Discover more at Birling Gap and the Seven Sisters
Find out how to get to Birling Gap and the Seven Sisters, where to park, the things to see and do and more.
Our coastlines are constantly changing due to rising sea levels, erosion and weathering. These natural processes have been happening for centuries and have shaped Birling Gap and the Seven Sisters into what you see today. These changes present us with unique challenges including those of the safety of our visitors. The geology at these sites are slightly different but both are important for wildlife and vegetation, providing a home for plants and nesting birds. We work with these natural coastal changes to plan for the future in this dynamic landscape.
The white chalk cliffs of the Seven Sisters are world famous. The chalk erodes in such a way that large pieces fall away and leave near-vertical faces which create the steepness of the cliffs.
It is not just the action of the sea from below that causes this erosion but also heavy rainfall. Water passes through the chalk and then freezes as temperatures drop. The water then expands and cracks the chalk, causing the cliffs to erode from the top.
The past year has seen significant change here at Birling Gap. We have had to take down the seaward section of our building and have relocated the cafe and visitor centre further inland. Changes will continue over the coming years as we adapt with our dynamic coastline. The next stage of work will be to redesign our exisiting car park to ensure that our visitors are always kept safe and have a great visit. This will include designing a dedicated space for motorcyles, minibus parking, a taxi drop off and pick up zone, improved surface conditions for Blue Badge holders and the removal of dedicated coach parking.
Our white cliffs are beautiful but also very fragile. They may appear safe to stand on, but chalk is a soft rock that can be softened further by heavy rain or undercut by wind and wave action. This means the cliff edge is very unstable and at risk of collapsing at all times. It is unsafe to stand on or near the edge and near the base of the cliffs. Always keep at least 5m back from the cliff edge and the base of the cliff, even when the sun is shining. Be aware of tide times. The sea comes in and out twice a day and often reaches the base of the cliffs so it is possible to get cut off by the incoming tide or forced up against the cliffs with the subsequent risk of drowning. We do not encourage anyone to walk further than 150m either way from the beach platform. Make sure you can always safely exit the beach.
At Birling Gap the geology is slightly different, and this can best be seen by looking back at the cliffs from the beach at low tide. The dry valley, underlain with coombe rock, was created during the last Ice Age (which lasted until about 12,000 years ago). As the coombe rock is much softer than the chalk it erodes at a faster rate – about one metre every year - causing a slight ‘bay’ at Birling Gap.
In 2014, the chalk cliffs at Birling Gap suffered seven years’ worth of erosion in just two months, in part due to heavy storms.
Most of the coastline in the south east of England is either built up or protected through sea defences. This has not happened at the Seven Sisters, which has remained unspoilt due to the long history of National Trust and East Sussex County Council ownership.
These cliffs and the wave cut platform below are nationally and internationally important for their biology and geology. They provide spaces for specialised plants and animals to thrive, as well as being a safe habitat for nesting birds such as fulmars, kittiwakes and peregrine falcons.
Find out how to get to Birling Gap and the Seven Sisters, where to park, the things to see and do and more.
Discover what to see and do at Birling Gap and the Seven Sisters. Fossil hunt on the beach, walk on the historic downland or enjoy the views as you spot birds.
Find out about bringing your dog to the South Downs. Explore the beautiful landscape together, from cliff-tops and beaches to ancient downland.