Looking for our old site? We've rebranded — new look, same exam success.

Geography · The natural environment

Coasts

CIE 04605 min read

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

  1. The waves swash at the angle of the prevailing winds
  2. The backwash is 90 degrees towards the sea
  3. The continuous swash and backwash transports the sediment across the beach

Erosional landforms

Similar to features of rivers — use keywords and the names of fluvial processes.

Headlands and bays

  1. A cliff is made of alternating layers of hard and soft rock
  2. The soft rock erodes quicker than the hard rock due to hydraulic action
  3. Hard rock is more resistant and erodes slower
  4. This difference in erosion speeds causes headlands and bays
  5. Headlands — hard rock
  6. Bays — soft rock

Caves, arches, stacks and stumps

  1. The headland is surrounded by waves on all sides, so energy is concentrated
  2. A crack opens up due to hydraulic action
  3. The crack grows due to erosion (hydraulic action and abrasion); the base of the cliff erodes, causing a wave-cut notch to form
  4. Over time, a cave forms
  5. The cave erodes on opposite sides of the headland, causing a natural arch to form
  6. The arch collapses after erosion to form a stack
  7. The stack erodes into a stump

Cliffs and wave-cut platforms

  1. The sea attacks the base of the cliff
  2. A wave-cut notch forms
  3. The backwash of the waves carries the rubble back into the sea, forming a wave-cut platform
  4. The notch increases in size, undercutting the cliff and causing it to collapse

Depositional landforms

Spit

  1. Longshore drift carries/transports sediment in the direction of the prevailing wind
  2. Material is curved due to the secondary winds as it meets the estuary — this is called a curved end
  3. The coastline changes direction, but the material is still deposited in the direction of the prevailing wind
  4. Behind the spit, a lagoon/marsh often forms

Beaches

  1. Material is deposited in bays
  2. Bays are more sheltered land with lower-energy waves that tend to be constructive
  3. More sediment is deposited than eroded
  4. Longshore drift transports this sediment along the coast, forming a beach

Sand dunes

  1. Embryo dunes form around deposited material such as a piece of rock or wood
  2. They develop and become stabilised by vegetation (marram grass)
  3. As vegetation dies, nutrients are provided to the dune, making it more fertile for vegetation to grow
  4. 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

TypeFormation
FringingClosest to shore. The island is new and coral surrounds it.
BarrierParallel to shore and is several km away. The island is subsiding, causing a lagoon to form.
AtollThe 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

BenefitsThreats
TourismPollution
Medicine (found in some coral species)Overfishing
FishingCoral 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

BenefitsThreats
Acts as a nutrient filter for the waterDeforestation
Reduces flood and storm impactsClimate change
Home to many speciesGlobal rise in sea levels
TourismSewage nutrients add nitrogen and phosphorus in overly high levels
Reduces CO2 in the air (photosynthesis)
Wood production

Coastal management

MethodDescriptionAdvantages / Disadvantages
GroynesWooden barriers built perpendicular to the beach to trap sedimentHard; unattractive and expensive
Rock armour barrierCollection of large boulders that break up wavesHard and ugly; long-lasting and cheap
GabionsMesh filled with rocks to absorb wavesShort lifespan
Sea wallsConcrete barriers used to stop waves from hitting the beachExpensive and reflects energy of waves back; unattractive
Beach nourishmentSand is dredged and moved onto the beach to even out longshore driftHas maintenance costs; noisy and kills marine life
Dune regenerationBuilding dunes by planting grass and fencing the areas so the area behind the dunes is unaffected by erosionSlow process for growth; cheap and creates habitats
Beach reprofilingBulldozers move material up the beach into a gentle slope to break down wavesShort 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

OpportunitiesHazards
TourismNatural disasters: flooding and tropical storms
FishingCoastal erosion: loss of beaches and settlements
FarmingSea levels rising: global warming
Settlements
Leisure

Solutions

  1. Hawaii Coastal Zone Management Program takes aerial pictures of the coast and discusses the next steps to stopping erosion and predicting future erosion.
  2. Sea walls (but this could threaten nearby coastlines like Sunset Beach).
  3. 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

CausesImpactsResponse
Storm path was not as predicted550,000 homes destroyed1,200 evacuation centres
Lack of communications400 mm of rain caused floodingUK government sent shelter kits
High population density30,000 fishing boats destroyedOxfam provided replacement boats
No transport to move inland6,300 killedTyphoon shelters built to accommodate people in the future
Lightweight building materialsShortage of water and shelterFrench and Belgian field hospitals set up
Infrastructural damageThousands of homes built away from areas that may flood
US helped with search and rescue

Test yourself

Term · tap to flip

Definition

← All Geography topics