Smallmouth Sands, located within Portland Harbour near Weymouth, is one of the UK’s most remarkable yet often overlooked fossil sites, exposing the Lower Jurassic Kimmeridge Clay. It is one of the most diverse assemblages of Kimmeridge Clay reptiles anywhere in the world. Fossils are typically tiny but abundant, with collectors finding vertebrate remains, fish, and shells scattered across the foreshore, especially after favourable tides and storms.Jurassic, Foreshore, Rating: ♦♦♦♦
The stretch of coastline from Peveril Point into the eastern half of Durlston Bay exposes part of the renowned Purbeck Limestone Group, one of the most important Late Jurassic–earliest Cretaceous sequences in Britain. This section is particularly known for its accessible ledges and foreshore exposures, where fossils can be found without venturing too far into the more hazardous parts of the bay. Although finds can be small and require careful searching, this area offers a rewarding introduction to the complex lagoonal environments of the Purbeck beds, with a mix of vertebrate fragments, shells and microfossils regularly discovered.Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦
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Totland Bay, on the western coast of the Isle of Wight, is a lesser-known but highly rewarding fossil collecting location. Covering the stretch from the south side of the bay to just before Hatherwood Point, this area exposes part of the Headon Hill Formation, with slipped blocks scattered across the foreshore. Although access can be challenging due to landslips and debris, the bay can yield a wide variety of fossils, particularly gastropods and vertebrate remains.Eocene, Foreshore, Rating: ♦♦♦♦
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Two separate locations near Worth Matravers provide an opportunity to see where, 140mya, sauropod dinosaurs gathered at the shoreline of a shallow lagoon and to visit their incredible trackways. The nearby quarry provides bivalves, gastropods, fish remains, turtle bones and carapace fragments, mammal teeth and bones, and plant remains from this bygone environment. Cretaceous, Quarry (permission required) and Attraction, Rating: ♦♦♦♦♦
Saltcom Bay is found to the south of Whitehaven, directly after the harbour. It yields a variety of Carboniferous fossils from a mix of shale and limestone. The cliffs have been formed from spoil dumped from the coal mine and steel works that previously existed in the area, which are now being eroded. The site is rich in plant remains, fish scales and corals. Carboniferous, Cliffs and Foreshore, Rating: ♦♦♦
Parton Bay is just north of Whitehaven and yields a variety of Carboniferous fossils from a mix of shale and limestone. There are no cliffs here, but material has been washed from the south and dumped from the former steel works and the coal mine that supplied it, containing plant remains, fish scales and corals. It is a safe and easy location, and is ideal for children. Carboniferous, Foreshore, Rating: ♦♦♦♦
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: ♦♦♦♦♦
Tidmoor Point, on the edge of The Fleet lagoon opposite Chesil Beach, is a small but highly productive Oxford Clay locality. Best known for its pyritised and limonitic ammonites, the low cliffs and foreshore regularly yield a wide range of fossils, including belemnites, crinoids, crustaceans, fish and occasional reptile remains. Despite its modest size, it remains one of the most reliable sites for collectors searching for well-preserved Jurassic fossils. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦
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Hooken Cliff is the best location in Devon for finding fossils, in particular, echinoids, ammonites, fish and brachiopods, which are easy to find – you just never know what you may find. They can be found in the White Chalk Subgroup (Seaton Formation) and the Grey Chalk Subgroup and in the Upper Greensand. Cretaceous, Cliffs and Foreshore, 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: ♦♦♦♦
At first site, Besom Hill can seem fairly poor for fossils. However, if you can find the thin Bullion Mine Marine Band, you will change your mind. This band of rock is highly fossiliferous and includes fish teeth, scales, fin spines and other remains. Goniatites and bivalves are also common within this layer. Carboniferous, Disused Quarry, Rating: ♦♦♦♦♦
Blue Anchor exposes a thin but highly productive Rhaetian bone bed within the Penarth Group, yielding abundant reptile, shark and fish remains, similar to the famous Aust site on the Severn Estuary. The foreshore is scattered with blocks ideal for splitting, while the overlying Jurassic beds also produce ammonites and occasional reptile material, making this a varied and rewarding location.Triassic, Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦
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Beltinge, near Herne Bay, is one of the UK’s premier locations for collecting fossil shark teeth, attracting collectors from across Britain and Europe. The foreshore exposes the famous Beltinge Fish Beds, which can yield a wide variety of shark, ray and fish remains. While fossils can be found year-round, the site is most productive during very low spring tides, when the richest layers are exposed and large numbers of teeth can be collected under the right conditions.Eocene, Foreshore, Rating: ♦♦♦♦♦
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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: ♦♦
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: ♦♦♦
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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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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From the Zig Zag path to Durlston Head, the western half of Durlston Bay reveals some of the finest and most complete exposures of the Purbeck Limestone Group in the UK. This section is more rugged and challenging, with steep cliffs, ledges and active rockfall zones, but it is also the most productive for serious collectors. The beds here are famous for yielding tiny mammal remains, reptile material, fish fossils and dinosaur traces, offering a rare glimpse into life in the lagoonal and coastal environments that existed at the end of the Jurassic period. While conditions can be difficult, this part of the bay is one of the most scientifically significant fossil localities on the Dorset coast. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦
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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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Thurso is famous for its rich fish beds, and fish remains (especially scales) can be found everywhere along the foreshore – the rocks are full them. Fish teeth and complete fish have also been found. Devonian, Cliffs and Foreshore, Rating: ♦♦♦♦♦
Achanarras Quarry once constantly yielded complete Middle Devonian fish from the Old Red Sandstone. However, it has been disused for many years and is now over-collected, but still very rich in remains. Complete fish can still be found, but are now rare. Devonian, Disused Quarry, Rating: ♦♦♦♦♦
This is the official ‘Hugh Miller Trail’. Hugh Miller was one of the most important Scottish geologists of the 19th century. Ammonites and fossil fish can be found here. The footpath down to the shore was created by Hugh Miller himself. Jurassic, Cliffs and Foreshore, Rating: ♦♦
Golspie is famous for the castle of Dunrobin. However, few people know that, just below the castle on the foreshore, fossils can be collected in Jurassic rocks. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦
This location is most famously known for being the furthest point in the northeast of the UK mainland. This location is actually highly rich in fish remains (especially large fish scales) from Middle Devonian, John O’Groats Sandstone Group. Devonian, Cliffs and Foreshore, Rating: ♦♦♦♦
Spittal Quarry is home to the famous Caithness Flagstone, There are a few disused pits around, but this quarry is still working. There is a fossil museum close by at Spittal. Devonian, Working Quarry, Rating: ♦♦
At Tarbat Ness, the Devonian rocks can contain small fish remains. Scales can be seen on ledges at the headland within a pebble bed. Larger fish fragments can also be found, but are less common. Devonian, Cliffs and Foreshore, Rating: ♦♦♦
Portishead is an interesting location with both Carboniferous and Devonian rocks. At Battery Point, many corals and crinoids can be collected from the rocks on the foreshore and there are plenty to be found. Further along Woodhill Bay, fish remains are also commonly found. Carboniferous, Devonian, Cliffs and Foreshore, Rating: ♦♦♦
Ketton Quarry is over a mile wide – its size has to be seen to be believed. The rocks here contain ammonites, corals, brachiopods, bivalves, fish and reptile remains, and much, much more. This is a superb location to visit. The quarry has recently been designated SSSI status. Jurassic, Working Quarry, Rating: ♦♦♦♦♦
The famous red and white cliffs of Hunstanton are visited by thousands of people each year simply to see this spectacular natural geological feature. The Red Rock and White Lower Chalk are rich in fossils including echinoids, fish, sharks’ teeth, bivalves and brachiopods, ammonites and more. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦
