Key definitions
Swash — the rush of sea water up the beach after a wave is broken.
Backwash — the flow of sea water back down into the sea.
- Swash — the rush of sea water up the beach after a wave is broken
- Backwash — flow of sea water back down into the sea
Waves
There are 2 types of waves:
- Constructive waves — powerful swash, weak backwash
- Destructive waves — powerful backwash, weak swash
Longshore drift
- The waves swash at the angle of the prevailing winds
- The backwash is 90 degrees towards the sea
- The continuous swash and backwash transports the sediment across the beach
Similar to features of rivers — use keywords and the names of fluvial processes.
Headlands and bays
- A cliff is made of alternating layers of hard and soft rock
- The soft rock erodes quicker than the hard rock due to hydraulic action
- Hard rock is more resistant and erodes slower
- This difference in erosion speeds causes headlands and bays
- Headlands — hard rock
- Bays — soft rock
Caves, arches, stacks and stumps
- The headland is surrounded by waves on all sides, so energy is concentrated
- A crack opens up due to hydraulic action
- The crack grows due to erosion (hydraulic action and abrasion); the base of the cliff erodes, causing a wave-cut notch to form
- Over time, a cave forms
- The cave erodes on opposite sides of the headland, causing a natural arch to form
- The arch collapses after erosion to form a stack
- The stack erodes into a stump
- The sea attacks the base of the cliff
- A wave-cut notch forms
- The backwash of the waves carries the rubble back into the sea, forming a wave-cut platform
- The notch increases in size, undercutting the cliff and causing it to collapse
Spit
- Longshore drift carries/transports sediment in the direction of the prevailing wind
- Material is curved due to the secondary winds as it meets the estuary — this is called a curved end
- The coastline changes direction, but the material is still deposited in the direction of the prevailing wind
- Behind the spit, a lagoon/marsh often forms
Beaches
- Material is deposited in bays
- Bays are more sheltered land with lower-energy waves that tend to be constructive
- More sediment is deposited than eroded
- Longshore drift transports this sediment along the coast, forming a beach
Sand dunes
- Embryo dunes form around deposited material such as a piece of rock or wood
- They develop and become stabilised by vegetation (marram grass)
- As vegetation dies, nutrients are provided to the dune, making it more fertile for vegetation to grow
- Wind may cause depressions in the sand called slack dunes, where ponds may form
Coral reefs
- Found in shallow waters less than 25 m
- Located in tropical water
- Thrive in saline water
- High biodiversity — home to over 25% of all marine species
- Temperatures of 23–25 degrees C
- The largest coral reef is the Great Barrier Reef
3 types of coral reefs
| Type | Formation |
|---|
| Fringing | Closest to shore. The island is new and coral surrounds it. |
| Barrier | Parallel to shore and is several km away. The island is subsiding, causing a lagoon to form. |
| Atoll | The island has subsided, many km away from shore, located in deeper water. An inner lagoon is formed where the coral surrounds. |
Benefits and threats to coral reefs
| Benefits | Threats |
|---|
| Tourism | Pollution |
| Medicine (found in some coral species) | Overfishing |
| Fishing | Coral bleaching |
| Biodiversity (25% of marine life) | Tourism |
| Provides protection from waves and tsunamis | |
Mangroves
- Found in between the tropics in warmer water
- Found around the coasts of every continent except Antarctica and Europe
- Salt-tolerant trees adapted for coastal conditions
- Has salt-secreting leaves, aerial roots and stilt roots to breathe during different tidal levels
Benefits and threats to mangroves
| Benefits | Threats |
|---|
| Acts as a nutrient filter for the water | Deforestation |
| Reduces flood and storm impacts | Climate change |
| Home to many species | Global rise in sea levels |
| Tourism | Sewage nutrients add nitrogen and phosphorus in overly high levels |
| Reduces CO2 in the air (photosynthesis) | |
| Wood production | |
Coastal management
| Method | Description | Advantages / Disadvantages |
|---|
| Groynes | Wooden barriers built perpendicular to the beach to trap sediment | Hard; unattractive and expensive |
| Rock armour barrier | Collection of large boulders that break up waves | Hard and ugly; long-lasting and cheap |
| Gabions | Mesh filled with rocks to absorb waves | Short lifespan |
| Sea walls | Concrete barriers used to stop waves from hitting the beach | Expensive and reflects energy of waves back; unattractive |
| Beach nourishment | Sand is dredged and moved onto the beach to even out longshore drift | Has maintenance costs; noisy and kills marine life |
| Dune regeneration | Building dunes by planting grass and fencing the areas so the area behind the dunes is unaffected by erosion | Slow process for growth; cheap and creates habitats |
| Beach reprofiling | Bulldozers move material up the beach into a gentle slope to break down waves | Short term and cheap; has to be done often and removes sediment from other parts of the beach |
Case study of a coast — Hawaii
- Tourism: $17 billion (2019) in visitor spending
- 10 million tourists in 2019
- 7,300 farm operations (2022)
- 60% of USA's coral reefs
Opportunities and hazards of living near a coast
| Opportunities | Hazards |
|---|
| Tourism | Natural disasters: flooding and tropical storms |
| Fishing | Coastal erosion: loss of beaches and settlements |
| Farming | Sea levels rising: global warming |
| Settlements | |
| Leisure | |
Solutions
- Hawaii Coastal Zone Management Program takes aerial pictures of the coast and discusses the next steps to stopping erosion and predicting future erosion.
- Sea walls (but this could threaten nearby coastlines like Sunset Beach).
- Sandbag gabions for citizens to use as a form of small-scale protection.
Coastal disaster case study — Typhoon Haiyan (Philippines)
- Wind speeds of 315 km/h
- 8th November 2013
- Category 5 tropical cyclone
- $2.98 billion in damage
Causes, impacts and response
| Causes | Impacts | Response |
|---|
| Storm path was not as predicted | 550,000 homes destroyed | 1,200 evacuation centres |
| Lack of communications | 400 mm of rain caused flooding | UK government sent shelter kits |
| High population density | 30,000 fishing boats destroyed | Oxfam provided replacement boats |
| No transport to move inland | 6,300 killed | Typhoon shelters built to accommodate people in the future |
| Lightweight building materials | Shortage of water and shelter | French and Belgian field hospitals set up |
| Infrastructural damage | Thousands of homes built away from areas that may flood |
| | US helped with search and rescue |