Formation of graded profiles Flashcards
formation of graded profiles
time climate geology and tectonics changes in base level reservoirs and dams land use
time
everything stays the same, erosion by the river will reduce its height above base level. sediment is carried as load and will be deposited into the sea forming a delta
climate
precipitation is the input into the river system. long term changes in climate will alter the rate at which a river can adjust its long profile to local variations in other factors. It will speed up when precip is high and vice versa for low
geology and tectonics
resistant intrusions prevent the smooth graded profile from developing. some features such as waterfalls are caused by the lowering of the long profile downstream with different rock resistances
changes in base level
a fall in sea level or rise in the land will lead to erosion by increasing the potential energy available. A fall to the sea creates a “nick point” of potential energy which trsvels upstream encountering varying levels of erosion depending on the river geology
reservoirs and dams
reservoirs control flood flows and reduces the winter energy surplus in rivers. waterfalls no longer retreat upstream with dam projects and new base level may be created
land use
overgrazing; destruction of the vegetation cover in the catchment area has noticiblee effects on the sediment carried, transporting the load uses up energy and reduces the rate of erosion
upper course consists of
v- shaped valleys straight channels waterfalls gorges rapids
middle course consists of
riffles and pools
point bars
alluvial fans
braiding
lower course consists of
esturies
deltas