GEOLOGICAL WALKS, BUDE, CORNWALL
(For Blockley Cotswold Geo-Walks, click here)

Geological walks on the beach & cliff path, guided by Dr Roger Higgs (Oxford doctorate on Bude Formation rocks, 1982-86).
Enjoy the fascinating geology exposed in the cliffs along this glorious sector of the legendary South West Coastal Path (see photos below). Alternating beds of sand ('turbidites') and mud, together totalling about 1.3 km in thickness, make up the 'Bude Formation'. These beds were deposited in a giant 'Lake Bude' 300 million years ago (long before dinosaurs existed), when the UK lay far to the south near the equator (see 'continental drift' in Wikipedia). Meanwhile, strata containing peat (now coal, hence the 'Carboniferous' name of this geological period) accumulated in shifting tropical-forest delta swamps that intermittently covered much of Wales, England and Scotland. Among the few fossils found in the Bude Formation, the extinct fish Cornuboniscus budensis (photo below) is unknown anywhere else in the world. Lake Bude was the last vestige of a former 'Rheic Ocean' that was gradually consumed (by 'subduction') as the 'Gondwana' supercontinent, with France on its leading edge, converged with the 'Euramerica' supercontinent, with the UK on its trailing edge. These 'plate tectonic' movements eventually led to supercontinent collision (producing the 'Pangaea' megacontinent), causing mountain building ('orogeny') at the collision site, folding and uplifting the Bude strata just a few million years after deposition. The resulting 'Variscan' mountain range trended along the length of Cornwall and continued eastward into present-day Europe and westward into the USA (the Atlantic did not then exist). Deep inside the new mountains, compression squeezed the Lake Bude beds into spectacular zigzag folds (photos below). This same 'Variscan Orogeny' is responsible for the Cornish and Dartmoor granites and the related mineral veins, both of which formed deep (km) underground. The granites are now exposed, like the Bude beds, thanks to uplift and erosion of many kilometres of vanished overlying rock.
Many oil company geologists, geophysicists and engineers visit here, using the Bude Formation as an 'outcrop analogue', to gain insights into the likely internal architecture (bed stacking) of 'turbidite' sandstone oil reservoirs deep underground (therefore hard to visualise) onshore and offshore around the world, in order to assist with the selection of future borehole locations, thereby aiming to minimise expense (fewer 'dry holes') and maximise oil production. Bude is also popular with Earth Science departments of universities and colleges, for training students in 'structural geology' (folds, faults, etc.) and 'sedimentology' (genesis and composition of sedimentary rocks).
As a sedimentary geologist ('sedimentologist'), with decades of experience in the oil industry, Roger is well qualified to answer your questions on fracking, global warming and sea-level rise.
Bude Geo-Walks can be arranged at any time of year for 1-25 people (dogs & infants allowed), timed to suit you. Walks last for three hours and cost £150 for up to 6 people (adults or children), plus £20 for each additional person. A very popular itinerary is the 'round-trip' from Bude to Northcott Mouth (1 mile each way), walking north along the beach (barefoot if you like!), discussing the marvellous folded beds in the cliffs; and returning south along the clifftop South West Coast Path, with stunning views up and down the coast. Adding a fourth hour (extra £50) allows us to extend this walk to Sandy Mouth (2 miles each way). There are seasonal cafeterias at both Northcott Mouth and Sandy Mouth. Alternative localities are Millook Haven (see 6th photo below!) and Widemouth Bay. Please note that Roger now lives in the Cotswolds, so your Bude Geo-Walk needs to be planned at least a few days ahead. To arrange your desired time and itinerary, please email rogerhiggs@hotmail.com
Tailored walks for clubs, societies, schools, colleges & universities by arrangement. Commentary in fluent Spanish if required. Please email rogerhiggs@hotmail.com
For reviews of Bude Geo-Walks and information on Bude's geology, please see:-
...TripAdvisor Reviews Weblink
...Geological publication 1 (download pdf 2.0 MB)
...Geological publication 2 (download pdf 6.1 MB)
'Bude Geo-Talks' are 1-hour lectures for schools, colleges, universities & other interested groups. Four talks are currently offered (others can be prepared on request), in English or Spanish:
1. "The Bude Formation: 300-million-year-old sand & mud beds deposited in a giant tropical lake inhabited by a unique fish"
2. "Geological evolution of Cornwall: pre-dinosaur mountains formed by collision of England & France"
3. "Global warming and sea-level rise: unstoppable?"
4. "Fracking explained by a petroleum geologist"
Lectures can be given at your premises (anywhere in the world), or virtually, or at one of several hireable venues in Bude. For prices & details, please email rogerhiggs@hotmail.com
Cliffs and wave-cut platform at low tide, looking north toward Bude. Photo copyright Roger Higgs.
Maer High Cliff, near Bude, beautifully exposing steeply dipping sandstone & darker mudstone (shale) beds of the Carboniferous-age Bude Formation, about 300 million years old. Note syncline (downfold) at right-hand side. For scale, note two people on cliff edge at centre. Photo copyright Roger Higgs.
Cliffs and wave-cut platform, looking south toward Bude. Note seaward-plunging zigzag folds at centre-right, seen in plan view. Photo copyright Roger Higgs.
Syncline (downfold) in the Bude Formation, Pearces Cove. For scale, note man and child standing on cliff edge, top right. Photo copyright Roger Higgs.
Anticline (upfold) in the Bude Formation, Upton. Photo copyright Roger Higgs.
Crackington Formation (slightly older than the Bude Formation) at Millook Haven. For scale, note group of people (red jacket) on beach, near cliff base, below magnificent cascade of zigzag folds. Photo copyright Roger Higgs.
Cornuboniscus budensis, an extinct fossil fish about 300 million years old (much older than the oldest dinosaur), globally unknown outside the Bude Formation, on display in the museum at Bude Castle Heritage Centre, on loan from the Natural History Museum (NHM) in London. This specimen (mirror-image impressions inside a split nodule) is only about 6 cm long. Note that the specimen tapers from the head (at right/top) toward the tail, and is kinked at about 3/4 of the way along. For a downloadable close-up photo (scale in mm), from the NHM website, go to Weblink
Two kinds of "trace fossil" made by fish swimming in contact with the muddy bottom of "Lake Bude". Type 1 consists of paired sinuous grooves made by a fish's tail fin and belly fin. Type 2 is a nearly straight, shallow trough (made by fish's breast) with superimposed zig-zag "flick marks" made by the tail (two examples visible). Were these fish hunting? Photo copyright Roger Higgs.
Dr Roger Higgs and HRH Prince Charles (King Charles III since 2022) at Bude Castle Heritage Centre, 15th July 2013, discussing Bude's geology and its unique fossil fish, Cornuboniscus budensis.
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