Foraminifera (forams) are single celled organisms belonging to the Protista kingdom. Their fossils have been found in rocks from the Cambrian period onwards, and they are still living and abundant today. Forams generally inhabit marine […]
Foraminifera (forams) are single celled organisms belonging to the Protista kingdom. Their fossils have been found in rocks from the Cambrian period onwards, and they are still living and abundant today. Forams generally inhabit marine […]
Flint meal is a rich source of siliceous microfossils. The material is often packed with sponge spicules, as well as foraminifera and ostracods. To collect flint meal unweathered, fresh flints recently eroded out of chalk […]
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: ♦♦♦♦
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: ♦♦♦
Hengistbury Head is at the most easterly end of Dorset and is a popular area for hikers. The cliffs are tall, but surrounded by water, with Christchurch Harbour just 400m round the corner to the east. These are Barton Age and are rich in fossil seeds. Therefore, this is an ideal location for the microfossil collector. Eocene, Cliffs and Foreshore, Rating: ♦♦♦
Microfossils can be obtained from the Grey Chalk Subgroup (formerly the Lower Chalk, minus the Plenus Marls) with great ease. This rock has a high clay content in comparison with the whiter chalks and breaks […]
Seatown is one of Dorset’s classic fossil-hunting locations, offering rich Jurassic material set against some of the most dramatic coastal scenery on the south coast. However, it can be more dangerous than many nearby localities due to the exceptionally high and unstable cliffs, so care is always required. Fossils are commonly found loose along the foreshore, with some of the finest specimens—particularly ammonites—preserved within hard nodules that require careful preparation. During periods of strong coastal scouring, belemnites can occur in abundance across the beach.Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦♦
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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: ♦♦♦♦♦
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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Flodigarry is a very picturesque beach, with amazing views and Oxfordian sediments, containing good pyrite and calcite fossils. The wild seas can add drama to this location, and the wildlife is second to none. This is a great place to spend a day with a picnic and a look for fossils on the low tide. Jurassic, Cliffs and Foreshore, 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 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: ♦♦♦♦