Lab 11:
Stream Processes and Landscapes
Objectives:
- Stream Processes:
- Drainage divides & basins
- Trunk vs. tributary streams
- 3 channel types (straight, braided, meandering)
- Stream gradient (should be review from topo lab)
- Characteristics upstream vs. downstream
- Alluvium
- Delta vs. Alluvial fan
Introduction:
Perennial streams: flow continuously during the year
Intermittent streams: flow only during certain times of the year
Flood: overflowing the banks of a stream or river
Land erosion: wearing away of the land through stream processes
Alluvium: sediment transported and deposited by streams and rivers, consists of gravel,
sand, + mud deposited in floodplains, point and channel bars, deltas and alluvial fans
Stream Processes and Landscapes:
Sheetflow: sheets of water several millimeters or centimeters deep
Figure 11.1 - Stream drainage system: sheetflows merge to form streams (headwaters,
tributaries), rivers (trunk), lakes and oceans
Drainage patterns: characteristic patters of drainage, controlled by relief and geology
Figure 11.2 - Dendritic, Rectangular, Radial, Centripetal, Annular, Trellis, Deranged
Figure 11.1 - Drainage basin: entire area drained by one stream, or an entire stream
drainage system
Divides: lines separating drainage basins (i.e. continental divide)
Weathering: physically erodes and disintegrates or chemically decomposes or dissolves
Earth materials
Transport and deposition: dependent on stream velocity and grain size
Valley Forms and Processes:
Form and shape controlled by: geology, gradient, base level (lowest level to which a
stream can theoretically erode), discharge (rate of stream flow at a given time and location), load (amount of sediment that is transported)
Figure 11.1 - Floodplains, meandering, cutbanks, point bar, oxbow lake, braided stream,
channel bars, stream terraces, delta, alluvial fan