Rivers Flashcards
Surficial Processes
- erosion
- transportation
- deposition on the Earth’s surface (or near surface)
Landscapes are constantly created and destroyed
Agents of Surficial Processes
- running water (streams and drainage systems)
– groundwater
– glaciers
– gravity (mass wasting)
– wind
Streams and Drainage Systems
Stream any flowing body of water, regardless of size.
River a major branch of a large stream system
Channel the stream passage way
Discharge the quantity of water passing a given point
Load the sediment carried by the stream
Stream Loads and Sediment Movement
- Solution load (dissolved material)
- Suspended load (silt and clay)
- Bed load (sand and gravel) a) rolling, b) sliding or traction, c) saltation
Factors the affect stream flow
1) Gradient ->the amount the stream falls between two points (change in elevation/distance between two points)
2) Discharge ->the amount of water that passes down the river (m3/s)
->cross-sectional area x average velocity
3) Velocity
4) Sediment load
Dendritic Drainage Patterns
Moderate slopes and rocks and soil of uniform resistance.
Parallel Drainage Patterns
Parallel drainage patterns form where there is a pronounced slope to the surface. A parallel pattern also develops in regions of parallel, elongate landforms like outcropping resistant rock bands
Trellis Drainage Patterns
Form in areas of hard and soft rock formations exist. Large streams occur in less resistant rocks and the smaller streams cur more resistant rocks in the higher ground
e.g., folded sedimentary sequences.
Rectangular Drainage Patterns
Typical of little topography and bedrock with uniform resistance and orthogonal joint sets being planes of weakness and more easily eroded.
Radial Drainage Patterns
Occurring on isolated topographic uplands such as volcanoes, domes and buttes
(steep-sided, flat-topped towers of rock)
Two Types of Water Flow in Streams
- Laminar Flow
low velocities
the fluid particles follow the streamlines - Turbulent Flow
higher velocities
the flow breaks up into a fluctuating velocity pattern or eddies (streamlines cross)
Two types of floodplains
- Braided Rivers: have numerous channels that repeatedly divide and merge
- Meandering rivers: consist of a single main channel that bends and loops
Flood Plains
a flat region of a valley floor located on either side of a stream channel, common location for
meandering streams
is built of sediments deposited by the stream that flows through it and is covered by water
during floods
floodplains tend to develop on the less steep sections of streams.
Types of Stream Deposit Types
- FloodPlains
- Levees
- Terraces
- Alluvial Fans
- Delta