Hydrologic cycle
Illustrates the circulation of Earth’s water supply. Cycle is balanced
Processes involved in hydrologic cycle
Precipitation, Evaporation, Infiltration, Runoff, transpiration
Running water
Infiltration capacity controlled by
Factors that determine flow velocity
What is the head of stream like
- gradient decreases downstream
Factors that increase downstream
Factors that decrease down stream
- channel roughness
What is base level?
It is the lowest point a steam can erode to.
Lowering base level causes erosion.
Raising base level causes deposition
What is a streams load?
Transported material (sediment) in steam. Three types of load: - dissolved load - suspended load - bed load
Capacity
The maximum load of solid particles a stream Can transport per unit of time. The greater the discharge, the greater the steams capacity for hauling sediment.
Competence
A measure if a streams ability to transport particles based on size rather than quantity. Increases proportionally to the square of its velocity.
When does deposition if a steam occur?
When velocity is decreased. Competence is reduced. Sediments begin to drop and be come new layers of the stream.
Alluvium
Stream sediments
Channel deposits
Bars, braided streams, deltas
Floodplain deposits
- natural levees •form parallel to the stream channel • built by successive floods over many years - back swamps - yazoo tributaries
Alluvial fans
What are deltas?
Stream valleys
• The most common landforms on earths surface.
• There are two general types of stream valleys
-narrow valleys
- wide valleys
• Stream energy is directed from side to side forming a flood plain
Narrow valleys
Wide valleys
- downward erosion is less dominant
Flood plains
There are two different types
Meanders
Incised meanders
Meanders in steep, narrow valleys
- caused by drop in base level or uplift of land