1.C - Sources of Sediment Flashcards
1
Q
what are the 3 main sources of sediment?
A
- TERRESTRIAL - including fluvial deposition, weathering and mass movement, marine erosion, aeolian deposition and longshore drift.
- OFFSHORE - including marine deposition
- HUMAN - including beach nourishment
2
Q
examples of sources of sediment
A
- offshore bars/sand banks
- wave/ocean sediment (marine)
- nearshore bank
- longshore drift (beaches mostly drift aligned in UK)
- rivers carrying sediment (alluvium)
- cliffs eroding
- aeolian processes
3
Q
what could affect the relative significance of different sources of sediment?
A
- GEOLOGY- more soft rocks = more input from cliffs = bigger beaches.
- WEATHER - nature of waves = more sediment
- GEOGRAPHICAL LOCATION - more exposed/destructive waves = removing sediment = decreased input
- SIZE OF RIVER = big beaches come with rivers.
4
Q
how do rivers input into a coastal system?
A
- rivers are main sources of sediment input to the coastal sediment budget and this is particularly true of coasts with a steep gradient, where rivers directly deposit their sediments at the coast.
- sediment delivery to the shoreline can be intermittent, mostly occuring during floods. in some locations, as much as 80% of coastal sediment comes from rivers.
- the origin of the sediment is the erosion of inland areas by water, wind and ice as well as sub-aerial processes of weathering and mass movement
5
Q
how do waves input into a coastal system?
A
wave erosion is also the source of large amounts of sediment and makes a major contribution to coastal sediment budgets.
6
Q
how do cliffs input into a coastal system?
A
- cliff erosion can be increased by rising sea levels and is amplified by storm surge events.
- the erosion of weak cliffs in high energy wave environments contributes as much as 70% of the overall material supplied to beaches, although typically it contributes much smaller amounts.
- some of this sediment may comprise large rocks and boulders, esp. if derived directly from the collapse of undercut cliffs.
- longshore drift can also supply sediment from 1 coastal area by moving it along the coast to adjacent areas.
7
Q
how do offshore sources input sediment?
A
- constructive waves bring sediment to the shore from offshore locations and deposit it (marine deposition), adding to the sediment budget
- tides and currents do the same
- wind also blows sediment from other locations, including exposed sand bars, dunes and other beaches elsewhere along the coast
- this aeolian material is generally fine sand, as wind has less energy than water, and so cannot transport very large particles.
8
Q
how do humans input sediment?
A
- when a coastal sediment budget is in deficit, beach nourishment is one way in which a sediment equilibrium can be maintained.
- this type of management has been adopted all over the world to preserve and protect the coastal environment
- sediment can be brought in by lorry and dumped on the beach before being spread out by bulldozers.
- alternatively, sand and water can be pumped onshore by pipe line from offshore sources. low bunds hold the mixture in place while the water drains away and leaves the sediment behind.
- in addition, hard engineering coastal management systems can affect the coastal sediment budget e.g. input from longshore drift is affected by building groynes
9
Q
what is equilibrium?
A
- when a system’s inputs and outputs are equal
- e.g. rate of sediment added to beach = the rate its being removed, ∴ beach remains same size.
10
Q
what happens when equilibrium is disturbed?
A
- the system undergoes self regulation to restore equilibrium
- this is called dynamic equilibrium and is an example of negative feedback.
11
Q
what is a positive feedback loop?
A
- an automatic response to a change in a system which GENERATES FURTHER CHANGE (an issue)
- causes rate of change to increase
- often caused by humans
- one small change leads to more change away from equilibrium
12
Q
what is a negative feedback loop?
A
- an automatic response to change in a system that restores equilibrium (a good thing!)
- e.g. storm removes sediment = not equilibrium,
constructive waves build up beach, restores equilibrium.