The Chilcompton site is an old spoil heap form coal mining days, with a publically accessible footpath through the middle. Although now overgrown, the footpath still provides coal measure shale debris, which yields plant remains. Carboniferous, Spoil, Rating: ♦♦♦
Stocker Hole is a large disused quarry to the south of Radstock, The quarry has a footpath running right through the middle and contains Carboniferous Black Rock Limestone. Corals, and brachiopods are the most common fossils here, with Bryozoans also being found. Carboniferous, Disused Quarry, Rating: ♦♦♦
Brown’s Folly is located in a nature reserve. Fossils can be found everywhere in the old quarries in the area and many exposures of Great Oolite can be seen. The reserve is managed by the Avon Wildlife Trust and kept clear by the Bath Geological Society. The site is an SSSI, so no hammering on the bedrock is allowed, but loose material can be picked up and collected. Jurassic, Disused Quarry, Rating: ♦♦
The entire section of coast along Compton Bay provides a worthwhile day out, with opportunities to find pieces of dinosaur bone (mostly rolled) and possibly teeth; and to see the large number of dinosaur footprints scattered along the coast. This section is famous for the remains and footprints of dinosaurs, for which the Isle of Wight is famous. Both commonly occur on the foreshore. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦
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Yaverland is one of the most famous fossil collecting locations on the Isle of Wight, renowned for its dinosaur remains, vertebrate fossils and classic Wealden exposures. However, despite its reputation, success here depends heavily on conditions. The site can often appear unproductive, particularly during the summer months when the foreshore is covered, but after winter storms and spring tides, fresh material is exposed and excellent finds can be made. Due to its popularity, the site is also heavily collected, meaning patience and persistence are essential. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦
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Brook Bay is one of the Isle of Wight’s most famous dinosaur localities, where teeth, bone fragments, fossil wood and reptile remains are regularly found with careful searching. Most material is worn, but storms and beach scour can reveal fresh specimens. The bay is also renowned for its dinosaur footprints, preserved both in situ and as natural casts on the foreshore, making it a key site for dinosaur discoveries. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦📺 VIDEO
The early Oligocene beds exposed along the coastline at Hamstead Cliff are exceptionally rich in fossils, particularly remains of mammals, crocodiles, turtles, fish and crustaceans. In addition, a wide variety of molluscs, plant material and fossil seeds can often be found scattered across the foreshore. This stretch of coast is widely regarded as one of the most productive fossil locations on the Isle of Wight, offering a remarkable diversity of finds for those willing to search carefully.Oligocene, Cliffs and Foreshore, Rating: ♦♦♦♦♦
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Brighstone Bay is famous for the partial sauropod skeleton found by Portsmouth University, and reptile and dinosaur remains are often found along this coastline. Barnes High was also featured on the live television programme, ‘The Big Dig’. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
Shepherd’s Chine and Whale Chine are superb locations that yields some superb fish remains, lobsters, ammonites, brachiopods, bivalves, and occasional reptile and dinosaur bones. During the right conditions, you can come back with some great specimens. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
The early Oligocene beds along the Coastline at Bouldnor Cliff (Near Hamstead) is highly fossiliferous in mammal, crocodile, turtle, crustaceans and fish remains. Molluscs, plants and seeds can also be found simply lying on the foreshore. It’s one of the most productive locations on the Island for Fossils providing a rare glimpse into life on land and in coastal lagoons around 33–37 million years ago. Oligocene, Cliffs and Foreshore, Rating: ♦♦♦♦♦
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Whitecliff Bay is a geologist’s heaven. Where else can you collect from the Upper Chalk, London Clay, Reading Clay, Bagshot Beds, Bracklesham Beds, Barton Clay, Fishbourne member, Cliff End Member and Totland Bay Member, plus much more? Eocene, Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦
Bembridge Foreland is an important Isle of Wight fossil site, where the Bembridge Limestone and Bembridge Marls are exposed across the foreshore as a broad wave-cut platform and scattered rock outcrops. Best searched on a low tide, these beds are well known for their shelly fossils, especially gastropods and bivalves weathering from the limestone onto the shore. At foreshore level towards the south-west of the bay, the Bembridge Oyster Bed is regularly washed out and is the main source of the site’s vertebrate material, including turtle, crocodile and mammal remains.Eocene, Foreshore, Rating: ♦♦♦
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In a peaceful corner of the Isle of Wight, Rocken End is a less visited location with a small inland quarry. It is ideal for anyone interested in ammonites and other molluscs, and also makes for an excellent day out for all the family. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
Thorness Bay exposes a continuation of the fossil-rich Hamstead Beds and Bembridge Marls, linking the classic Isle of Wight localities of Hamstead and Gurnard Bay. Although generally less productive than those better-known sites, the bay can still yield shells, plant remains, insects and occasional vertebrate fossils, particularly after erosion exposes fresh material along the foreshore and low cliffs. Eocene, Oligocene, Cliffs and Foreshore, Rating: ♦♦♦
Shanklin is a very good location on the Isle of Wight for Lower Greensand fossils, in particular, dinosaur remains and molluscs. When the Lower Greensand is exposed to air and left to dry, it becomes extremely hard. However, when fresh and, especially when exposed on the foreshore, it is like clay. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
Gurnard Ledge is a classic location for finding insects but fish, turtle and crocodile remains can also be found. Today, the famous insect bed has become less productive, but insects and leafs can still be found. Over 200 species of insects have been recorded, including delicate remains such as beetles, flies and wings. Oligocene, Eocene, Cliffs and Foreshore, Rating: ♦♦♦
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Whitby is one of the most iconic fossil localities on the Yorkshire coast, renowned for its rich Jurassic heritage and dramatic cliff scenery. While access to parts of the foreshore is tide-dependent and requires careful planning, the rewards can be considerable. The area is celebrated for its abundant ammonites, marine reptile remains and diverse shell beds, as well as for jet — fossilised wood from ancient conifer-like trees that became highly prized in Victorian jewellery. Its reputation means it is rarely quiet, but with patience and good timing.Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦♦
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Saltwick Bay is one of the most productive sites on the Yorkshire Coast, well known for its abundant ammonites, reptile remains and marine fossils. The foreshore is rich in fossiliferous nodules, often easy to split and frequently yielding well-preserved specimens. The bay is also famous for jet, a form of lignite historically used in jewellery, adding to its geological and historical significance.Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦♦
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Port Mulgrave is one of the most productive fossil sites on the Yorkshire Coast, famed for its abundant ammonites and rich Jurassic marine fauna. Once a thriving ironstone mining harbour, the foreshore now yields a wide range of fossils, including reptile remains, belemnites and nodules packed with ammonites, often exposed after cliff falls and erosion. With its combination of historical interest and exceptional fossil potential, it remains a must-visit location for serious collectors.Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦♦
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Kettleness is one of the most productive fossil sites on the Yorkshire Coast, especially renowned for its abundant reptile remains, often found loose or within nodules along the foreshore. The site is also highly regarded for its ammonites, similar to those found at nearby Port Mulgrave, making it a top location for collectors seeking both vertebrate and invertebrate fossils.Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦♦
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Staithes is a popular and accessible Yorkshire Coast locality, well known for its abundant and easily prepared ammonites. These are commonly found within nodules along the foreshore or weathering out from ledges, often requiring only minimal effort to collect. While productive and close to access points, the foreshore near the beach entrance can be extremely slippery, so care is needed when conditions are wet.Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦♦
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Robin Hood’s Bay is one of the most geologically important sites on the Yorkshire Coast, known for its diverse ammonite fauna and extensive Jurassic exposures. While much of the central bay is covered by boulder clay, the foreshore and reefs to either side can be highly productive. Success here depends on conditions and experience, but with careful searching, a wide range of ammonites and other marine fossils can be found.Jurassic, Cliffs and Foreshore, Rating: ♦♦♦
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Runswick Bay is a highly regarded Yorkshire Coast locality, known for its diverse ammonite fauna and productive foreshore exposures. Under the right conditions, the bay can yield a wide range of ammonite species along with bivalves and other marine fossils, often found loose or within nodules. With its broad beach and regular fresh material from erosion, it can be a very rewarding site for collectors.Jurassic, Cliffs and Foreshore, Rating: ♦♦♦
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Reighton Gap is a useful stop along the Yorkshire coast, offering a mix of Kimmeridge Clay fossils and glacial erratics. When exposed, the clay can yield ammonites and marine shells, although productive layers are often covered and depend on scouring tides. The overlying boulder clay is particularly interesting, producing erratic fossils from Jurassic, Cretaceous and even Carboniferous rocks, giving a wide variety of finds in one location.Jurassic, Erratics (Jurassic, Cretaceous, Carboniferous), Cliffs and Foreshore, Rating: ♦♦♦
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Hayburn Wyke is one of Yorkshire’s most important and rewarding plant fossil localities. This site exposes Middle Jurassic rocks that have yielded an exceptional diversity of fossil flora. The fine-grained sediments here preserve delicate leaf impressions in remarkable detail, offering a rare glimpse into the lush, humid landscapes that bordered the Jurassic sea around 170 million years ago. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦
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Speeton Cliffs are one of the most important Lower Cretaceous sites in the UK, with the highly productive Speeton Clay yielding ammonites, fish, shells and crustaceans. Often compared to the famous Folkestone Beds, the foreshore can be very rewarding under the right conditions. It is also a great location for families, although the clay can become extremely sticky and difficult underfoot in wetter months.Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦
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It is quite a long walk down to the beach, but ammonites are well preserved and often found at this location. They can be found both at the north and south end of Ravenscar, but unfortunately, there is very little beach material and cliff falls are rare. Jurassic, Cliffs and Foreshore, Rating: ♦
Cayton Bay yields ammonites and some superb gastropods, bivalves and brachiopods from the Oxford Clay. These are best found on extreme low tides on the foreshore. This location is best during scouring conditions. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦
This is a very good location if you are into plant remains. The Gristhorpe Plant Bed yields some of the best specimens in Yorkshire. There is a wide variety of plants too, but ammonites and shells can also be found at this location. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦
Cloughton Wyke is an excellent location for finding plant remains. The beds are rich in a variety of flora and collecting is fairly easy. Bivalves can also be found here, along with trace fossils, such as ripple marks and burrows. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦
Filey Brigg is a very famous foreshore platform that extends a long way out at low tide. Many walk along the Brigg, but often do not realise that superb plants and shells can be collected near the cliffs next to it. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦
Scalby Ness is another good location for collecting plant remains. It is not as highly productive as other Yorkshire locations, due to the limited area. However, you can still find some very good plant remains from the boulders on the foreshore. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦
Boggle Hole is to the southern end of Robin Hood’s Bay and is a site of special scientific interest (SSSI). Foreshore exposures of siliceous shales yield a range of trace fossils and, during scouring conditions, some superb ammonites can be found. Jurassic, Cliffs and Foreshore, Rating: ♦♦
You can find reptile remains on the foreshore, along with many ammonites and shells. One of the problems is that the foreshore is extremely slippery and there are very few rocks to search through. It can also be covered with algae. Jurassic, Cliffs and Foreshore, Rating: ♦
The Long Nab Member exposed at Crook Ness yields the occasional plant remains or brachiopod. However, fossils are not easy to find and this location is overgrown in places, but is ideal for an alternative day out (but not recommended if time is limited). Jurassic, Cliffs and Foreshore, Rating: ♦♦
Barton-on-Sea is one of the UK’s most famous Eocene fossil sites, with the Barton Clay yielding hundreds of species of shells, particularly gastropods. The foreshore regularly produces shark teeth, fish remains and occasional mammal fossils, often found loose after erosion. With abundant material and easy collecting, it is an excellent location for both beginners and experienced collectors alike.Eocene, Cliffs and Foreshore, Rating: ♦♦♦♦♦
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Taddiford Gap is a classic site and well documented for mammal and crocodile remains. Shark and other fish remains, along with a wide range of microfossils, can also be found. The latter can be found by sieving from the Crocodile and Mammal Beds. There is also a black bed of sediments containing a huge variety of fossils seeds. Eocene, Cliffs and Foreshore, Rating: ♦♦♦♦
Milford on Sea provides an excellent opportunity to collect a wide range of fossil seeds from the Headon Hill Formation. These are in very good condition, but you will need to take samples home for processing using a sieve. Ironstones can also be found containing bivalves and gastropods. Eocene, Cliffs and Foreshore, Rating: ♦♦♦
During scouring conditions, The famous ‘elephant bed’ is exposed at Stansore point, yielding various mammal remains. To the western end of the car park, fossils can be found in the many blocks both along the footpath to the cliffs and the foreshore. At the western end, foreshore Eocene clays yield microfossils. Pleistocene, Eocene, Cliffs and Foreshore, Rating: ♦♦♦
At Brownwich Cliff, fossiliferous septarian nodules of Bracklesham age are washed onto the shore from offshore deposits. The cliffs at both Brownwich Cliff and Chilling Cliff can occasionally yield fossil molluscs, but the best deposits are those from below beach level, which are full of brachiopods and other molluscs. Pleistocene remains can also be found washed from the gravel beds. Pleistocene, Eocene, Cliffs and Foreshore, Rating: ♦♦♦
At Beckton Bunny, the continuation of the Barton Beds yield brachiopods, gastropods and bivalves. However, the shells are far more sporadic than at Barton on Sea and tend often to be broken. During scouring, exposure of the Chama Beds yields the best specimens. Eocene, Cliffs and Foreshore, Rating: ♦♦
Latchmoor Brook is one of the only places where you can collect fossils in the New Forest. They come from the uppermost Bracklesham Group sediments and the lowermost Barton Clay. The stream and banks are very shallow, which makes collecting here far easier than other stream-based locations. Gastropods, bivalves and fish remains are all common here. Eocene, Stream, Rating: ♦♦♦♦♦
Walton-on-the-Naze is an unpredictable location, which can be highly productive one day and bare the next. It is the best coastal location for fossils from the Red Crag and is famous for fossil bird remains from the London Clay. It also while yields some of the largest sharks’ teeth in the UK (including the rare Carcharocles megalodon), together with plant remains and much, much more. Pliocene, Eocene, Cliffs and Foreshore, Rating: ♦♦♦♦♦
Burnham-on-Crouch has yielded an incredible variety of fossils – you just never know what you will find. There are various species of shark (with teeth and vertebrae being most common fossils), crabs, seeds, fish remains (including ray teeth) and much, much more. Eocene, Cliffs and Foreshore, Rating: ♦♦♦♦
The most productive location for lobster fragments – found in small yellow nodules – this small location with its tiny cliffs can bring some nice surprises. Sharks’ teeth and fish remains can also be found. There are several species of lobster to be collected and it is also rich in microfossils. Eocene, Cliffs and Foreshore, Rating: ♦♦♦♦
What looks like a flat beach behind a concrete seawall actually yields plenty of shark and fish teeth, plant remains and much more. People have been collecting here for years. However, success at this location is subject to beach conditions. Eocene, Foreshore, Rating: ♦♦♦♦
East Mersea can be very popular in the summer, as it is a beautiful area, not far from Colchester. The foreshore is made up of London Clay, with a few sharks’ teeth to be found. This site is also well documented for OIS5 and OIS6 Pleistocene deposits, rich in (among other things) the teeth from small mammals and the shells of molluscs. Pleistocene, Eocene, Cliffs and Foreshore, Rating: ♦♦♦♦
Steeple Bay is very similar to Maylandsea. It is very productive for lobster fragments, which are found in small yellow nodules, and for crabs. There are several species of lobster that can be collected here and it is also rich in microfossils. All fossils are washed out of the London Clay from the low cliffs and foreshore. Eocene, Cliffs and Foreshore, Rating: ♦♦♦♦
Along the Wrabness shoreline of the River Stour and after scouring tides or stormy seas, fossils are washed up from sediments from the Quaternary. These include bones of deer, horse and whale from the Red Crag, with turtles, shells, and shark and fish teeth within cement stones and pyrite concretions from the London Clay. Pliocene, Eocene, Cliffs and Foreshore, Rating: ♦♦♦
Stansgate is situated along the south side of the River Blackwater and is east of the classic London Clay sites of Maylandsea and Steeple. Like these two other sites, phosphate nodules containing lobsters and crabs can be found, with sharks’ teeth and fish remains found loose in the shingle. Eocene, Foreshore, Rating: ♦♦♦
