Tag: Sponges

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Upper Gilwern Quarry

On the edge of the Brecon Beacons, Upper Gilwern Hill is a site long known for its well-preserved and complete trilobites. The hill is made up of rocks from the Lower and Middle Ordovician, and the privately owned quarry is accessible to parties staying at the onsite Shepherd’s Hut self catering accommodation. The trilobite fossils here are plentiful and the chances of finding a good number is very high. Ordovician, Private Quarry, Rating: ♦♦♦♦♦

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Little Wern

Tucked away in the fold of a valley near Llandrindod Wells, in Mid Wales, sits Little Wern holiday cottage. The cottage has its own small quarry, which is solely open to visitors staying there. And what’s more, it is stuffed full of trilobite remains. Ordovician, Private Quarry, Rating: ♦♦♦♦♦

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Strawberry Wood

This is a disused Carboniferous limestone quarry, within a small wood. It is very rich in fossils. Studies indicate important changes in the palaeo-environments of the deposits and in the varied macrofossil assemblages from the surrounding Carboniferous sediments, which are of similar age. Due to the importance of the site, keep collecting to a minimum. Carboniferous, Disused Quarry, Rating: ♦♦♦♦♦

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Danes Dyke

Famous for its many species of sponges, Danes Dyke is a must go location for anyone into chalk fossils. In fact, this is the best location in the UK for sponges. Echinoids, bivalves, brachiopods and crinoids can all be found too. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦

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Bridlington

The beach at Bridlington is popular with tourists and ideal for children. However, towards Sewerby, the beach becomes increasingly rocky and it is here you can find excellent fossil sponges. Despite these being more common at Bridlington, Sewerby is picked over by collectors, so you are more likely to come across something. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦

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Overstrand

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: ♦♦♦♦♦

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Weybourne

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: ♦♦♦

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West Runton

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: ♦♦♦♦♦