flow into it
River terraces
Steps that show the level of the valley floor prior to rejuvenation
Saltation
Smaller rocks and stones are bounced along the river bed
Saturated zone
Part of the crust where all the air spaces are filled with ground water
Sheet flow
Water flowing downstream in thin sheets
Slip-off-slope
Gentle river bank, due to deposition, on the inside bend of a meander
Source
Place where a river begins
Spurs
Ridges of high ground between individual channels
Strata
Rock layers
Stream order
The category of a stream in a network determined by the order of the streams flowing into it
Superimposed drainage pattern
A river develops a pattern on a surface that has eroded over time, so now the river is flowing in the older rocks or structures that have been uncovered
Surface runoff
Rain water flowing over the surface
Suspension
Silt and very small particles are carried within the flow of the water
Temporary base level
Changes in the gradient along a course of a river where vertical erosion of the river is slower
Throughflow
Water is flowing through the soil
Traction
Boulders and large rocks are pushed and rolled along a river bed
Transpiration
Water loss from pants through the pores in their leaves
Tributaries
Individual river channels forming the stream network
Turbulent flow
Water flowing in a bubbling motion; with lots of vertical movement
Undercutting
The force of water eroded the base of the banks creating a notch and eventually causing the bank to collapse
Under-graded rivers
Rivers that do not have enough energy to flow and to transport their load; they will deposit some of their load
Valley within a valley
Rejuvenated river begins to erode a new valley within the old one
Velocity
Speed of river
Vertical erosion
Erosion downwards, cutting deeper into the landscape
Waterfalls
A place where water flows over a vertical drop in the course of a river
Watershed
High ground separating one drainage basin from the adjacent drainage basin
Water table
The upper surface of the groundwater
Wind tap
The part of the original river valley, between the elbow and misfit, now dry and filled with deposited gravel