The Fluvial Process
Erosion by Streamflow
Once surface flow is channelized
hydraulic power
gravity (steep gradient)
turbulence
When all factors are high - erosion is highest
mountains and floods
Sierra Nevada Story
Transportation
and Deposition
attrition
- natural sizing,
rounding
and sorting
large boulders to fine, suspended silt
less sorted to well-sorted
dissolved load
- invisible minerals dissolved in solution
suspended load
- fine particles (silt) are suspended (never touching bottom)
saltation
- coarser material (like gravel and sand) bounce along
traction
- larger material dragged along (large rocks)
degrading streams
cutting down, carving and eroding
adding to suspended load
max. on steeper gradient
soft parent material
aggrading
streams -
more sediment than it can transport - deposition
maximum on flattened landscapes downstream
decrease in velocity
silt-filled
deltas
and estuaries
Yuba River in Marysville 1870 - hydraulic mining day
Graded streams
neither
degrading
or
aggrading
( flowing in equilibrium)
striving toward
River Questions
Stream Channels
three (3) dimensional and complex nature
gravity must overcome friction from bank walls & bottom
most energy is used up by overcoming friction!
erosion is limited - (5%) on average
faster current is in
middle of river
(with less friction)
(many more drainage patterns - read in book)
straight channels - unusual in nature; often along faulted rock
thalweg
- stream flow will wander in even the straightest channels
likely to transform into a sinuous channel
indicating the deepest part of channel
meandering channels
- sinuous channels with defined loops
generally associated with low gradient streams
broad floodplains resulting from migrating river
Sacramento Valley
braided streams
- multiple, interwoven channels filled with sediment
often broad
glaciated streams
loaded with silt and gravel
Canada and Alaska
Next