What is another term for Stream Processes?
Fluvial Processes
What is a stream?
Any area of channeled water flow
What is Sheet Flow?
over-land flow (spread out, even depth)
What is Stream Flow?
concentrated flow into a direct channel
What are Fluvial Processes?
a stream’s ability to shape a landscape, depending on CAPACITY and COMPETENCY
Define Capacity
total amount of material that the stream can move *depends on discharge- volume of water moving out.
Higher discharge = higher capacity
Define Competency
the size of material that can be carried by the stream
*depends on stream velocity.
Higher velocity = higher competency
Arises from kinetic energy- stream flow converts potential energy into kinetic energy (movement)
What is the Stream Gradient?
Stream Steepness, related to kinetic energy
Gradient = Steepness
What is the Base Level?
Level below which a stream cannot erode its valley
Ultimate base level = the ocean
Local base level = a local limit to erosion, such as a lake or resistant rock layer
Describe Stream Energy
Ability of a stream to erode and transport materials is dependent on its total amount of energy.
-Influenced by velocity, volume of water.
Energy used for erosion is not available for transportation and vice-verse
What is Stream Erosion?
Hydraulic action (movement of materials through pressure and shearing force) + Abrasion (mechanical erosion of stream bed by waters or solids in the stream) -occurs with both stream and sheet flow
What are the 3 types of stream transportation?
Solution Load
Suspended Load
Bed Load
Solution Load
Material dissolved and carried in stream (usually through chemical weathering)
“Kool-Aid” - dissolved throughout
Suspended Load
Small, clastic particles held aloft in water, with the energy of the water keeping them suspsended
Bed Load
Material pushed along the bottom by the water’s energy (rolling, bouncing along the bottom of the stream)
Saltation: skip/bounce
Traction: sliding along the bottom
Describe Deposition
Occurs when stream energy is no longer sufficient to transport load, results in sorting based on sizes.
-dramatic decrease in energy
-deposits/dumps material
(largest things drop first)
Braided rivers
river split into different channels (multiple, interwoven)
-more materials than the stream has the capacity to transport
Meandering Streams
The river’s form changes as undercuts and point bars migrate (curves = meanders)
-outside of the river has more energy at turns, inside is moving slower)
Inside = deposition
Where do deltas form?
At the end of streams
What are Nickpoints?
Hard rock on top of softer rock
What are graded streams?
Graded streams have reached a balance between erosion, transportation and deposition
-when uplift occurs, streams can return to active periods of down cutting.