The drainage area that supplies water to a river; the water comes from rainwater, which flows down the slope, and from underground water, which seeps into the river.
Drainage basin
Area drained by a river system
source
Place where a river begins
Mouth
Where the river flows into a sea or lake
Surface runoff
Rainwater flowing over the surface
Watershed
High ground separating one drainage basin from the adjacent drainage basin
stream or river network
Individual streams and rivers that are connected
Tributaries
Individual river channels forming the stream network
Confluence
Point where one river in the network joins another
Interfluves
Ridges of high ground between individual channels
Overland flow
Rainwater flowing over the surface
Channel flow
Water flowing in a river channel
Throughflow
Water flowing through the soil
Permeable rocks
Rocks that allow water to seep in
Groundwater
Underground water
Groundwater flow
Water flowing through underground rocks
Impermeable rock
Rock without pore spaces or cracks through which water is able to pass
Water table
Upper surface of the groundwater
Baseflow
Groundwater that seeps into a river
Permanent rivers
flow throughout the year because the water table is above the ground and constantly supplied with water
Periodic rivers
flow during periods of rainfall (the rainy season) only. The water table rises above the ground during the rainy season and forms these rivers.
Episodic rivers
These flow during periods of heavy rainfall only.
Exotic rivers
start in an area of high rainfall. There is a constant supply of water from their upper reaches and then they flow through semi-arid or arid areas.
Radial pattern
Develops on a dome where streams flow outwards and downhill
Trellis pattern
Forms on inclined strata that are unequally resistant to erosion, or in areas where there are parallel fold mountains
strata
Inclined rock layers
Rectangular pattern
Forms on igneous rock that has joints and crack; the streams develop right angled bends where joints meet
Centripetal pattern
Streams flow into a central pan or low-lying area
Dendritic pattern
Has a treelike appearanc; forms on rocks of similar hardness in an area with a similar gradient
Parallel pattern
Develops on a surface that slopes uniformly but is fairly steep; the river and its tributaries flow downslope nearly parallel to each other
Deranged pattern
no apparent drainage pattern
Drainage density
Total length of streams per unit area of a drainage basin
Stream order
The category of a stream in a network determined by the order of the streams feeding into it
Discharge
The amount of water flowing in a river channel past a point in a given time
Laminar flow
Water flowing in sheets; it does not change levels
Turbulent flow
Water flowing in a bubbling motion; it changes levels