This is the location of the famous ‘West Runton Elephant’ find. From the West Runton Fresh Water Bed, mammal and fish remains are common, along with freshwater shells. On the foreshore, during scouring tides, the chalk yields echinoids and sponges.
♦ West Runton is located to the west of Cromer on the northern Norfolk coast and is a small village. Driving through the village, you will pass some caravan sites and then a road sign leading to the beach. There is a small corner shop near the entrance to the road. Follow the road all the way down and, on the left, you will come to a car park.
♦ In summer, parking fees apply at a toll gate, but, during the off peak season, tickets are issued from the cafe. Toilets and the cafe are also next to the beach. Once on the beach, you need to walk east and it isn’t very far until you get to the beds (providing they are exposed).
♦ The best chalk section, including the Micraster Bed, is just west of the road on the shore. During scouring tides, the entire foreshore is exposed with chalk.
♦ Ref: 52.94173°N, 1.25137°E
FIND FREQUENCY: ♦♦♦♦♦ – West Runton is a very productive site. However, you do need the right conditions – either scouring to expose the chalk on the foreshore and Weybourne Crag or a high tide to wash out the Cromer Forest Bed. In fact, the best beds at West Runton are in the lowest part of the Cromer Forest Bed, which are exposed during scouring tides.
CHILDREN: ♦♦♦♦♦ – West Runton is ideal for children. Indeed, local schools often take their students to this location to study the geology of the area. They can collect fossils on the foreshore and, when they get bored, they can play in the sand. Toilets and a cafe are provided at the car park near the beach.
ACCESS: ♦♦♦♦ – There is easy parking nearby at West Runton, with good access to the beach.
TYPE: – Fossils at West Runton can be found within the cliff (in the Cromer Forest bed) or on the foreshore (in the chalk).
The Forest Bed is rich in fossils. There is a large number of different freshwater shells to be collected, together with fossil seeds, and fish, birds, frogs and mammal remains. The mammal remains from this bed can be anything from beavers to vole and even elephants, deer and hippopotamus. So many different mammals have been recorded from this bed that you never know what you may find. On the foreshore, the chalk yields superb corals, sponges and echinoids. Bivalves can also be found. Between the Fresh Water Forest Bed and the chalk, the Wroxham Crag also yields mammal and fish remains, and anything from deer to mammoth and whale remains have been found.
The best time to collect fossils at West Runton is after high tides, heavy rainfall and scouring conditions. Fossils are exposed on the Forest Bed surface, which can easily be seen and collected from. After a very high tide and during scouring conditions, mammal remains are often found. However, even if the conditions are not favourable, with a small knife or pick, you can very gently break apart the loose material at the base of the cliff section to make finds. On the foreshore, fossils from the chalk and Wroxham Crag can be found. Search carefully around the chalk exposures and in the areas of heavy-iron coloured cemented pebbles (that is, the Wroxham Crag).
West Runton beach is most famous for the elephant or steppe mammoth, Mammuthus trogontherii, which was discovered in 1990 and is one of the oldest and best preserved fossil elephants ever found in the UK. Deposits of bone and teeth can still be collected from this bed, but, being a SSSI, it should not be dug into and it is better to collect from the beach, unless something is obviously exposed at the surface.
The section between West and East Runton is complex in terms of its geology. The beach itself is comprised of ﬂint, which sits on top of a Cretaceous chalk, wave-cut platform, with various glacial erratics.
Directly on top of the chalk is the Cromer Stone Bed, followed by the Wroxham Crag. The Wroxham Crag consists of sands, gravels, silts and clays, which represent a period from the pre-Pastonian cold stage to the Pastonian warm stage and into the Beestonian cold stage.
The Cromer Stone Bed and Wroxham Crag are often cemented together by calcrete and iron pan, and are exposed during heavy tidal scouring conditions. The shelly sands, grey silts and conglomerates have produced a rich fauna, including voles, shrews, giant beaver, deer and elephant, and is signiﬁcantly older than the West Runton Freshwater Bed.
Overlying the Wroxham Crag is the West Runton Freshwater-bed. This is a prominent dark, peaty bed at the base of the cliﬀ, which is up to two metres thick. It is highly fossiliferous and contains the remains of plants and trees (seeds, cones, fungi and pollen), terrestrial and aquatic molluscs, ﬁsh (scales, teeth and bones), amphibians, large and small mammals (teeth and bones) and bird bones. It is comprised of glacial sands.
Both the Cromer Stone Bed and West Runton Freshwater-bed form part of the Cromer Forest Bed formation and is exposed at intervals along the coast of Norfolk and Suffolk, from Weybourne to Kessingland. The Forest Bed is between 700,000 to 500,000 years old, from the Quaternary.
Common sense when collecting at all locations should be used and knowledge of tide times is essential. The main issue at West Runton to consider is the tide if visiting the chalk past the headland. This is the main place where you can be cut off by the tide.
The West Runton Freshwater-bed is protected by SSSI rules, so digging and removing samples is not permitted, but the use of small tools, such as a knife or small pick to remove any fossils is. Collecting from the foreshore chalk is less restricted, but a knife or pick is still the best tool for removing fossils. Remember to bring specimen boxes to ensure your fragile specimens make it safely back home.
This site is a site of special scientific interest (SSSI). This means you can visit the site, but hammering the bedrock is not permitted. For full information about the reasons for the status of the site and restrictions, download the PDF from Natural England.