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Streams and Watersheds

Streams and Watersheds. Authors: Gene Surber, MSU Extension Natural Resources Specialist Bob Ehrhart, Research Specialist, RWRP, Univ. of Montana. Introduction. Riparian Areas Uplands Watersheds. Importance of a Watershed. What happens in one part of the watershed – effects other parts

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Streams and Watersheds

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  1. Streams and Watersheds Authors: Gene Surber, MSU Extension Natural Resources Specialist Bob Ehrhart, Research Specialist, RWRP, Univ. of Montana

  2. Introduction • Riparian Areas • Uplands • Watersheds

  3. Importance of a Watershed • What happens in one part of the watershed – effects other parts • Riparian areas – links between the uplands and the stream

  4. Stream Classification • 1st order stream • starter stream • 2nd order stream • two or more 1st order • 3rd order stream • two or more 2nd order

  5. Stream Classification, cont. • Perennial streams • Intermittent streams • Ephemeral streams

  6. Stream Classification, cont. • Gaining stream • Losing stream

  7. Stream Classification, cont. • Channel Shape Method (Rosgen Classification) • Slope • Sinuosity • Ratio (width to depth) • Entrenchment • Particle size

  8. Streams Reflect the Landscape • Steep, mountainous channel • Wide floodplain

  9. Stream Mechanics • Stream hydrology • Stream channels – “pipelines” • Average bankfull flow • Stable streams • Water/sediment IN = water/sediment OUT

  10. Stream Mechanics, cont. • “Out of Balance” • Water and sediment load changes

  11. Stream Mechanics, cont. • Energy = Mass x Velocity • Biggest influence on a stream’s energy is speed

  12. Energy • Friction slows water • Sediment is deposited • No vegetation versus vegetated banks

  13. Change is constant • Streams are dynamic • Natural versus man-made causes

  14. Stability • Dynamic  Unstable • Stable streams change, but remain in equilibrium • Unstable streams are “out of balance” • Nature has a different time scale

  15. Stream Instability • Instability: • Change in water flow • Elimination of streambank vegetation • Excessive sediments • 2 types: • Lateral Instability • Vertical Instability

  16. Stream Instability, cont. • Vertical Instability • Downcutting • More difficult to control than lateral cutting • Influences BOTH upstream & downstream

  17. Summary • Where we go from here…

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