Tag: Wales

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Penarth

Penarth’s north shore reveals red and green Triassic cliffs, pale gypsum and fossil-bearing beach stones. This guide follows the shore north from the pier towards Penarth Head, where loose shell fossils reward careful observation, but tides, unstable cliffs and uncertain collecting permissions demand care. Jurassic, Triassic, Cliffs and Foreshore, Rating: ♦♦♦♦

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Lavernock

At Lavernock Point, the coast records a remarkable transition from late Triassic mudflats to an Early Jurassic sea. Shells, ammonites and vertebrate remains occur in different parts of the succession, and the discovery of Dracoraptor hanigani made the locality internationally known. Careful observation reveals both the fossils and the changing environments that preserved them. Jurassic, Triassic, Cliffs and Foreshore, Rating: ♦♦♦♦

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Llantwit Major

At Llantwit Major’s Cwm Colhuw beach, pale limestone ledges and darker mudstones reveal a fossil-rich Early Jurassic sea. Ammonites and bivalves are the main attractions, often preserved as impressions or shells within the foreshore rocks. The striking cliffs and jointed platforms also make this a rewarding place to see how sedimentary rocks weather and break apart. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦

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Southerndown

Southerndown’s Dunraven Bay brings together a sandy beach, striking Early Jurassic limestone cliffs and fossil-rich shore platforms. Look closely at the Blue Lias and you can see curved oysters, other bivalves, ammonites and traces of life on an ancient seabed. The changing rocks also reveal how a Jurassic sea spread across an older limestone landscape. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦♦

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Gileston

The shingle shore at Gileston, near Limpert Bay, offers a quieter way to look for traces of Jurassic life. Some loose rocks contain shells and ammonite impressions, while small crinoid fragments have also been reported. The interest lies in careful observation of weathered beach stones and in understanding how much older fossils became part of a modern shoreline. Jurassic, Foreshore, Rating: ♦♦

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Abereiddy Bay

Abereiddy Bay is a classic place to see Ordovician graptolites in dark shale. The southern foreshore is especially known for the paired branches of the tuning-fork graptolite, while folded sediments and volcanic rocks around the bay tell a much more varied geological story. Ordovician, Cliffs and Foreshore, Rating: ♦♦♦♦♦

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Nolton Haven

Nolton Haven’s Carboniferous sandstones and shales preserve plant remains from ancient river and coal-swamp landscapes. The main bay and the coast towards Rickets Head offer different views of this history, including large rooting structures best enjoyed and photographed where they lie. Carboniferous, Cliffs and Foreshore, Rating: ♦♦♦

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Porthgain

Above Porthgain’s harbour, loose slate waste records the village’s quarrying past. Fossils are uncommon, but occasional graptolites reward a careful look at natural surfaces, while the cliffs and surviving stone hoppers reveal a much wider geological and industrial story. Ordovician, Cliffs and Foreshore, Rating: ♦

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Whitesands Bay

The northern rocks at Whitesands Bay expose steeply inclined Cambrian beds beside a broad sandy beach. Fossils are sparse, but careful observation of loose rock surfaces may reveal dark impressions of small brachiopod shells, giving a glimpse of the ancient sea in which these sediments formed. Cambrian, Cliffs and Foreshore, Rating: ♦

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Upper Gilwern Quarry

Upper Gilwern Quarry, near Howey in Powys, is known for its well-preserved Ordovician trilobites, from tiny growth stages to occasional complete specimens. Its fine-grained rocks record an ancient marine environment. This privately owned quarry is available to booked accommodation guests under the operator’s current access and collecting conditions. Ordovician, Private Quarry, Rating: ♦♦♦♦♦

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Bettws

A small stream cutting near Bettws exposes Ordovician mudstone with occasional trilobite fragments and graptolites. Its dark, fissile rocks offer a close view of marine life preserved in a much older succession than many of the surrounding Silurian hills. Ordovician, Stream cutting, Rating: ♦♦

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Caim

The coast below Caim reveals fossil-rich Carboniferous limestone, with weathered colonial corals, horn corals and large brachiopods. The ledges and headlands show how marine shells and corals were preserved within a changing shallow-water environment. Carboniferous, Cliffs and Foreshore, Rating: ♦♦♦♦