Camber dunes information


Following the latest Government advice all of our rights of way sites and countryside parks are open, but some facilities are still closed.

The following car parks are open:

  • Seven Sisters Country Park – both car parks
  • Ditchling Common – car park
  • Ashdown Forest – Pooh car park, off Chuck Hatch Lane in Hartfield Parish
  • Broomhill Sands – car park
  • Camber Sands – Rother District Council’s Camber Western, Camber Central and Old Lydd Road car parks

The following remain closed:

  • Seven Sisters Country Park – visitor centre and public toilet

The sand dunes at Camber are a popular educational resource for students researching coastal, recreational and conservation issues.

Camber Sands
Camber Sands

Location and ownership

Camber Sands is situated towards the eastern end of the East Sussex coast and is the only sand dune system in East Sussex.

A large section of the western end of the dunes lie within the Camber Sands and Rye Saltings Site of Special Scientific Interest (SSSI), while the rest is designated a Site of Nature Conservation Importance (SNCI). Camber village lies behind the dunes towards the eastern end.

East Sussex County Council owns the sand dunes towards the eastern end, covering about 53 acres. Rye Golf Club owns the western end, up to the harbour arm. Rother District Council owns and manages the car parks and beach areas next to the dunes.


Dune systems are formed by a complex interaction between geology, tide, sun, wind and vegetation.

Sand, produced by the grinding action of the waves or from material brought down by river systems, is deposited along the coast. When the tide goes out (almost 1km at Camber) the sand is dried by the sun and wind, and blown inland by the prevailing south-westerly wind. This process is called saltation.

When the sand meets an obstruction, eg vegetation and the wind speed drops, the sand is deposited and forms dunes.

The dunes can be divided into three distinct zones:

  • embryonic fore dunes
  • unstable yellow dunes running parallel with the coast
  • stable grey dunes located on the golf course towards the western end of the system.

Camber is an accreting dune system, which means the dunes are gradually getting bigger. 7,500 cubic metres of sand are deposited here every year.

Camber is part of the Dungeness cuspate foreland, a triangular mass of shingle formed after the last ice age. The dunes have formed within the last 350 years and are now restricted by urban development.

The dune system is wedge-shaped, 1km wide in the West tapering to 10 metres wide in the East, after a distance of 3km.


The sand dunes contain locally and nationally important animal and plant communities.
The plants found on the dunes are an important habitat for moths. Many scarce species have been recorded at Camber Sands, including:

  • Sand Dart (Agrostis ripae)
  • Shore Waistcoat (Mythimna litoralis)
  • White Colon (Sideridis albicon).

The dunes are an important site for wintering birds. The following species have all been spotted:

  • Hen Harrier (Circus cyaneus)
  • Short-eared Owl (Asio flammeus)
  • Snow Bunting (Plectrophenox nivdis)
  • Stonechat (Saxicola rubetra)
  • Sanderling (Calidris alba).

There are also many beetles, with the dunes being the only place in the county where you can find the beetle Bradycellus distnctus.
Surveys carried out at Camber Sands using the National Vegetation Classification system, identified these habitat types:

  • fore dune
  • shingle
  • dune scrub
  • inter tidal
  • woodland
  • acid dune grassland.

Current management

Nature Conservation

An area of Sea Buckthorn is cut and burnt each year between October and February and the regrowth sprayed the following spring.

Fences encourage visitors to keep to the paths over the dunes. Many plants on the dunes are very fragile and are damaged by visitors trampling them. Vegetation along the paths is cleared during the summer to keep paths open.

The rangers regularly clear broken chestnut fencing and rubbish from the dunes. This is particularly important during the summer when the site is very busy with visitors.

Sea buckthorn
Sea buckthorn

Past management

In the 1920s Camber’s large sandy beach was a popular seaside destination. The growing tourist industry let to urban development in Camber village and damaged the dunes.

In 1939 the coastal land at Camber was used by the War Department for military exercises. Concrete tank traps and pillboxes were built because of the threat of German invasion during the 1940s. The beach was also used for practising beach landing manoeuvres in preparation for D-Day.

After the war, the sand dunes had to be restored. In 1967, the council carried out major reseeding of the dunes and wind-blown sand was removed to build Dungeness Power Station. In recent years there has been increasing pressure from tourism with up to 25,000 people visiting on hot summer days. This has resulted in further erosion of the dunes.