Coast Gateway 1 Flashcards
1
Q
Coastal erosion
A
- hydraulic action
- abrasion
- solution
- attrition
2
Q
Hydraulic Action
A
- When waves strike against rock surface, air is trapped in rock joints
- Air is compressed repeatedly by oncoming waves, exerting pressure on joints
- Joints are weakened and shatter
3
Q
Abrasion
A
- Waves carry sediments such as sand and rocks which are hurled against the coast when waves break
- These sediments knock and scrape against the coastal cliff surface
- This weakens the surface and coast breaks down
- Overtime, impact can be powerful enough to undercut a cliff
4
Q
Solution
A
- Seawater reacts chemically with and dissolves water soluble minerals in rocks
- Rocks are weakened and eventually disintegrate
- Carbonic acid easily corrodes limestone rocks
5
Q
Attrition
A
- Sediments such as rocks carried by waves rub and hit against each other
- Rocks break down into smaller pieces
- Overtime, rocks become rounder and smoother
6
Q
Sediment transport
A
- Involves 2 processes, beach drift and longshore drift
- These 2 processes resulted from waves approaching coast at an angle
Beach drift
- When waves approach coast at an angle
- Waves break on shore
- Swash carry sediments up the beach at an angle
- Backwash carry sediments perpedicularly down the beach
- The resultant zig zag movement of sediment is beach drift
Longshore drift
- It is the combined effect of both beach drift and longshore current
- When waves approach coast at an angle
- Longshore currents are generated in offshore zone near shore and carry sediments along shore
- Longshore currents are currents flowing parallel to the coast
- It is most rapid when approach coast at 30 deg
7
Q
Sediment deposition
A
- It involves the addition of materials onto beach, building it up
- When wave energy decrease, waves can no longer carry sediments
- Coarser sediments are deposited first before finer sediments
- Deposited sediments vary in types and sizes resulting in a variety of beaches
- Location of coasts affect the deposition of sand
Finer sediments are deposited in sheltered coasts of calm waters where destructive waves are less common and sheltered from strong winds
- sandy beaches often found in deep bays sheltered by headlands
Coarser sediments are deposited in more exposed coasts where wave energy is higher to remove finer sediments