Tag: Fossils

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Osmington Mills

The section of coast, east of Ringstead Bay, between Bran Point and Osmington Mills, expose a superb succession of Corallian (Middle Jurassic) rocks, which reveal the entire sequence of the Osmington Oolite Formation and other beds, which are rich in fossils. A good variety of fossils are found in broken rocks from rockfalls and along the foreshore, which may be collected. Ammonites, bivalves and gastropods and trace fossils are common finds.Jurassic, Cliffs and Foreshore, Rating: ♦♦♦

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Bowleaze Cove

The Oxford Clay and the Corallian Beds at Bowleaze Cove in Weymouth (Furzy Cliff) can yield bivalves and ammonites and in the past the clay was particularly rich in marine reptile remains. Giant fossil oyster shells are plentiful. These locations are best after scouring tides and/or rain. You will need wellington boots or good walking boots, towards the east, the terrain is tough going towards Redcliff Point. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦

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Lulworth Cove

Lulworth Cove is a popular tourist location and its famous ‘Fossil Forest’ can be visited at low tide. It is ideal for children and makes for a great whole day out. However, fossils are less common than at other Dorset locations nearby. Jurassic, Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦

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Ringstead Bay

Ringstead Bay is a wonderful location, with rocks and fossils from the Corallian, Kimmeridge Clay, Purbeck Beds and Portland Beds to be found. The site consists mostly of Kimmeridge Clay from the Upper Jurassic. It is rich in fossils and with easy parking, toilets and refreshments nearby; it’s an ideal, safe location for the family. The site is productive in either direction from the access point. This location is also just a short walk away from other good sites and makes for an ideal day trip. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦

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Kimmeridge Bay

If you are intending to use Kimmeridge Bay as the start of a trip to get to other nearby sites, this can be one of the most dangerous locations for fossil hunting. The tides have cut many people off in the past. Kimmeridge Bay and the adjacent cliffs and foreshore are rich in ammonites, reptiles and shells, but the best collecting sites to the east are a long walk if you are planning to look for fossils along the coastline from Kimmeridge Bay to Chapman’s Pool. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦

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Burley Hill

There are three sites at Burley Hill, giving the opportunity to collect Carboniferous corals and brachiopods from a small cutting, scree slopes and the hillside. There is plenty to be found here and it makes for a fantastic day out. It is also within an Area of Outstanding Natural Beauty (AONB). Carboniferous, Cuttings and Scree, Rating: ♦♦♦

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Llangollen

Llangollen is Carboniferous Limestone scenery heaven. About a kilometre and a half north of the town, the Eglwyseg Escarpment presents some really fantastic views. What’s more, among the huge amount of scree that covers its scarp slope, fossil brachiopods and corals can be found. Carboniferous, Scree Slope, Rating: ♦♦♦

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Seaton Sluice

Seaton Sluice at the north end of Whitley Bay is an excellent chance to collect fossils from the Carboniferous coal measures. Coal itself can be seen in the rocks which are also rich in plant remains, corals and bivalves. An easy location to access and fossils are common. Carboniferous, Cliffs and Foreshore, Rating: ♦♦♦♦

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Gristhorpe

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: ♦♦♦

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Crook Ness

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: ♦♦

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Brook Bay

Brook Bay is popular for dinosaur fragments along the beach. Here, many rolled fragments get caught up in the shingle and you can find these remains by simply searching along the foreshore. Other reptile and larger bones can also be found. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦

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Beer Head

The chalk at Beer Head is very hard, unless you are lucky enough to find boulders on the foreshore from the softer beds at the top of the cliffs. There are a huge variety of echinoid species to be found here and the location is also well known for ammonites, brachiopods and bivalves. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦

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Fremington

Along the banks of the River Taw at Fremington, rocks from the Devonian age can be seen packed with brachiopods and bivalves. The site is easy to access and makes a wonderful day out. All you need is a good eye and to stroll along the banks. Devonian, Foreshore, Rating: ♦♦

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Watton Cliff

Watton Cliff, part of West Cliff at West Bay and is an excellent location for collecting microfossils. While the site is also rich in other fossils (such as brachiopods, crinoids, fish, sharks’ teeth, crocodiles, amphibians and plants). ihis guide concentrates more on the microfossils, including small mammals, fish, reptiles and ostracods, which are well preserved and abundant. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦♦

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Durlston Bay

This is a location for the experienced and fit fossil collector! The wild, rugged coast and dangerous terrain of Durlston Bay make this site a challenge but you’re often rewarded with microfossils, tiny mammal remains, turtle shell and bone, crocodile bone and skin fragments, with fish and reptile remains, including dinosaur footprints. Take samples for wet sieving and don’t forget your field lens when visiting. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦

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Swanage

This Cretaceous site represents an alternative to the many Jurassic sites of Dorset. It yields fossils from the chalk, including echinoids, bivalves, brachiopods and ammonites. However, fossils here are, less common than other chalk locations in Dorset. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦

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Eype

Continuing from Seatown, what used to be known as the Beacon Limestone (formerly the Dorset Junction Bed) at Eype yields plenty of ammonites, but will require some hard work with a large geological hammer. Many of the fossils are also poorly preserved, but decent specimens do turn up, if you look hard enough. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦

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Corton

Ammonites, belemnites and reptile remains can all be found in the boulder clay, along with many erratic rocks full of shells. The foreshore sometimes yields fossil wood, seeds and bone from the Forest Bed during times of scouring. This used to be a highly productive site, but the sea defence limits scouring.Pleistocene, Erratics (Jurassic, Cretaceous), Cliffs and Foreshore, Rating: ♦♦♦

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Capel Green

The pit at Capel Green provides an excellent opportunity to collect shells from the Red Crag. It is next to the road and disused, but has two large, clear faces full of shells. In addition, shells can be collected from the quarry floor or the nearby spoil heap. Evidence of cross bedding is also clearly visible. Pliocene, Part Worked Pit, Rating: ♦♦♦

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Broom Pit

The Coralline Crag at Broom Pit is extremely fossiliferous and rich in a wide variety of molluscs and bryozoans. You will be sure to come home with plenty of finds. The shells are in excellent condition and some are very large. It is a site definitely worth visiting. Pliocene, Disused Pit, Rating: ♦♦♦♦♦

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Folkestone

Folkestone is internationally famous for the ‘Channel Tunnel’, but also for the cliffs of Gault Clay at Copt Point and in the Warren and East Wear Bay. These rapidly eroding cliffs yield a vast range of ammonites, crabs, echinoids, belemnites, brachiopods, bivalves and much, much more. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦

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Samphire Hoe

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: ♦♦♦♦♦

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Kingsdown

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: ♦♦♦

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Dumpton Gap

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: ♦♦

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Birchington

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: ♦♦

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Freshwater Bay

Freshwater Bay is the best place on the Isle of Portland to access the Portland Stone. Here mollusc’s and ammonites can be found, although the later is not common, along with trace fossils. You can collect from the cliff-top quarry or from the foreshore. Jurassic, Cliffs, Foreshore, Disused Quarry, Rating: ♦

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Studland Bay

The famous plant beds from the Poole Formation used to be found at Bournemouth, but, after the sea defence was constructed, this bed gradually became obscured and today it can hardly be seen. However, the Poole Formation can be found at Studland Bay, which also yields some plant remains. Eocene, Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦

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Pinhay Bay

Pinhay Bay is both geologically interesting and a less popular location that can provide a good variety of fossils to be found, ranging from Triassic rocks, the Jurassic Lower Lias and from the Cretaceous Chalk. Jurassic, Cretaceous, Cliffs and Foreshorem, Rating: ♦♦♦

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Croyde

Within the Baggy Beds at Baggy Point, layers of sandy deposits yield corals, bryozoans, brachiopods, bivalves and crinoids. However, these deposits can sometimes be hard to find and the fossils are poorly preserved. Devonian, Cliffs and Foreshore, Rating: ♦♦

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East Runton

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: ♦♦♦♦♦

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Sheringham

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: ♦♦

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Dalmellington Burns

There are a few burns around the village of Dalmellington, which have cut into fossiliferous Carboniferous shale. The most common finds are mussels, but plant remains can also be found. This location is best visited after a dry spell, because, if the water is too high, the beds are not exposed. Carboniferious, Stream Cutting, Rating: ♦♦

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Saltcoats

A small area at Saltcoats yields plant remains. Although much of the rich Carboniferous beds have been washed away by the sea, and fresh beds have not been exposed due to the sea defence, you can still occasionally find plant remains in the shale on the foreshore. However, most of the shale today is unproductive. Carboniferous, Cliffs and Foreshore, Rating: ♦♦

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Kirkcudbright

The coastline to the south of Kirkcudbright has low cliffs of shale, which is also exposed along the foreshore. There are several areas where the shales contain fossils from certain zones, although these are very hard to find. Graptolites, cephalopods and crustaceans can all be found. Silurian, Cliffs and Foreshore, Rating: ♦♦