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Lab 8 Stream Processes. Channel Types Braided - steeper, large sediment supply Meandering - less steep, lower sediment supply.

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Presentation on theme: "Lab 8 Stream Processes. Channel Types Braided - steeper, large sediment supply Meandering - less steep, lower sediment supply."— Presentation transcript:

1 Lab 8 Stream Processes

2 Channel Types Braided - steeper, large sediment supply Meandering - less steep, lower sediment supply

3 Terminology Flood – river overflows its banks Alluvium – stream deposits Drainage system – network of streams and rivers that drain a given area of land Many types of drainage patterns (e.g., dendritic, rectangular, trellis, etc.)

4 Drainage Patterns

5 Drainage Basins and Divides Drainage basin – area of land drained by one stream Divides – linear boundaries that separate one drainage basin from another. –Continental divide: Rocky Mts.

6 Stream Processes Weathering –Dominant process upstream –Headward erosion – streams erode into V- shapes uphill. –Erode their own valleys and channels Transport Deposition –Dominant process downstream –Velocity decreases and sediment dumped

7 River Valley Forms and Processes Gradient – steepness of slope Gradient = (height)/(distance) Base level – lowest level to which stream can theoretically erode –Imaginary line between erosion and deposition Discharge – rate of stream flow at a given time and location Load – the amount of material that is transported by a stream (mostly sediment)

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9 River Forms Cutbanks Point bars Oxbow lake Delta Alluvial fan


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