Landforms of Coastal Deposition (Cambridge International IGCSE Geography)

Specification link

This page covers section 2.2.1 of the CIE IGCSE specification .

• 2.2.1 - The characteristics and formation of landforms: beaches, spits, bars, sand dunes.

Formation of deposition coastal landforms

Spec point — The characteristics and formation of landforms: beaches, spits, bars, sand dunes.

Beaches

• Typically, beaches form during the calmer summer months, in sheltered areas such as bays

• Constructive wave action causes deposition, with the swash being stronger than the backwash

• Strong winds can occasionally carry sand from offshore bars onto the shore

• Blown sand can create sand dunes at the backshore of a beach

  1. When a constructive wave carries sediment up the beach, the largest material is deposited along the upper reach of the swash
  2. As the backwash moves back down the beach, it loses water and therefore energy as it travels due to the porosity of the sand
  3. Consequently, the deposition of sediment gets progressively smaller, and the beach is therefore, sorted by wave deposition, with the smallest mud particles settling in the low-energy environment offshore
  4. If a destructive wave forms due to a storm, then large shingle is thrown above the usual high tide level to form a ridge at the top of the beach called a berm

Diagram of sediment deposition on a beach

Spit

• A spit is an extended stretch of sand or shingle that extends out to sea from the shore

• Spits occur:

  • When there is a change in the shape of the coastline
  • or
  • When the mouth of a river prevents a spit from forming across the estuary

• A spit may or may not have a 'hooked' end, depending on opposing winds and currents

• A good example is Spurn Point, which stretches for three and a half miles across the Humber Estuary in the northeast of England

Stages of spit formation

1. Sediment is transported by longshore drift
2. Where the coastline changes direction, a shallow, sheltered area allows for deposition of sediment
3. Due to increased friction, more deposition occurs
4. Eventually, a spit slowly builds up to sea level and extends in length
5. If the wind changes direction, then the wave pattern alters and results in a hooked end
6. The area behind the spit becomes sheltered
7. Silts are deposited here to form salt marshes or mud flats

Illustration showing spit formation with a 'hooked' end

Bar

• A bar occurs when a spit grows across a bay, and joins two headlands together
• A bar of sand is formed (sandbar)
• Sandbars can also form offshore due to the action of breaking waves from a beach

Illustration showing bar formation

Lagoon

• A lagoon is where a small body of water is cut off from the sea
• They may form behind a bar or tombolo
• Lagoons do not last forever and may fill with sediment and form new land

Tombolo

• A tombolo is formed when a spit joins the mainland to an island
• Chesil Beach in Dorset is a tombolo, as the mainland is joined to the Isle of Portland

Barrier island

• Barrier islands form parallel to the coast
• The main difference between a bar and a barrier island is that a bar joins two headlands, whereas a barrier island is open at one or both ends

Illustration showing the formation of a tombolo and barrier island

Exam Hint You may be asked to draw and label a diagram showing how depositional landforms (beaches, spits, etc.) are formed. You must demonstrate how waves transport sediment along the coast. Practice drawing and labelling these diagrams so you can reproduce any of them in the exam. Marks are awarded for the accuracy and completeness of your labelling and drawing.

Sand dunes

• Sand dunes are a dynamic environment and changes occur quickly
• Sandy beaches are usually backed by sand dunes due to strong onshore winds, which transport dried-out, exposed sand
• Sand grains are trapped and deposited against an obstacle (rubbish, rocks, driftwood, etc) to form dunes
• Dune ridges move inland due to onshore winds pushing the seaward side to the leeward side
• It is the interaction of winds and vegetation that help form sand dunes

Formation of a sand dune

• Windblown sand is deposited against an obstruction, such as a pebble or driftwood
• As more sand particles are caught, the dunes grow in size, forming rows at right angles to the prevailing wind
• In a process known as succession, vegetation will eventually colonise and fix the ridges of the dunes

Illustration of coastal dune succession

• Embryo dunes

  • Embryo dunes are very fragile and easily damaged
  • Pioneer species such as Lyme Grass and Sea Couch Grass begin to grow

• Fore dunes

  • Marram grass begins to stabilise the dune with its root system
  • A microclimate forms in the dune slack

• Yellow dunes

  • Marram grass continues to stabilise the dune with its root system
  • More delicate flowering plants and insects are found in the dune slacks

• Grey dunes

  • Grey dunes are more stable and shrubs and bushes begin to appear

• Mature dunes

  • These are the oldest and most stable of the dunes
  • The soil can support a variety of flora and fauna, such as oak trees
  • This is the final stage in succession

Worked Example Figs. 3.1, 3.2 and 3.3 show three coastlines.

Identify each of the following landforms: (i) landform W in Fig. 3.1

[1]

(ii) landform X in Fig. 3.2

[1]

(iii) landform Y in Fig. 3.2

[1]

(iv) landform Z in Fig. 3.3.

[1]

Solution

• W: Wave-cut platform
• X: Beach
• Y: Sand dunes
• Z: Cliff