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Kent · Kent

Fossil hunting at Folkestone Warren

Gault Clay and Greensand beneath the chalk, with well-preserved ammonites and shells.

Coastal cliffs and foreshore typical of Kent

Representative photography of this stretch of coast, not a photograph of the site on a particular day.

What can you find?

About the site

Folkestone Warren is a large landslip complex between Folkestone and Dover where the Gault Clay is exposed beneath the chalk. The Gault is famous for beautifully preserved ammonites, often with original shell, along with bivalves, gastropods and occasional fish and reptile remains.

Collecting concentrates on material weathering out of the clay on the foreshore. The site is an SSSI and the cliffs are unstable, so the cliff faces themselves should be left alone.

Planning a visit

Geological period
Early Cretaceous (Gault Clay and Lower Greensand), around 110–100 million years old
Difficulty
Moderate
Suitable for children
Not recommended for young children at this site.
Best time to go
Winter, after storms have washed the clay.
Tides
Only work a falling tide; the foreshore below the Warren is cut off at high water.
Access
Steep paths through the landslip and a rough foreshore. Not accessible for limited mobility.
Parking
Parking at Capel-le-Ferne or in Folkestone, then a walk down into the Warren.
Walking and terrain
1 km or more, including steep descents.
Location type
Beach, Cliff, Geological site
Collecting
SSSI. Collect loose foreshore material only; do not hammer the cliffs or the in-situ Gault.

Check before you travel: Paths in and out of the Warren change as the landslip moves — check the current route locally.

Safety

  • Active landslip with frequent movement and rockfall.
  • Tidal cut-off risk along the foreshore.
  • Railway land borders the site — keep out.

What to bring

  • Boots
  • Tide table
  • Small pots for delicate ammonites
  • A companion

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