EGS Lecture Programme
Our varied programme of illustrated lectures runs from October to Easter, on Wednesday evenings. These meetings are open to the public, there is no charge, and visitors are most welcome.
Speakers and topics are carefully chosen to provide interest for both the amateur and professional geologist. These meetings also provide an informal opportunity to chat to other members, and find out more about geological sites from local experts. At the annual Fellows’ Night, members give accounts of their own geological interests, specimens or travels.
We will continue to broadcast our lectures online via Zoom and also, if speakers agree, record them for later viewing on our YouTube channel. If you are not a member, please contact Angus Miller (promotion@edinburghgeolsoc.org) for details.
Information about the lectures, including more detailed abstracts where provided, are available below.
This is my first term as Lectures Secretary, and I’m keen to receive your feedback and ideas for the future!
Alastair Milne, Lectures Secretary – email lectures@edinburghgeolsoc.org.
The lectures usually take place in the Hutton Lecture Theatre in the Grant Institute of Geology, The King’s Buildings, James Hutton Road, Edinburgh EH9 3FE.
The Grant Institute is part of the School of Geosciences (it is labelled The Grant Institute on the door). It is one of the large buildings just back from, and facing West Mains Road.
Coming by bus: Lothian service 9 travels along West Mains Road and enters Gate 1 to Kings Buildings to its final stop on David Brewster Road. Head east on David Brewster Road (in the direction the bus is facing), cross over the junction with a large red brick building on the right (School of Chemistry) and a statue of David Brewster on the left. Continue straight ahead at the next junction onto James Hutton Road. Beside this is a large blue information board which includes directions to the Grant Institute. Continue a few metres along James Hutton Road to the first large building on your right, labelled School of Geosciences, Grant Institute.
Coming by car or bike: From West Mains Road turn into Gate 2 of King’s Buildings (the entrance closest to Mayfield Road) onto James Dewar Road. At the first junction, turn left onto James Hutton Road. There is a large blue sign which includes directions to the Grant Institute. Continue a few metres along James Hutton Road to the first large building on your right, labelled School of Geosciences, Grant Institute. Parking is available in front of the building.
Once inside the Grant Institute, turn left and follow the corridor round to the end where you will find the James Hutton Lecture Theatre at the bottom of a short flights of steps (a stair lift is available).
What3Words link for the front door: what3words.com/spends.claims.slate
EGS Evening Lecture Programme 2025-26
Monday 6 October 2025, 7pm: Public event: Introducing James Hutton
Introducing James Hutton – public event
Monday 6 October 2025, 7:00 to 9:00pm
Dynamic Earth, Edinburgh
Join us at this public event to launch the James Hutton Tercentenary celebrations. James Hutton (1726-1797) is widely acknowledged as the Father of modern geology, a self-taught Edinburgh philosopher who made significant contributions to the understanding of Earth processes and agriculture. As we approach 2026, the “Tercentenary Campaign Group” of organisations and individuals are working together to reintroduce James Hutton to Scotland and the wider world, learning more and sharing an appreciation of his legacy.
Wednesday 15 October, 7pm Prof John Underhill, University of Aberdeen
Wednesday 15 October, 7pm
Prof John Underhill, University of Aberdeen
Geoscience’s Critical Role in the Energy Transition
Over the past Century, the global population has increased fourfold from just 2 Billion in 1928 to over 8.1 Billion today. It is projected to rise yet further to exceed 11 Billion by 2100. Growth of his magnitude places enormous pressure on Earth Systems and its resources as people seek to improve their quality of life, but with negative consequences on biodiversity, the environment and climate. Over the same period, the levels of atmospheric carbon dioxide have risen from 300ppm to over 420ppm and carbon dioxide emissions have gone from 4 to 35 Gigatons per year, with all the consequences for global warming and sea level rise that has. In this context, it is an inconvenient reality that fossil fuels currently account for over 80% of primary energy consumption and even countries that have weaned themselves off coal, still rely heavily on oil and gas to power industry, keep the lights on, heat homes and to meet their transportation needs (e.g. 75% dependency in the UK). Given the stark figures, the starting point on our road to decarbonise society and meet net zero emissions targets is an extremely challenged one, and a misstep along the way could impose blackouts, power outages, impose fuel poverty and job losses.
In light of recent global events, there has been an increasing appreciation and focus on trying balance the energy trilemma that ensures security of supply, affordability, and environmental sustainability & climate compatibility to ensure that there is a smooth, orderly, managed transition rather than a cliff edge, with a highly variable degree of success. While some are intent on shutting down industrial clusters, doing so will come at a cost to jobs, communities, national economics (GDP), energy security and, given the demand for the products is unlikely to diminish, the (higher) carbon footprint will simply be exported. We are in danger of not learning the lessons of past mistakes which afflicted coal mining, ship-building, and the steel-making sectors to name but a few, meaning a “fair and just transition” will not be achieved. There is also an urgent imperative to gain a social license to operate from affected communities as places get rewired for the transition (e.g. offshore wind connections to the grid replace those from the old industrial heartlands).
Geoscience has a huge role to play as we wrestle with the massive challenge to transition our energy systems and seek viable solutions to enable the pivot from fossil fuels to renewable sources. There is a need to have forensic data-led, evidence-based research undertaken to characterise the subsurface, seabed, and metocean conditions exist that enable industry to decarbonise and emissions targets to be met. Integration of core descriptions with wireline log analysis, seismic data and field analogues will help determine where the best sites are for carbon dioxide, hydrogen, and nuclear waste storage, (low- and high-enthalpy) geothermal energy sources, wind farms and placer deposits containing critical minerals. Despite the evident need for the expertise to communicate with communities and technically inform policy and decision-making, the career pathway is proving to be less attractive and there are serious recruitment challenges to be addressed. It is imperative that we articulate the message that our subject and its practitioners are crucial if we are going to meet the challenges embodied in the energy trilemma. As society seeks the solutions to save the planet yet continue to meet the energy needs of an increasing world population and geoscientists will be at the forefront of that.
Biography
John is the Interdisciplinary Director for Energy Transition and Professor in Geoscience and Energy Transition in the School of Geosciences at the University of Aberdeen, a post he took up in March 2022. He is the academic director of the UK’s GeoNetZero Centre of Doctoral Training (CDT), a £22M partnership consisting of 12 Universities and 8 company sponsors that has seen 128 PhDs graduate, all of whom have secured employment in a relevant discipline. His research interests focus upon the role of geoscience in the energy transition and use of technologies, methods and data in providing the best solutions and outcomes to deliver low-carbon net zero goals. John is the Chair of the National Energy Skills Accelerator (NESA), a collaboration between Aberdeen University, RGU, North-East Scotland College, Skills Development Scotland, and Energy Transition Zone (ETZ) Ltd., which secured a £1M award from the Scottish Government’s Just Transition Fund to up-skill and re-skill workers for a career in renewable energy. Before taking up an academic career, John worked in industry and has also undertaken two industrial fellowships when at The University of Edinburgh. Prior to joining Aberdeen John co- lead Heriot-Watt University’s efforts to establish the Lyell Centre for Earth and Marine Science and Technology and was their Chief Scientist. John is a member of the UK Energy Minister’s Subsurface Task Force and also populated the Scottish Science Advisory Council (SSAC), the leading independent advisory board for Scottish Government between 2018-22. John was President of the European Association of Geoscientists and Engineers (EAGE) in 2011-12, an EAGE Board Member for 3 years and was awarded their Alfred Wegener Prize in 2016. He also has received the Lyell Medal from the Geological Society, the Silver Medal from their Energy Group, and the Clough Medal from the Edinburgh Geological Society for 2012-13. An unusual fact is that John was an international soccer referee, who officiated in international (FIFA and UEFA) football and the Scottish Premier League between 1994-2008.
This lecture will be preceded by an informal ‘pizza and pop’ session, from 6pm in the Grant Museum. All welcome: please book.
Wednesday 29 October, 7pm Prof Malcolm Hole, University of Aberdeen
Wednesday 29 October, 7pm
Prof Malcolm Hole, University of Aberdeen
A Brief Guide to the Geology of the Moon
It is more than 55 years since the Apollo 11 mission provided the first sample returns from the Moon. The Apollo samples were subjected to a plethora of investigations and analysis in the two decades from 1970 onwards. Developments in chemical analytical techniques in the 21st century has allowed far more detailed analysis of much smaller samples than was possible in the 1970s. Moon rocks therefore continue to give up their secrets. Advances in satellite remote sensing has also allowed detailed mapping of the entire Lunar surface, with high-resolution geochemical and mineralogical maps being available to all. Nasa’s Artemis missions, the first crewed flight being scheduled for 2026, has reinvigorated research into Lunar geology.
The Moon was born during the impact between Theia and proto-Earth 4.55 billion years ago. Unlike Earth, the Moon is not tectonically active, and it is likely that geological activity on the Lunar surface stopped around 3.4 billion years ago. The geology of the farside and nearside of the Moon are quite different (the ‘Lunar Dichotomy’) with the farside dominated by old (4.55 Gy) anorthosite crust and the nearside dominated by 3.8-3.4 Gy flood basalts known as the Lunar Maria. Lunar Maria basalts are astonishingly fresh in thin section and preserve pristine olivine, pyroxenes and ilmenite phenocrysts and often display a vitrophyric texture.
The talk will cover some of the historical aspects of the Apollo missions and illustrate how the Department of Planetary Science at Aberdeen is utilizing modern petrological and remote sensing data to examine the origin and petrogenesis of lunar Maria flood basalts.
Wednesday 12 November, 7pm Norman Moles, University of Brighton
Wednesday 12 November, 7pm
Norman Moles, Honorary School Fellow, School of Applied Sciences, University of Brighton
The Trainor’s Rocks gritstone–conglomerate, Mourne Mountains, Northern Ireland: a volcanic arc-derived channel–fan deposit in the closing Iapetus Ocean
In the western Mourne Mountains of County Down, a hitherto unrecorded pebbly gritstone–microconglomerate formation outcrops in an area 0.4 by 1.1 km adjoining the Palaeocene Mournes G4 Granite. The unit lies within otherwise fine-grained Hawick Group (Wenlock) strata. The occurrence is regionally significant because this is one of the youngest (~430 Ma) coarse clastic units within the Ordovician-Silurian Southern Uplands – Down-Longford Terrane, and is rich in extraformational clasts including granite, rhyolite, andesite, basalt, vein quartz and metamorphic rocks, plus intraformational rip-up clasts of mudstone. Detrital zircons extracted from samples of the highly indurated conglomerate yield predominantly Ordovician U-Pb ages of 450-490 Ma, peaking at ~470 Ma, coincident with arc-related magmatism in the Midland Valley Terrane. Whole rock geochemical data are consistent with derivation from a calc-alkaline continental arc, with clast provenance matching 473-464 Ma arc volcanic and intrusive rocks from the Tyrone Igneous Complex located >100 km to the north. It seems likely that the gritstone–conglomerate was deposited as a submarine channel fan deposit during the final stages of closing of the Iapetus Ocean, while the northwestern hinterland underwent episodic tectonic unroofing in response to strike-slip movements. More speculatively, the gritstone–conglomerate might be the source rock for alluvial gold occurring in modern sediments of the nearby Leitrim River.

Wednesday 26 November, 7pm School of GeoSciences early career researchers
School of GeoSciences early career researchers
Three early career researchers from the School of GeoSciences, University of Edinburgh will share their research in a series of short talks.
Edwin Rodriguez Dzul
Non-marine early eukaryotes: new insights from the microfossil diversity of the ca. 1 Ga Torridon Group
This study examines exceptionally preserved organic-walled microfossils from phosphorites within the Diabaig Formation (Torridon Group, NW Scotland) that contributes to our understanding of early eukaryotic organisms during the Mesoproterozoic-Neoproterozoic.
Beau Jones
Assessing Palaeoecology across the K-Pg of Antarctica with Quantitative Sampling and Biomarker Analysis
Seymour Island, Antarctica (65°S), contains the most complete sedimentary record of the Cretaceous-Palaeogene (K-Pg, ~66 Ma) boundary at high latitudes, abundant with well-preserved marine invertebrate macrofossils. Here, we present preliminary results of our systematic sampling across the K-Pg boundary on Seymour Island, soon to provide the highest resolution account of the marine ecosystem during this period and from this region.
Steve Hollis
Chlorite and white mica as halos in metamorphosed VMS deposits: insights from the Archean King Zn deposit, Yilgarn Craton, Western Australia
Most ancient volcanogenic massive sulphide (VMS) deposits have been subjected to metamorphism particularly those Archean in age. Despite countless advances in recent years, exploration remains challenging. This is particularly the case in the Yilgarn Craton of Western Australia, where there is a paucity of outcrop, and weathering is deep and extensive. Recent significant breakthroughs in the accessibility of low-cost hyperspectral data to industry offer a great opportunity as a VMS exploration tool in geologically complex terranes. Here we present results of a detailed mineralogical and hyperspectral study of the King Zn deposit. We demonstrate that integrated mineral chemistry and hyperspectral datasets provide rapid and cost-effective tools for the detection of hidden orebodies.
This lecture will be preceded by an informal ‘pizza and pop’ session, from 6pm in the Grant Museum. All welcome: please book.
Wednesday 10 December, 6.30pm Fellows’ Night
This meeting, close to the anniversary of the foundation of the Society, is a chance to meet other members informally, with refreshments served from 6.30pm, followed by a series of short talks given by members.
Tickets cost £5 per person: please book in advance – webcollect.org.uk/edinburghgeolsoc/event/egs-fellows-night-2025
Please note that Fellows’ Night is live, in-person only. There will be no Zoom broadcast or recording.
Prof Mark Wilkinson (School of GeoSciences, Edinburgh University)
Why James Hutton is not called the ‘Father of Modern Diagenesis’
Hutton’s Theory of the Earth revolutionised our understanding of geological time and described the rock cycle. A vital part of the latter was the consolidation of sediments (sand, mud) into solid rock. Hutton considered two consolidation mechanisms: aqueous reactions and fusion, i.e. the softening and melting of the rocks by heat. Hutton argued that aqueous reactions are unimportant, and that heat is the sole driver of consolidation. Modern thinking considers this to be entirely wrong, with the role of heat relegated to a control on the rate of aqueous chemical reactions. Heat, in the sense that Hutton imagined, is confined to the igneous and metamorphic realms.
Carina Hoorn (Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, The Netherlands)
When the Amazon flooded
The Amazon is among the most species-rich places in the world, with 10% of all plant and vertebrate species concentrated in 0.5% of the Earth surface. How did the Amazon become so biodiverse and what can past records tell us about the history of the Amazon? One intriguing feature in the sedimentary record are the marine incursions that reached deep into the Amazon until about 12 million years ago. Fossil remains of flora and fauna illustrate a rich past diversity. It has even been suggested that the marine incursions are partly responsible for the current plant geography in the region. In this presentation I will explore some of these topics and take you on a journey into Amazonia’s past.
Steve Garrett (Earth Scientist, Musician, Author)
Exploring Scottish Geology in Creativity
Steve Garrett summarises some recent examples as part of a blossoming of creative works inspired by our Earth. This includes: diverse art work by the Moine Thrust at Knockan Crag in Assynt; Skye-based Julie Brook’s land art in Fife and on Harris; Dundee-based Callum Wallis’s response to the Angus coast and Great Glen Fault; Fife-based Katie Paterson’s sampling of geological materials from deep time showcased at Edinburgh’s Ingleby Gallery; NE Scotland’s Olivia Rafferty’s pop songs inspired by geology; Borders-based Matilda Brown’s music responding to the ground beneath her feet on long distance walks; and diverse poetry, song, ambient music and film inspired by Siccar Point from East Lothian’s Michael Begg and Karine Polwart, Edinburgh’s Patrick Corbett, and others.
Wednesday 14 January 2026, 7pm Cendi Dana, University of Edinburgh
Wednesday 14 January, 7pm
Cendi Dana, University of Edinburgh
Exploring a Metamorphosed VMS System in Scotland: Lessons from the Kerry Road Cu-Zn-Au Deposit
Volcanogenic massive sulphide (VMS) deposits are well-studied mineral systems capable of hosting significant base- and precious-metal resources. In unmetamorphosed terranes, their hydrothermal alteration zones are relatively simple, with well-defined mineralogical, geochemical, and isotopic halos that guide exploration. However, in high-grade metamorphic settings, these signatures are often obscured: alteration assemblages are overprinted, footwall sequences become mineralogically complex, and ore lenses are deformed, recrystallized, or remobilized. Consequently, only ~11% of known VMS deposits occur in amphibolite-facies rocks, and just 0.5% in granulite-facies settings—suggesting major untapped potential if robust exploration tools can be developed. This presentation integrates bulk geochemical, mineral chemical, and geophysical data from the Kerry Road deposit to investigate ore-forming processes and identify vectors to mineralization in metamorphic terranes. Several mineral chemical indicators show strong potential for distinguishing mineralized from barren systems, opening new possibilities for effective targeting in these challenging yet promising geological environments.

Figure: Representative outcrops around the Kerry Road VMS deposit, Gairloch, NW Scotland
Wednesday 21 January 7pm, Expressing the Earth film screening
Wednesday 21 January 7pm
Expressing the Earth film screening
Please note that the film showing will be live, in-person only. There will be no Zoom broadcast or recording.
This special event for EGS members and friends brings the Expressing the Earth documentary film to Edinburgh for the first time. It explores geopoetics as the creative expression of the Earth in stunning locations on the west and east coasts of Scotland. In doing so its beautiful cinematography also reveals the captivating poetry of the Scottish writer and thinker Kenneth White who spent a childhood at Fairlie on the Ayrshire coast – a shoreline of Devonian Old Red Sandstone cut by Palaeogene dykes. Influenced by his Fairlie geological grounding and a life spent in the remote and natural landscapes of the Scottish Highlands, the Pyrenees and France, Kenneth White coined the term ‘geopoetics’. This interdisciplinary approach combines oral expression, writing, the visual arts, music, geology, geography, science and philosophy to explore the relationship between places, landscapes and human experience.
Producer Norman Bissell says, “I believe that it will inspire those who watch it to a greater understanding of geopoetics which offers society as a whole a better way of living on the planet.”
The film was crowdfunded by the Scottish Centre for Geopoetics based on the Isle of Luing in Argyll and was sponsored by RSK environmental consultancy, the Curry Fund of the Geologists’ Association and the Edinburgh Geological Society. It was awarded Best Documentary Feature at the New Renaissance Film Festival in London, and Best Director for Glenda Rome at the Stratford upon Avon Film Festival.
“The first time I encountered the work of Scottish poet and thinker Kenneth White, I felt as though someone had found words for what I had always sensed in wild places — that profound stillness where the mind and the land seem to speak the same language.
Expressing the Earth is, for me, an act of listening — to landscape, to poetry, to the spaces in between. It’s about finding new ways of seeing and expressing our connection to the living world, at a time when that connection feels more fragile than ever. I hope the film invites reflection, and perhaps a quiet remembering — that to truly express the Earth, we must first learn to listen to it.” Glenda Rome, Director
“I have just finished watching the film. It is incredible, I really enjoyed it. The film offered the viewer so much, the atmosphere created by the shots and music, the inclusion of multiple artists, the educational pieces about geology, poetry and art. All deeply inspiring. It kept me engaged and was very stimulating to watch. Well done, a fantastic job.” Fiona Sturrock (Presenter, Words To Inspire Poetry, Purbeck Sounds)

Wednesday 28 January, 7pm Prof Jane Evans, BGS
Wednesday 28 January, 7pm
Prof Jane Evans, BGS
The geographic origins of the builders of Stonehenge
This talk explains how the matching of tooth enamel composition to aspects of British geology has enabled us to track the origins of the workers who built Stonehenge and provide insights into the diversity of origins of those buried nearby.
Wednesday 11 February, 7pm MIS/EGS Joint lecture Chris MacKenzie
Wednesday 11 February, 7pm
MIS/EGS Joint lecture Chris MacKenzie
Please note that this lecture will be live, in-person only. There will be no Zoom broadcast or recording.
Exploration for Critical Metal Mines in Scotland
Mineral exploration and mine discovery & development is a long, complex process dependent on many variables – technical, economic, political and social. Many of these have recently changed, causing increased demand for “critical metals” used in modern technological equipment, electrification etc..
Mines are long-life industrial developments taking many years, and lots of money, to explore and commission. A single mine complex can create many thousands of direct and indirect jobs with a long-term influence on a country’s progress. Fluctuation in commodity prices and other socio-economic issues may hinder mine development or put mines out of business. Technological advances and increased demand for certain metals generally speeds things up, and may make sub-economic projects viable.
At present, the vast majority of the UK’s critical metals needs are met from overseas sources, normally from countries with lax environmental controls which use cheap power (i.e. coal). Whilst the UK turned its back on coal, recent developments in UK mining, such as the re-opening of South Crofty tin mines may give some pointers to the future.
The talk will discuss critical metals and their exploration, focussing in on the Ordovician basic magmatic rocks of NE Scotland for nickel-copper-cobalt “battery metals”. These rocks were explored by some major mining companies in the “nickel boom” of the 1960s and 1970s but have received scant attention since then. Following modern exploration efforts over the last few years it is clear that, despite the various economic and other hurdles, NE Scotland could supply responsibly-sourced and low environmental impact battery metals.
Chris MacKenzie is an economic geologist who has spent the last 35+ years working globally. In 1988 he graduated in Geology from Portsmouth Polytechnic. His early career focussed on Ni-Cu-Co-PGE mining and exploration on the major mines in Botswana, before stints of aid work in the Middle East & Africa then back to geology in South America. He gained his M.Sc. in Exploration Geology at Rhodes University, South Africa in 2001. He has been involved in forming and running junior exploration companies working throughout the world, but mainly in Africa, resulting in the discovery of a number of mines and resources. He is currently actively exploring for critical metals much closer to home…
Wednesday 25 February, 7pm Prof Katriona Edlmann, University of Edinburgh
Wednesday 25 February, 7pm
Prof Katriona Edlmann, University of Edinburgh
Clough Medal Lecture: The Role of Scotland’s Geology in the Energy Transition
To meet Scotland’s commitment to net-zero carbon emissions by 2045, our energy system must transition away from fossil fuels towards secure, affordable, low-carbon alternatives. Achieving this will require large-scale deployment of carbon capture and storage (CCS), hydrogen production and storage, and low-carbon heat systems. Scotland’s diverse geology offers an exceptional foundation for these technologies, including saline aquifers for CO₂ storage; granites and salt deposits for hydrogen storage in lined or solution-mined caverns; depleted gas fields for hydrogen and CO₂ storage; offshore salt caverns for compressed air energy storage (CAES); and legacy mine workings and deep aquifers for geothermal heat. Scotland also hosts many of the geological conditions that may generate natural hydrogen, including serpentinisation of ultramafic rocks, radiolysis of water near granites, and decomposition of organic material. This talk will examine the scale of the decarbonisation challenge and explore how Scotland’s geology can support multiple energy technologies to deliver a secure and decarbonised energy system.
Katriona Edlmann is Professor of Sustainable Energy at The University of Edinburgh, with over 25 years researching the secure and sustainable utilisation of the subsurface for low-carbon energy applications including hydrogen energy and CO2 storage. Katriona is responsible for several UKRI, EU and industry funded projects investigating underground hydrogen storage technologies. Katriona is a member of the UK Government Department for Energy Security and Net Zero Hydrogen Advisory Council Transportation and Storage Infrastructure Working Group and is sub-task lead on the International Energy Agency Technology Collaboration Programme task 42: Underground Hydrogen Storage and contributor to Task 49: Natural Hydrogen.
Wednesday 11 March, 7pm Romesh Palamakumbura, BGS
Wednesday 11 March, 7pm
Romesh Palamakumbura, BGS
Geological characterisation of the Great Glen Fault to support the development of new pumped storage hydropower projects
Pumped storage hydropower projects are of vital importance to the reliable decarbonisation of the future electricity provision in the UK. These typically involve construction of tunnels and underground cavern and hence, geological factors can play a significant role in their design and construction. The British Geological Survey (BGS) has provided impartial geological expertise and knowledge during the ground investigations of several major hydropower projects with clients across the UK. This involves providing an in-depth understanding of geological features from micro-scale processes to larger-scale regional geological controls. A robust understanding of the site-scale geology supports a more in-depth and accurate geotechnical characterisation of the rock mass including features that may impact rock strength, such as fault and fracture networks or hydrothermal alteration processes. Working in close collaboration with engineering geology consultants, such as to provide a better understanding of the site-scale geology can support a more focussed ground investigation phase and most importantly will further derisk future proposed pumped storage hydropower projects.
Wednesday 18 March, 7pm Edinburgh film premiere: As Old As The Hills
Join us for the Edinburgh premiere screening of the film As Old As The Hills – made for the Orkney Science Festival. The film is timely – the celebrations of the 300th anniversary of the birth of James Hutton, the father of modern geology, start in June.
Slovenian filmmaker, Selena S. Kuzman, takes us on an epic scenic journey through Caithness and Orkney, with magnificent drone footage. Along the way, presenters Mara Gibb and Katy Firth use quirky timelines and models to help the viewer to grasp the immensity of Deep Time. As Old As has been described as the ultimate slow movie.
Edinburgh geomorphologist, Adrian Hall, wrote the script. We find that rock hills have half-lives of tens or even hundreds of millions of years. But soft hills, like sand dunes and glacial drumlins, appear and disappear over thousands of years. Watch out for the final Da Vinci code twist supplied by renowned Orkney storyteller, Tom Muir.
Selena Kuzman and Adrian Hall will be available after the showing for a Q&A session about the making of the film.
VENUE: Lecture Theatre G01 – Lister Learning and Teaching Centre, 5 Roxburgh Place, Edinburgh, EH8 9SU
Wednesday 25 March, AGM 7pm, Lecture 7.30pm Beverly Bergman, EGS
Wednesday 25 March, AGM 7pm, Lecture 7.30pm
Beverly Bergman, EGS
James Hutton: the man, his family and the mythology
Well-known as the “father of modern geology”, James Hutton has been a somewhat enigmatic character as few of his personal papers survived. Recent research using newly discovered material has enabled us to examine some of the mythology surrounding him and provide a better understanding of the man and his family.
EGS Recorded Lectures 2025-26
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EGS Recorded Lectures 2022-23
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EGS Recorded Lectures 2021-22
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