Offerton is superb for fossil ferns, roots and trunks, which can all be found in a small river cutting. The specimens are very well preserved and the brownish leaves are much clearer to see here than at most other Carboniferous plant locations. This is an outstanding site where you will certainly come back with many good quality specimens. Carboniferous, Stream Cutting, 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: ♦♦♦♦♦
Newhey Quarry is full of Calamities (fossil stems of giant, tree-like horsetails), bivalves, and brachiopods. Some of the most interesting finds at this site are the superb trace fossils, including ripple marks, worm burrows and ‘fish marks’.Carboniferous, Disused Quarry, Rating: ♦♦♦
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. Pleistocene, Cretaceous, Cliffs and Foreshore, 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: ♦♦♦♦♦
The chalk at Weybourne yields echinoids and brachiopods, but resting on this is the Wroxham Crag. This yields mammal and fish remains, along with a wide variety of molluscs in the thick shell beds and crag sands. Pleistocene, Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
East Runton is the best location for mammal remains from the Pastonian Stage interglacial. It also is one of the only locations where you can see younger Pleistocene beds below huge chalk cliffs. The chalk was transported here during the ice age and is spectacular to see. Pleistocene, Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦
Overstrand is a foreshore collecting location. Chalk is exposed during low tide, especially during scouring conditions or winter/spring months. The chalk is highly fossiliferous, yielding many echinoids, sponges and molluscs. Pleistocene, Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦
Happisburgh has always been infamous for its rapid rates of erosion, but more recently, deep and regular scouring is yielding a phenomenal amount of mammal remains from the Forest Bed. It is now quite common to find mammoth molars lying around on the beach, as well as a whole range of other mammals, which are washed from the beds both below beach level and at the lower part of the cliff.Pleistocene, Cliffs and Foreshore, Rating: ♦♦♦♦
Near the lifeboat station on the foreshore, chalk is exposed during scouring conditions. Corals and shark remains have been found at this location at these times, although scouring only happens a few times a year. If you do visit during favourable conditions, you should find some nice specimens. Cretaceous, Cliffs and Foreshore, Rating: ♦♦
The cliffs from Trimingham to Sidestrand are some of the most spectacular glacial formations along the northern Norfolk coast. These tall, rapidly eroding cliffs here display an array of various colours from the sands, tills and clays. Fossils are mostly Jurassic and Cretaceous erratics. Erratics (Jurassic, Cretaceous), Cliffs and Foreshore, Rating: ♦♦
Trimingham has the youngest chalk on the UK mainland, from which a few shells can be found in a small cliff face. The chalk has actually been tilted and folded by glaciation, and is a geologically important site. There is easy access onto the beach, although the road turning is easily missed. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦
Mundesley was once an important site for Cromer Forest Bed material, with a number of large vertebrate specimens being found from foreshore deposits. Today, the sea defence prevents this bed from being washed out, although the occasional bone can turn up. However, erratic fossils, mostly of flint echinoids and sponges, can be found. Pleistocene, Cretaceous, Cliffs and Foreshore, Rating: ♦♦
This location consists of a series of locations along a designated geological route in Mortimer Forest. You can collect a large number of superb corals, brachiopods, bivalves and trilobites from various cuttings and all the fossils are in superb condition. It is an excellent walk too. Silurian, Cuttings, Rating: ♦♦♦♦♦
Many Silurian fossils, such as crinoid pieces, corals and brachiopods, can be collected at this National Trust managed limestone escarpment. The tourist information centre and museum in Much Wenlock is also worth a visit to learn a little more about the location and to view fossils from the area. Silurian, Cutting, Rating: ♦♦♦♦♦
This quarry is overgrown, but still has lots of fossils. Good exposures of the Wenlock Limestone yield a variety of corals, shells and trilobites. It is quite large, with three main sections. Silurian, Disused Quarry, Rating: ♦♦♦
This is another walk along a designated geological route visiting two stream sections and two further cuttings, including an old railway cutting and a quarry. The rocks here are Silurian, Ordovician and Pre-Cambrian. Shells, graptolites and trilobites can all be found. Silurian, Ordovician, Cuttings, Stream, and Disused Quarry, Rating: ♦♦♦
Fossils can be found in shales, which outcrop in the stream banks of the Hope Valley stream near the nature reserve. Finds are few and far between, but occasionally a nice, whole trilobite can be collected. Ordovician, Stream Embankment, Rating: ♦
This is a stream section, which has been cut back into highly fossiliferous Silurian rocks. Plenty of excellent corals can be found, along with brachiopods, bivalves and trilobites. Most of the fossils have been washed out from the rocks and are just lying in the stream. Silurian, Stream, Rating: ♦♦♦
This location is so over collected that you have to crawl into the cutting and it can be hard to get any decent rock samples for splitting, but the rewards are worth the hard work. Superb trilobites and graptolites in excellent condition can be found, and some are complete. Silurian, Stream and Cuttings, Rating: ♦♦♦♦♦
This is a beautiful location, surrounded by luscious, green rolling countryside. Betton Dingle offers trilobite fossils, a pleasant walk and the guarantee of getting wet. Not a site for the unadventurous. Ordovician, Stream Embankment, Rating: ♦♦♦♦
This is a small roadside cutting, which yields brachiopods and trilobites. The fossils here are poorly preserved in soft mud stones and will require treatment quickly, but it is an ideal location to stop off by the road side with a grass lay-by. Silurian, Roadside Cutting, Rating: ♦
The area around the town of Coniston from which fossils and minerals can be collected is quite large. It includes several quarries, and several becks and scree slopes. There is also a number of small cuttings. Graptolites and trilobites can be collected here, along with brachiopods. Silurian, Ordovician, Cuttings, Disused Quarries, Rating: ♦♦♦
Whitehaven is one of the only places in the UK where fossil plants from the Carboniferous can be collected on the coast both on the foreshore and in the cliffs. This unique location can yield some well-preserved specimens. Carboniferous, 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: ♦♦♦♦
At Stockdale Beck, Silurian rocks have been cut through by water and various zones are exposed. There is one particular zone in which well-preserved graptolites can be found. Silurian, Stream, Rating: ♦
At Stockdale Quarry, Ordovician slates yield a variety of fauna including trilobites, corals, graptolites, brachiopods, bivalves and gastropods. This disused quarry is situated at the top of a large hill. Ordovician, Disused Quarry, Rating: ♦♦
Unworked since the early twentieth century, Clints Quarry is now quite overgrown. Some areas of scree can still be found, but fossils are becoming less common. This is a site of special scientific interest (SSSI). Carboniferous, Disused Quarry, Rating: ♦♦
Not is not a location for fossil hunting, but a wide range of minerals can be found from the Duddon Hall Tuff Formation in the Borrowdale Volcanic Group. Most of the disused quarries here are now filled with spoil, but are still productive. Ordovician, Disused Quarry, Rating: ♦♦♦
The fossils found at Hodgson How Quarry can be seen in the local Keswick Museum, where there are some superb and unusual species of graptolites. These are common in the beds at this disused quarry. In fact, this is one of the best graptolite locations in the Lake District. .Ordovician, Disused Quarry, Rating: ♦♦♦
Most of the old clay pits have been swallowed up by the building of huge housing estates to the south of Peterborough. However, one area at Yaxley has been left as a nature area, with public byways taking you around the rim of the pits, which are now filled with water. On the banks, the Oxford Clay is rich in fossils. Jurassic, Lake Embankment, Rating: ♦♦♦♦♦
Famous for its high number of reptile remains, this location has been the site of some complete skeletons in the past, but also yields fish remains, ammonites, belemnites, bivalves, brachiopods and crinoids. There is also a ‘fossil hunting area’ in the disused part of the pit, which the general public can collect from and which is regularly replenished from spoil from the main pit. Jurassic, Working Quarry, Rating: ♦♦
The Devonian rocks at Pendower Beach contain shell impressions, but are poorly preserved and trilobites are extremely rare. However, as with all Cornish fossil locations, this site is mainly for fossil enthusiasts and geologists who are not expecting lots of finds, but who can appreciate an interesting location. Devonian, Cliffs and Foreshore, Rating: ♦♦♦♦
The Bude Formation, magnificently exposed in the cliffs of this popular tourist destination, is poor in fossils. However, the formation does boast a unique, 300-million-year-old fish, the goldfish-sized Cornuboniscus budensis, found nowhere else in the world! Plentiful crinoids and solitary corals can be seen (but not collected) in quarried limestone blocks used to build parts of Bude breakwater in the early 1800s). Carboniferous, Cliffs and Foreshore, Rating: ♦♦
Widemouth Bay contains a number of popular holiday parks, situated with easy access to the sandy beach. This is a well-known tourist hot-spot, especially for surfers, yet few realise that it has spectacular geological features and yields a variety of Upper Carboniferous fossils. Carboniferous, Cliffs and Foreshore, Rating: ♦♦♦
Sandy Mouth is the most northerly coastal Lower Carboniferous location in Cornwall, where plant remains can be found. Here, the rocks consist mostly of the Bude Sandstones, but the upper beds, which consist of mudstones and siltstones, often fall down onto the beach. These contain plant remains, which are fairly common. Carboniferous, Cliffs and Foreshore, Rating: ♦♦♦
Maer Cliff is accessed from the popular tourist beach of Northcott Mouth. The most common finds here are from the Upper Carboniferous and consist of plant and fish remains, together with burrows and tracks within nodules. In addition, plants and fish scales can be found loose within the layers of shale. The site is easily accessed and suitable for children. Carboniferous, Cliffs and Foreshore, Rating: ♦♦♦
Rusey Cliff is one of the few places in Cornwall where well-preserved fossils can be collected. Plant remains can be found in slabs of the Lower Carboniferous-aged Boscastle Formation, and corals, brachiopods and goniatites can be found in similar aged limestone rocks along the foreshore. The site can be accessed by walking along a cliff top footpath, which takes you through a large area of landslip. Carboniferous, Cliffs and Foreshore, Rating: ♦♦♦
Crackington Haven is a small, but popular location, which has outstanding views. Fossils have been found on both sides of this small cove, but unfortunately it has become over collected. Today, fossils can be difficult to find and those within the bedrock are SSSI protected. Carboniferous, Cliffs and Foreshore, Rating: ♦♦
Upton Cross is situated between Widemouth Bay and Bude. The Bude Formation, which is Carboniferous in age, sandwiches outcrops of shale at two areas of the cliff and foreshore. These contain nodules that yield fish remains, worm tubes and tracks. Carboniferous, Cliffs and Foreshore, Rating: ♦♦
Wanson Mouth is located just to the south of Widemouth Bay. It is a privately owned beach, but with public access permitted and no restrictions on collecting fossils. It is also a quick and easy site to access, with some excellent Upper Carboniferous fossils to be found, such as goniatites, ostracods, molluscs and worm tubes. Carboniferous, Cliffs and Foreshore, Rating: ♦♦♦
Foxhole Point features the Crackington Measures, which continue from Widemouth Bay. While it is possible to walk here from Widemouth Bay, it is best accessed from the village of Millook to avoid a long walk over difficult terrain. Plant remains and goniatites can be found here from the Upper Carboniferous. Carboniferous, Cliffs and Foreshore, Rating: ♦♦
An old, cliff top quarry, situated along the coastal footpath near Boscastle, was once rich in trilobites. Today, most of the quarry has fallen into the sea, but a small part still exists with blocks that can yield fossils when split. Devonian, Disused Quarry, Rating: ♦
Castleton has long been known for its Carboniferous Limestone, its caves and for the Blue John semi-precious stone mined here. Much of the area is owned by the National trust and is designated an site of special scientific interest (SSSI). This means that fossils can only be looked at and photographed, but must not be collected. Carboniferous, Outcrops, Rating: ♦♦♦
Monsal Dale, near Little Longstone, is set among breathtaking scenery. Carboniferous fossils can be found here, such as crinoid pieces in limestone and chert. Carboniferous, Outcrops, Rating: ♦♦♦
Set within the rolling Peak District countryside, Parkhouse Hill, near Earl Sterndale, is a beautiful location with various types limestone reef fossils. The view from the top of the hill is nothing short of stunning. Carboniferous, Outcrops, 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: ♦♦♦
In the village of Holymoorside, a public footpath takes you to a small quarry that yields small plant and stem remains from the Carboniferous Wingfield Flags Formation. Stem fragments are the most common find here. Carboniferous, Disused Quarry, Rating: ♦♦
Marsh Brook cuts through Carboniferous marine deposits. These are rich in goniatites, bivalves and gastropods, but also contain many other types of fossils. Often, these are not particularly well preserved, being flattened, but the shale is also extremely rich in well-preserved microfossils. Carboniferous, Stream Embankment, Rating: ♦♦♦♦
This is a large quarry owned by the National Stone Centre. It exposes the Eyam Limestone Formation, which is full of excellent corals, crinoids, bivalves and brachiopods. Access is easy by entering the National Stone Centre. Carboniferous, Disused Quarry, Rating: ♦♦♦♦
