
Image: Wikimedia Commons
Understanding the Sand Dunes — Why the Sefton Dune System Matters
15 November 2025
The sand dune system on the Sefton Coast is one of the most extensive in England. It stretches nearly 20 miles from Crosby to Southport, averaging a kilometre wide. From the beach looking inland, it looks uniform — just sand and rough grass. It isn't. There are distinct zones, each with its own ecology, and some of the most unusual plant and animal communities in lowland England are hiding in the damper hollows.
How dunes form
Sand dunes form where sand is blown inland from the beach and trapped by vegetation. On the Sefton Coast, the process has been running for several thousand years — the youngest, most mobile dunes are at the seaward edge; the oldest, most stable dunes are furthest inland.
The key plant in dune formation is Marram Grass. It tolerates burial by sand and actually grows faster when covered — its roots bind the sand and its stems trap more. Without Marram, dune systems don't accumulate. With it, they can build to ten or fifteen metres in height.
The dune zones
Moving inland from the beach: the embryo dunes just above the high-tide mark are sparsely colonised by Sea Rocket and Prickly Saltwort. Behind them, the mobile yellow dunes — steep, unstable, dominated by Marram — are where the system is still building.
Further back, the fixed grey dunes are older and more stable. The Marram gives way to a richer plant community — Restharrow, Lady's Bedstraw, Sand Sedge, Hare's-foot Clover. These are the botanically interesting dunes and they hold most of the dune-specialist invertebrates.
In the hollows between ridges — the dune slacks — the water table reaches the surface in winter. These are the wettest part of the system and they hold some of the rarest species: Grass of Parnassus, Round-leaved Wintergreen, Marsh Helleborine, and the Natterjack Toad.
Why the system is changing
Two things are changing the dunes. At the seaward edge, erosion is taking the front face of the dunes back by a metre or more a year in some places. This is partly natural process, partly accelerated by sea level rise and changing wave patterns.
At the landward edge, the problem is different. Without disturbance, scrub — Sea Buckthorn and Creeping Willow in particular — invades the grey dunes and slacks and shades out the specialist plants. The fixed dunes are becoming scrub woodland in some sections, losing their open character and the species that depend on it.
Active management — scrub removal, cattle grazing, occasional heavy machinery — is required to maintain the open dune habitats. It's expensive, ongoing and unglamorous. The alternative is losing the habitat entirely.
What to look for when you visit
The botanically best areas are the fixed grey dunes and the wet slacks. Ainsdale NNR is the best site — Natural England runs guided walks in summer that are worth booking for their plant-identification value.
For invertebrates, the fixed dunes on sunny days in summer produce impressive diversity — look for mining bees and solitary wasps in bare sand patches, and several nationally scarce beetle species have been recorded in the dunes here.
Don't walk on the mobile dunes unnecessarily. Marram breaks under foot traffic and once the surface is broken, erosion accelerates. The paths exist for a reason.
About the author
Ed
Ed has been walking the Sefton Coast since the 1980s. He keeps a yearly bird tally, owns more waterproof jackets than he'd care to admit, and has strong opinions about which hide has the best light in the morning. Retired geography teacher. Still gets up at five.