Final For Lecture Class Flashcards
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
- Begins as sheet flow
Infiltration capacity controlled by
- intensity and duration of the rainfall
- prior wetted condition of the soil
- soil texture
- slope of the land
- nature of the vegetative cover
Factors that determine flow velocity
- Channel Gradient or slope
- channel characteristic. (Shape, size, roughness)
- amount of water flowing in the channel
What is the head of stream like
- Profile is a smooth curve
- gradient decreases downstream
Factors that increase downstream
- velocity
- discharge
- channel size
Factors that decrease down stream
- gradient or slope
- 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
- develop where a high- gradient stream leaves a narrow valley
- slopes outward in a broad arc
What are deltas?
- forms when a steam enters an ocean or lake
- consists if three types of beds
•Forest beds • topset beds •bottom set beds
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
- V-shaped
- down cutting toward base level
- features often include rapids and or waterfalls
Wide valleys
- stream is near base level
- downward erosion is less dominant
Flood plains
There are two different types
- erosional flood plains
- depositional flood plains