Abbey Wood’s highly fossiliferous shell beds are open to the public for digging, with prior permission. The Eocene beds here are extremely rich in fossil sharks’ teeth, fish, mammal and bird remains, and fossil shells. Fossils are best found by onsite sieving, and is often visited by schools and society organised events. Eocene, Disused Pit, Rating: ♦♦♦♦♦
Birchington is generally a poorly fossiliferous location. However, with patience, some specimens can be collected. Finds include Echinocorys, Micraster and Conulus echinoids (sea urchins), as well as bivalves, sponges and belemnites. Cretaceous, Foreshore, Rating: ♦♦
Betteshanger (formerly Fowlmead) Coutry Park is a great site for Carboniferous plants, which are abundant and come from Kent’s former Betteshanger Colliery. Fossils are found in spoil, which is maintained by Geoconservation Kent Rigs. This is a perfect site for all the family, which is easy to access. Carboniferous, Spoil, Rating: ♦♦♦♦♦
The picturesque bay at St. Margaret’s is eroded out of Conacian Upper Chalk. Fossils can be found in the cliffs, boulders and shingle both to the east and the west of the bay. The location is picturesque and there is a very nice pub to relax in after fossil hunting. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
The Lower Chalk exposed at Samphire Hoe is highly fossiliferous. Brachiopods are most commonly found, with corals, urchins, ammonites, sharks’ teeth and more also present. Microfossils are extremely abundant within the chalk and can be extracted relatively easily from rock samples taken home Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦
This stretch of chalk coastline can be accessed from Broadstairs to the south or Joss Bay to the north. Fossils can be found both in the chalk and in the abundant flint pebbles on the foreshore. Common finds include echinoids (sea urchins) and sponges. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
The cliff section between Pegwell Bay and Ramsgate Harbour is composed of Upper Chalk. There are many fallen blocks to investigate for sea urchin fossils, with other common finds including crinoid stem parts, brachiopods and starfish plates. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
This is a popular location for families and dog walkers. The chalk on the foreshore and any fallen boulders or cobbles can be investigated for fossils. Although finds are fairly plentiful, they are often broken. Cretaceous, Cliffs and Foreshore, Rating: ♦♦
The coastline between Kingsdown and St Margaret’s Bay is made up of towering chalk cliffs. Some spectacular collapses have taken place over recent years, yielding a vast quantity of fresh chalk and flints to look over. However (and unfortunately), the rocks here are poorly fossiliferous. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
At this site, fossils can be found in accumulations of flint. They can also be found in the chalk foreshore and in fallen boulders. They can also be seen in the cliffs. Finds are not particularly abundant, but you should go home with something. Cretaceous, Cliffs and Foreshore, Rating: ♦♦
The huge expanse of London Clay exposed on Seasalter’s foreshore lends the location a bleak atmosphere. It is not the most picturesque of fossil hunting sites, but occasionally stunning phosphatic fossils can be found. Perseverance is rewarded here. Eocene, Foreshore, Rating: ♦♦♦♦
The east of Herne Bay marks a dramatic change from rich fossil-bearing Eocene clays to the sandy cliffs of Reculver. Although sharks’ teeth do occur in the Thanet Sands, this location is mainly for those interested in collecting bivalves. These are found within foreshore exposures and the shell beds exposed within the cliff. Eocene, Cliffs and Foreshore, Rating: ♦♦♦
Elmley Hill is situated on the south side of the Isle of Sheppey, on the opposite side to the classic London Clay section of Minster to Warden Point. It is not a particularly rich location for fossils, but nevertheless, some important finds have been made over the years. Getting to this location involves a long walk. Eocene, Cliffs and Foreshore, Rating: ♦♦♦
Allhallows-on-Sea is a London Clay foreshore location, northwest of the Isle of Sheppey on the south side of the River Thames. The actual site runs along the beach next to a large holiday park, which is protected by a 1.8km-long seawall. Success at this location is often subject to beach conditions, which, if favourable, can yield nodules containing lobsters and especially crabs. Eocene, Foreshore, Rating: ♦♦♦
Lower Upnor is probably the most unproductive of all the London Clay sites in Kent, but is situated not far from the Isle of Sheppey and also along the route to Elmley Hill, both of which are covered on this website. Not only do the cliffs contain a lot of vegetation and are badly slumped, but the foreshore often covered in rubbish and the beds here are also from the less productive Division B1 of the London Clay. However, there are still fossils to be found. Eocene, Foreshore, Rating: ♦
This is a classic location and well worth a visit, subject to the access problems discussed below. Fossils are found both in the chalk and as flint casts. The scenery here is magnificent and it is hard not to be impressed by this stretch of coastline. However, access is now more difficult, the dramatic stairs down the cliff having now been closed. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
The Studd Hill location is a foreshore exposure, which begins at Hampton Pier and ends at Long Rock (both are marked on OS 1:50,000 maps). In recent years, continuous erosion has been exposing the London Clay more frequently, although fossils are still not as common as they are at the popular neighbouring sites of Tankerton and Herne Bay. Eocene, Foreshore, Rating: ♦♦
The striking red and white cliffs at Aust, on the Severn Estuary, expose the Rhaetian Penarth Group, home to one of the most famous bone beds in the UK. This thin but highly productive layer is packed with teeth, fish remains and reptile material, making Aust the richest Triassic fossil site in Britain. Under the right conditions, the foreshore can yield a wide variety of microfossils, rewarding careful searching and sieving. Triassic, Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦♦
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For those who have visited Watchet in Somerset looking for fossils in the Blue Lias, this location will seem remarkably similar. Indeed, the same fossils can be found in thick limestone bands and soft shale. Hock Cliff is a classic Jurassic location to explore. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦
On the opposite side of the River Severn from the famous Aust Cliff, there are the much less famous Sedbury Cliffs. At what first appears to be a location similar but far less productive than Aust, it is actually a very productive location for Jurassic fossils. Triassic, Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦
Further up the River Severn from the other classic sites, such as Aust and Hock Cliff, Westbury-on-Severn (also known as Garden Cliff) is one of the finest localities for collecting from the famous Rhaetian- aged bone bed from the Penarth Group. Out of all of the localities along the Severn, this has the most rapid erosion. Triassic, Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦
Soudley Valley has a geological trail, taking you through the geological features of the Forest of Dean. One of the locations on the trail features a spoil heap of Carboniferous coal measures, where you can find fossil plants. This guide concentrates on this location.Carboniferous, Spoil, Rating: ♦♦
Crickley Hill is now part of a national park, where there is an official geological trail with an Iron Age hill fort nearby. There are a few sites along the official guide taking you through the geological history of the area, but this guide concentrates on the Crickley Member (formerly known as Pea Grit) quarry of the Birdlip Limestone. Jurassic, Disused Quarries, Scree, Rating: ♦
The actual site is a foreshore location on the eastern shore of the River Severn to the west of Tites Point, in Gloucestershire. At low tide, the Silurian Ludlow beds are exposed, yielding a range of fossils, including seeds, plants and molluscs. However, of most importance is the abundance of fish remains from the Ludlow Fish Bed. Silurian, Foreshore, Rating: ♦♦♦♦
Wainlode Cliff is a less popular location for collecting fossils from the Triassic bone beds of the Rhaetic aged rocks of the Westbury Formation than, for example, Aust. The cliff height is quite impressive, but the problem is this location is more overgrown than others, and does not wash out as regularly. The taller cliffs also mean that the bone bed is inaccessible and unfortunately rarely falls.
Triassic, Jurassic, Cliffs and Foreshore, Rating: ♦♦
The two large quarry faces at Robinswood hill are sites of special scientific interest (SSSI), as they expose the best inland section of early Jurassic rocks in the country. As such, fossil hunting is limited. However, some fossils may be collected from loose material and the views from the top of the hill are worth the walk. Jurassic, Disused Quarry, Rating: ♦♦
A pleasant few hours can be spent at Leckhampton Hill. There are numerous old quarry faces with piles of scree to investigate. Fossils are not abundant but, with patience, some should be collected. The views from this hill are impressive and the walk to the various sites is an enjoyable (if hilly) one. Jurassic, Outcrops, Disused Quarries, Rating: ♦♦♦
There are many old quarries on the west side of the elevated golf course at Cleeve Hill and on top of the common itself. Fossils are varied and abundant, and plenty can be collected from scree below the faces. However, the in situ rock should not be hammered. Views from the top of Cleeve Common, the highest hill in Gloucestershire, are stunning. Jurassic, Disused Quarries, Rating: ♦♦♦
This is a disused railway cutting, hidden away in a thick forest. The small cutting has good exposures of Inferior Oolite and this location is well documented for its Clypeus sinuatus flat echinoids, but many brachiopods and bivalves can also be found. Jurassic, Disused Railway Cutting, Rating: ♦♦♦♦
The Forest of Dean is full of evidence of past coal mining. This old spoil head in Whitecroft, although overgrown, contains some excellent shale full of fossil plants. It is a shame the site is so overgrown, which means you will need to do some digging. Carboniferous, Spoil, Rating: ♦♦♦
There are nearly always people collecting at Bracklesham Bay. Fossils can simply be found washed up on the sand, and you can normally come back with bags full of decent finds, especially sharks’ teeth. During scouring tides, the fossiliferous Bracklesham Formation form the Eocene is exposed and the beach can be covered with ray and sharks’ teeth, and also bivalve shells. Occasionally, you can find corals, but you will definitely find lots of the often overlooked, large, single-celled foraminifera (Nummulites laevigatus). Eocene, Foreshore, Rating: ♦♦♦♦♦
This location is highly fossiliferous, with chalk packed with ammonites, echinoids, brachiopods, bivalves and crinoids. This is one of the best chalk locations in the UK and is full of surprises. It is highly recommended to all fossil hunters who love the chalk. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦
This site is world famous for its highly fossiliferous chalk, which is packed with a wide range of different echinoids, brachiopods, bivalves and crinoids. This is one of the best chalk locations in the UK for its variety of fossils and is recommended to all keen chalk fossil hunters. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦
This popular location near Hastings has yielded some important finds over the years. Sharks’ teeth, plants, reptile remains and shells can all be collected, and the site is exceptional for small mammal and fish remains. Crocodile teeth can also sometimes turn up. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
Hastings is one of the only places outside of the Isle of Wight where dinosaur bones can be found and this popular and important site has yielded some important finds over the years. Fish, shark, plant, reptile remains, bivalves and gastropods can also be collected. Keep a look out for dinosaur footprints. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦
This is a classic British chalk location and a must for experienced fossil hunters. This guide concentrates on access from Cow Gap to Beachy Head. Over just a relatively short distance, fossils can be collected from the White Chalk Subgroup and Grey Chalk Subgroup. Please refer to the Eastbourne guide for the Eastbourne to Cow Gap section. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦
Bognor can be an outstanding London Clay location. Unlike the classic sites of Kent and Essex, this site yields insects, plant remains and a large number of brachiopods and bivalves. Some of these shells are enormous. When beach conditions are favourable, expect to find lots. Eocene, Foreshore, Rating: ♦♦♦♦
Bexhill was made famous after the storms of November 2000 exposed dinosaur trackways on the foreshore. Since then, collectors have been finding a wide range of fossils, including fish, crocodile, turtle and dinosaur remains. Cretaceous, Cliffs and Foreshore, Rating: ♦♦
Some lovely echinoids can be found in the chalk at Peacehaven, including some superb, large Echinocorys cincta. This locality is also good for fish remains, which can sometimes be found on the foreshore. Fossils at Peacehaven are best found during scouring conditions. They can also be found in the fallen blocks on the beach. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
Birling Gap is situated between the Seven Sisters and Beachy Head. Indeed, both of these locations can also be visited from Birling Gap on a retreating tide. However, due to dangerous tides along this part of the coastline, these three locations have been split into separate guides, with separate access points. This guide concentrates on the area around the access point of Birling Gap. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
Depending on foreshore conditions, this can be an excellent location for chalk fossils. There is a foreshore platform immediately to the right of the steps, which is extremely rich in echinoids. You can see vast numbers of damaged ones in the rocks of the foreshore, but, if you look harder, you should be able to find some complete specimens. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦
Many echinoids can be found at Newhaven, in particular, Offaster pilula, which is very common – certain chalk blocks can be split open to yield numerous specimens of this small species. Also abundant (but often incomplete) are Echinocorys. If you walk as far as Peacehaven, you may be lucky enough to spot giant ammonites (probably Parapuzonisa or Havericeras) in the wave-cut platform. Do not hammer or damage these. Leave them for others to see – they are too big to get home and should not be touched. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
Cooden is located at the western end of the town of Bexhill. Along the foreshore, exposures of Weald Clay and Tunbridge Wells Sand can be seen. Fossils – including dinosaurs, crocodiles, turtle, plants and fish remains – can be found here. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
The Wren’s Nest National Nature Reserve is an area of nature reserve to the northeast of Dudley in the West Midlands. It was designated as a National Nature Reserve in 1956 because of its exceptional geological and paleontological features of Silurian age. It is also a SSSI. Silurian, Disused Quarry, Rating: ♦♦♦♦♦
Situated on the border of Warwickshire and Oxfordshire, this quarry is popular with schools. These are able to visit and collect fossils from a designated area, where the quarry regularly dumps fresh material on a spoil heap. Rich in echinoids and now an SSSI, this is a site definitely worth visiting, if permission can be obtained. Jurassic, Disused Quarry, Rating: ♦♦♦♦♦
Wootton Bassett is an incredibly interesting and unique location. Fossils are found in a stream, which washes them from the famous ‘Wootton Bassett Mud Spring’. The mud spring erupts from time to time, bringing fossils from the underlying Ampthill Clay to the surface, where they are washed out by a stream from the spring. While the spring itself is fenced off, the stream is accessible. Jurassic, Stream Embankment, Rating: ♦♦♦♦♦
This disused sandpit (known as the Sahara Sandpit) is now being used for landfill, but a special area has been designated as a RIGS, because of its geological importance. Entrance to the site can be obtained by prior arrangement from the occupants of the house next to the sandpit, who will open the gates for you. They are usually very accommodating to visitors. Jurassic, Disused Pit, Rating: ♦♦♦
It has only been in recent years that Bawdsey is once again being washed out by the sea, but this time it is a small cliff north of the famous (now overgrown) Red Crag cliffs. However, the London Clay on the foreshore is rich in fish, bird and shark remains. Eocene, Pliocene, Cliffs and Foreshore, Rating: ♦♦♦♦
Ramsholt is one of the best fossil sites in Suffolk, exposing a diverse range of deposits from the London Clay, Red Crag and Coralline Crag. The foreshore yields shark teeth, shells, corals and echinoids, along with more exceptional finds such as complete crabs, lobster remains and fish material from the basement bed. With multiple fossil-bearing layers present, it offers a varied and highly rewarding collecting experience, particularly after favourable tides and erosion.Eocene, Pliocene, Cliffs and Foreshore, Rating: ♦♦♦♦♦
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During favourable scouring conditions, Easton Wood exposes Norwich Crag shell beds along the foreshore. These are extremely rich in mammal remains and are the best preserved bones from any Norwich Crag site. Although highly productive, scouring only occurs every few years, although after gale force storms, mammal remains can often be washed ashore, lifted by the waves from the seafloor. Shell beds are also sometimes exposed in sporadic pockets along the cliff, but bones from these upper shell beds are rare. Pliocene, Cliffs and Foreshore, Rating: ♦♦
