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.
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
3
Q
What effects do normal faults have on topography?
A
- Facets will be created.
- Large facets = active faults
- Degraded facets = inactive faults
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
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.