An acclaimed international collection of earth science articles and book reviews on palaeontology, geology, minerals and more
Jon Trevelyan (UK) This is the seventh in my series of short articles on fossils of the Ordovician. Of all the Ordovician gastropods, few are as visually striking as Maclurites bigsbyi. With its large, open-coiled shell and broad, planispiral whorls, the species represents a unique experiment in molluscan shell architecture … Read More
One of the great advantages of publishing Deposits online is that an article does not disappear once the next issue comes along. Everything we publish remains available on the website, creating an ever-growing archive of articles, covering geology, palaeontology and the wider Earth sciences. However, as that archive grows, there … Read More
Jon Trevelyan (UK) A museum built on fossils Hastings is usually associated with history rather than prehistory. Its name is inseparable from 1066, while its fishing beach, old town and cliffs are familiar features of the modern resort. Yet the rocks beneath and around the town preserve evidence of a … Read More
In Part 1, we reconstructed the long-lived Devonian lakes of the Orcadian Basin from their sedimentary record. Here, we turn to a much more recent and far more fleeting landscape. At the end of the last Ice Age, ice-dammed lakes formed across parts of Britain, leaving behind traces that are often subtle – but in Glen Roy, they are spectacular. The famous ‘parallel roads’ provide one of the clearest records of changing lake levels anywhere in the country, preserving the story of a landscape shaped over centuries, rather than millions of years.
Jon Trevelyan (UK) This is the sixth in my series of short articles on fossils of the Ordovician. Trilobites reached their zenith in diversity during the Ordovician, but few species are as impressive as Isotelus maximus. Renowned for producing some of the largest articulated trilobite specimens ever found, this North … Read More
Jon Trevelyan (UK) A museum unlike any other Perched above Scarborough’s South Bay, the Rotunda Museum occupies a unique place in the history of geology (Fig. 1). Opened in 1829, it is one of the world’s earliest purpose-built geological museums and remains one of Britain’s most historically significant centres for … Read More
Stephen K. Donovan (UK) One of the first volumes that I bought when I first took up palaeontology over 50 years ago was the very excellent Directory of British Fossiliferous Localities (Arkell et al., 1954; Donovan, 2025a), a tome full of meat. It was published in the same year as … Read More
Jon Trevelyan (UK) This is the fifth in my series of short articles on fossils of the Ordovician. If one fossil trilobite has achieved near-universal recognition among collectors, it is Flexicalymene meeki. Abundant, beautifully articulated and famous for its perfectly enrolled specimens, this species offers a remarkably complete view of … Read More
Jon Trevelyan (UK) A landscape full of holes Grime’s Graves does not announce itself with the drama of a great cliff, cave or quarry. On a low Chalk ridge in the Breckland of Norfolk, the most immediately striking feature is instead the ground itself. Across the grassland are hundreds of … Read More
This is the first of a three-part series exploring Britain’s lost lakes – landscapes that once existed across very different timescales, from the Devonian world of the Orcadian Basin to the fleeting ice-dammed lakes of the last Ice Age. In this opening article, we go deep into the Devonian, reconstructing the Orcadian lakes from the evidence preserved in Caithness and Orkney. Here, finely layered sediments, exceptional fossil preservation and subtle environmental clues allow us to rebuild not just the organisms that lived there, but the structure and behaviour of the lakes themselves.
Jon Trevelyan (UK) This is the fourth in my series of short articles on fossils of the Ordovician. Among the diverse and often bizarre echinoderms that flourished during this period, Echinosphaerites aurantium is one of the most distinctive. A rhombiferan cystoid with a rounded, grapefruit-like body, it embodies the experimental … Read More
Jon Trevelyan (UK) A small museum with a remarkable geological story Tucked away behind the parish church in the centre of Cromer, Cromer Museum occupies a modest site that visitors could easily overlook. Entering through a modern reception building, the museum opens into a narrow courtyard surrounded by a terrace … Read More
Every coal seam in the West Cumberland Coalfield district records the accumulation of peat in a mature lycopsid swamp. But just as revealing as the coal itself is what lies immediately above it – the roof shales. These fine-grained sediments record the moment when the forest drowned, the swamp surface subsided or flooded, and a new ecological phase unfolded above the buried peat. In the West Cumberland Coalfield, roof shales are exceptionally well developed and preserve a full sequence of the events that followed each catastrophic rise in water level.
Jon Trevelyan (UK) This is the third in my series of short articles on fossils of the Ordovician. Although the famous Pterygotus of Silurian and Devonian fame had not yet reached their iconic size in the Ordovician, their ancestors were already present in the marine ecosystems of the period. These … Read More
Jon Trevelyan (UK) Rising above the hills near the town of Blaenavon is the distinctive headgear of Big Pit, one of the most recognisable symbols of the South Wales Coalfield (Fig. 1). Today, the site forms part of the National Coal Museum of Wales, but for nearly a century it … Read More
Deborah Painter (USA) There is a fault zone that trends southwest to northeast from Stafford County, Virginia USA and joins a fault that extends through the capital of the United States. It is a high-angle reverse fault. Cambrian and Ordovician mylonites, schists and phyllites lie unconformably atop Cretaceous gravels or … Read More
Jon Trevelyan (UK) This is the second in my series of short articles on fossils of the Ordovician. Among the many colonial organisms that chart the course of Ordovician seas, Didymograptus murchisoni remains one of the most recognisable. A key graptolite of the Middle Ordovician, it combines elegant morphology with … Read More
Jon Trevelyan (UK) The ruined furnaces of Blaenavon rise unexpectedly from the Welsh hillsides like the remains of some vast industrial fortress. Massive retaining walls, towering masonry structures and steep charging ramps still dominate the landscape, despite the silence that now surrounds them. Grass and wild flowers spread across terraces … Read More
Trevor A Jackson (Trinidad) and Stephen K Donovan (The Netherlands) The Caribbean island of Antigua lies towards the northern end of the Lesser Antilles volcanic arc. In this particular region, it is a double arc, diverging northwards. To the west, the arc is a line of islands formed by volcanoes … Read More
Jon Trevelyan (UK) This is the first in my series of short articles on fossils of the Ordovician. Among the many graptolites recovered from the classic Dob’s Linn section of the Southern Uplands, Climacograptus wilsoni is one of the most elegant. Its slim, saw-toothed profile captures a phase in graptolite … Read More
Jon Trevelyan (UK) Keswick Museum is not a geology museum in any conventional sense. There are no long stratigraphic runs of specimens, no systematic mineral displays, and no attempt to present geology as a complete discipline. Instead, visitors encounter a typically Victorian mixture of natural history, literature, local industry and … Read More
Jack Shimon (USA) I recently went to the Denver Museum of Nature and Science. This was my first member’s night and I want to go to them every time now.My mom and I went to see Dr Scott Sampson talk about a dinosaur. He is the new chief curator and … Read More
Jon Trevelyan (UK) This is the twentieth and last in my series of short articles on fossils of the Cambrian. Yunnanozoon lividum, from the Early Cambrian Chengjiang biota of southwest China of about 518 million years old, is one of the most intriguing fossils in the long search for the … Read More
Jon Trevelyan (UK) Beneath Dudley Castle lies a landscape that began as a tropical Silurian sea and ended as one of the most intensively worked limestone systems in Britain. Around 425 million years ago, this part of the Midlands lay beneath a warm, shallow sea, building the reef limestone now … Read More
The trunks of Lepidodendron and Sigillaria (Part 2) dominate most people’s mental image of the Carboniferous swamp, but to understand how these forests actually functioned, you need to look beneath the surface, into the layer that supported and anchored the entire ecosystem. In the West Cumberland Coalfield, this means one thing above all – Stigmaria, the distinctive rooting systems of the giant lycopsid trees.
Jon Trevelyan (UK) This is the nineteenth in my series of short articles on fossils of the Cambrian. Wiwaxia corrugata is one of the most distinctive animals of the Middle Cambrian Burgess Shale – a soft-bodied creature decked in shimmering scales and sharp defensive spines, crawling slowly across the seafloor … Read More
Jon Trevelyan (UK) The road over Honister Pass does not feel like a place for industry. It climbs abruptly into the high fells, threading between steep slopes and exposed rock faces, with little sense of the gentler, pastoral Lake District often presented in guidebooks. Yet, set into this harsh landscape … Read More
Peter Perkins (UK) While an undergraduate, I had the opportunity to be involved in a student exchange with IAESTE (International Association for the Exchange of Students for Technical Experience) during the summer of 1959. Although not specialising in mineralogy, I was assigned to the mine at Stari Trg with three … Read More
Jon Trevelyan (UK) This is the eighteenth in my series of short articles on fossils of the Cambrian. Waptia fieldensis is one of the most beautifully preserved and behaviourally informative animals from the middle Cambrian Burgess Shale. Living around 508 million years ago, it represents an early and unexpectedly sophisticated … Read More
With the restoration of the Crystal Palace prehistoric sculptures and their remarkable Geological Court now virtually complete, it is perhaps worth asking why this unique Victorian landscape continues to command such scientific and historical importance. Why should geologists, palaeontologists and members of the public still make the journey to south London to see reconstructions that are now more than 170 years old and, in many respects, scientifically outdated?
