Lecture 11-12 - Knickpoints Flashcards

1
Q

What are knickpoints?

A

Steps on the river longitudinal profiles, a disturbance to the equilibrium that needs to be destroyed. Regulated by the stream power law.

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2
Q

The equation for stream power law is i=kA^mS^n. What does it mean when m and n =1 and when m and n = <1?

A
  • When m and n = 1 then incision rate is directly proportionate to stream power, parallel retreat
  • When m and n <1 erosion rates are proportional to bed shear stress. The height and slope of knickpoints decrease, slope replacement
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3
Q

What effects do normal faults have on topography?

A
  • Facets will be created.
  • Large facets = active faults
  • Degraded facets = inactive faults
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4
Q

What is drainage spacing and what happens to these in tectonically acitve and tectonically inactive areas?

A
  • Drainage spacing is the ratio between the length of the river and the distance between two river mouths.
  • Tectonically active: small catchment area, closesly spaced rivers
  • Tectonically inactive: bigger catchment areas. widely spaced rivers
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5
Q

What is sinuosity and what does it mean when this = 1 and what does it mean when it is >2?

A
  • Sinuosity: ratio between the actual length of the mountain front and the straight length of the mountain front.
  • When sinuosity = 1 then actively deforming, when >2 then inactive front.
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