Ask a Geologist - Under Dippy!
2026-05-30 10:00 - 16:00 (Europe/London)
To celebrate GeoWeek 2026, the Warwickshire Geological Conservation Group (WGCG) is hosting a special “Ask a Geologist” session. Join us right beneath the tail of Dippy the Diplodocus at the Herbert Art Gallery & Museum in Coventry. WGCG geological experts will be at hand to discuss geology in our everyday lives, geological careers, and geological science in general. Come along and examine specimens in super detail with our blue tooth microscope. We will have a number of rocks, minerals and fossils on hand to be viewed and discussed, a number of posters, geological references and free brochures of nearby geology trails.

This is a drop in event, no need to book ahead.

To view the event flyer please click here

Venue:Herbert Art Gallery & Museumhttps://maps.app.goo.gl/3w57Gv8vonQH8sxT9

WGCG: Ask a Geologist
2026-06-06 10:30 - 13:30, 2026-09-05 10:30 - 13:30, 2026-12-05 10:30 - 13:30 | Market Hall Museum, Market Hall Museum, Market Pl, Warwick,, CV34 4SA, United Kingdom
The WGCG shall be holding a special Ask a Geologist session at Market Hall Museum in Warwick. WGCG geological experts will be at hand to discuss geology in our everyday lives, geological careers, and geological science in general. Come along and examine specimens in super detail with our blue tooth microscope. We will have a number of rocks, minerals and fossils on hand to be viewed and discussed, a number of posters, geological references and free brochures of nearby geology trails.

This is a drop in event, no need to book ahead.

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WGCG Field Trip to South Shropshire - Led by Dr Martin
2026-06-12 15:00 - 2026-06-14 14:00
This field trip follows on from the WGCG weekend field trip led by Martin Whiteley to the north part of Shropshire in June 2025, when we looked at Precambrian to Silurian rocks. It is not needful for you to have attended last year’s trip in order to come on this trip, which will visit late Silurian to Triassic rocks between Ludlow and Bridgnorth.

Furthermore, WGCG will extend its lecture season to May this year, so that Martin can give a talk on the geology of Shropshire. This will be presented on Zoom at 7.30pm on Thursday 14th May and will be open to all WGCG members and friends. It will cover the geology of both the 2025 and 2026 field trips and therefore also serve as the introductory talk for the 2026 outing.

Image: Shropshire Geological Society https://shropshiregeology.org.uk/

DurationFormal leadership will commence at 3pm on Friday afternoon with a building stones walk around Ludlow. Activities will draw to a close mid-afternoon Sunday to allow good time for homeward travel.

Accommodation Participants are asked to book their own accommodation for this trip. Ludlow is the obvious and most convenient base for the Friday and Saturday nights, although anywhere in the Ludlow – Kidderminster – Bridgnorth triangle would also suffice. Martin Whiteley, the group leader, will be based in Ludlow.

Meals Participants should arrange their own meals, including a packed lunch for each day, except for Saturday evening. A group dinner on the Saturday evening will be organised, but no venue has yet been selected, although it is likely to be in or near to Ludlow. Participants will pay for this on the day. It is possible that the group could also informally eat together on the Friday evening in Ludlow, after a building stones walk in the afternoon.

Travel Arrangements Travel to and from Shropshire is members’ own responsibility, but if you want to lift share on this journey, please indicate that on the registration form and we will see if we can match you up with other participants for travel. The form seeks your permission to share your contact details with the other trip participants so that lift sharing, and possibly the sharing of accommodation, can be discussed easily. Travel to the start point on the Saturday and Sunday is members’ own responsibility, but on each day car sharing will be encouraged to simplify travel and because of limited parking spaces in the locations to be visited.

Registration and Cost There will be an upper limit of 15 participants. A minimum number of 8 participants will be required to make this trip viable. There will be a charge of £40 per person to cover the leader’s fee and expenses.

Clothing and equipment Normal field gear is required, including provision for wet weather. There is no need to carry a helmet or high-vis jacket, but a walking pole may well be useful for the steeper ground. A small hammer with a sharp chisel head, a stout penknife and a x10 hand lens come in handy if you like looking for fossils in loose blocks of rock.

SafetyOutdoor activities will be subject to all the usual care and precautions expected in the field as dictated by the terrainand weather conditions, with suitable clothing and sturdy footwear being required and participants expected to takecare.The terrain we are likely to encounter includes going over fields, uneven and rough ground in places, and steepground in a few places. As with most ‘field activity’, people with mobility issues will need to be prepared to exemptthemselves from parts of the itinerary as suggested in the itinerary outline above.Each person attending should be acquainted with the WGCG’s guidance on field activity (Item 7 on the WGCGwebsite at https://www.wgcg.co.uk/safety-documents/.

InsuranceMembership of WGCG (or a partner group such as LLPS or BCGS) is a requirement for insurance purposes (pleaseensure you are a fully paid-up member, separately from this registration process). You are advised to have suitabletravel insurance to protect against any losses that may arise from cancellation or loss of personal belongings.

ItineraryMeeting locations and a field guide will be forwarded to participants a week before the trip. The field guide will be inthe form of a PDF that can either be printed off, or taken into the field on your phone.Friday 12th June – informal walk around Ludlow, looking at building stones, starting at 3pm (for those who can getto the area early). No pre-field trip briefing will take place in the evening because Martin will be introducing thegeology of Shropshire to us on Thursday 14th May.Possible communal evening meal in Ludlow.Saturday 13th June – field trip to look at late Silurian, Devonian and Carboniferous successions around Ludlow andTitterstone Clee.Packed lunch required.Formal group evening meal, likely to be in or near to Ludlow.Sunday 14th June – field trip to look at Permian and Triassic red beds around Bridgnorth, possibly picking up one ortwo Carboniferous localities around Clee Hill beforehand if we didn’t squeeze them in on Saturday.Packed lunch required.Depart for home from Bridgnorth mid-afternoon.

RegistrationTo register for this field trip please send a completed registration form to julieharrald@googlemail.com by the registration deadline of Friday 1st MayRegistration Form

To view the field trip flyer please click here

Castle Quarry Kenilworth & Gibbet Hill Quarries - Geoconservation Work
2026-07-04 10:30 - 15:00
To enable the planned fieldtrips on 8th and 15th July to go ahead some geo conservation work is required at these two sites. It should be a maximum of 2 hours on each site only following extensive geoconservation work undertaken last year.

Castle Quarry KenilworthThe work is likely to mainly consist of cutting down vegetation that has grown in the last year so that the outcrops can be accessed.

Long trousers and long sleeved shirts are recommended on the Castle Quarry site in particular due to stinging nettles.

Tools required secateurs and shears, gardening gloves.

There is a steep access down the quarry face with very little to hand onto so is not suitable for those with reduced mobility or not sure on their feet.

The plan is to undertake the Castle Quarry work first at 10am and then move on to the Gibbett Hill site.Paid parking for non English Heritage members is available opposite the English Heritage shop (///moth.seats.covers).

Gibbet Hill QuarriesWhen complete at Castle Quarry or at 12MD we will go over to the Gibbett Hill site where this is less to cut down but important to create good access for the evening field trip. The same equipment is required for this site.

Paid parking bays are available within the university area, whilst free street parking after 6pm is available in Moreall Meadows. Meet in Moreall Meadows for 18.30pm

Extreme caution is required when crossing the busy Gibbet Hill Road to access these sites. If you have a high visibility vest or jacket, we recommend it is worn.

If you wish to help out please send an email to: julieharrald@googlemail.com

For the event flyer please click here

Day Field Meeting: Burton Dasset - Ray Pratt
2026-07-05 10:30 - 14:00
WGCG & BCGC Field Trip to Burton Dassett. Field trip Leader: Ray Pratt

The Burton Dassett Country Park, part of the Cotswolds, is located in Southern Warwickshire just off the M40. This is a popular upland leisure area for walkers and picknickers with good parking and toilet facilities. The park has been created in 1972 from what was a complex of quarries and intervening disturbed ground, mostly overgrown but with some good exposures of Liassic Marlstone Rock Formation chiefly about 200m south west of Windmill Hill. This large site incorporates several stratigraphic units and lithologies ranging from the Lower Jurassic Dyrham Formation to the Middle Jurassic Northampton Sand. Take a look at the 6-minute WGCG video on the geology of Burton Dassett https://youtu.be/p6oUfmzB3yQ

Car Parking at Burton Dassett costs. £3.50 per day (can be paid by card or cash)

The geological map of England and Wales (opposite) shows that the rocks of Southern Warwickshire and North Oxfordshire are in a zone (shaded blue) which stretches from Dorset through the Cotswolds to North Yorkshire. These rocks were formed during the Jurassic Period of time, roughly between 135 and 195 Ma (million years) ago. The rock layers are tilted very gently towards the south east and disappear below younger Cretaceous rocks (green).

The view WNW from the Beacon tower location is believed to be a consequence of Quaternary glaciation and the former site of a glacial lake.

WGCG and BCGS member, Ray Pratt, will lead this 2–3-hour trip. Following the trip participants may wish to walk around the area taking in the 12th Century Church, (made of local stone), the site of a Saxon graveyard, ancient springs, ridges and furrows and the Beacon, a circular tower built on one of the hill tops. A packed lunch is recommended. Alternatively, the Yew Tree pub in nearby Avon Dassett offers a relaxing spot for those wishing to socialise and refresh before setting off back home. For NT members Upton House and Gardens at Edge Hill is a short drive to the west.

To register for this trip, send an email to: geostart@btinternet.com

Evening field meeting at Kenilworth Castle Quarry
2026-07-08 18:00 - 20:00
Evening field meeting at Kenilworth Castle Quarry led by Stuart Burley and Jane Allum.

(W3W:///entry.songs.down, Grid Reference SP278 719)

For more information, please view the flyer by clicking here

Note that access down into the quarry is steep and is not recommended for anyone who isnot confident on their feet. No geological knowledge is necessary to learn about the rocks.

Paid parking is available at the Queen and Castle pub (///fever.sadly.watch).

To register for this trip, send an email to: warwickshiregcg@gmail.com

Evening field meeting at Gibbets Hill
2026-07-15 18:30 - 20:30
Evening field meeting at Kenilworth Castle Quarry led by Stuart Burley and Jane Allum.

W3W: larger.waving.ages, SP 305 751

For more information, please view the flyer by clicking here

Extreme caution is required when crossing the busy Gibbet Hill Road to access these sites. If you have a high visibility vest or jacket, we recommend it is worn.

Paid parking bays are available within the university area, whilst free street parking after 6pm is available in Moreall Meadows. Meet in Moreall Meadows for 18.30pm.

To register for this trip, send an email to: warwickshiregcg@gmail.com

WGCG Summer Social field walk in Leek Wooton
2026-08-05 17:45 - 19:45
Evening field meeting at Leek Wooton led by Jane Allum, Stuart Burley, and Ray Pratt

Members and their guests are invited to participate in our summer social event, centred around the Anchor pub in Leek Wooton. For the physically active we have scheduled a gentle summers evening walk along the Millenium Way footpath on the western side of Leek Wooton golf course to visit, to Woodloes Quarry. Sedimentological features are now clearly revealed following recent geo-conservation work by WGCG volunteers. The round trip walk to Woodloes Quarry is 2.4km over undulating ground on a well-established footpath. Returning to Leek Wooton we will meet up at the Leek Wooton bus stop, meeting up with others unable to undertake the earlier walk. Here we can view another exposure of the Helsby sandstone and its sedimentological features. We will then take refreshments in the Anchor pub. Please note that participants will need to pay for their own for food and drinks. Free car parking in Leek Wooton is available by the village hall and at the Anchor Pub.

The field trip Itinerary is:17:45 Meet, registration and HSE at Leek Wooton Golf Club – Groundsman area-free parking. (W3W:///captive.wove.anchorman SP 283 676) 18:00-18:15 Walk to Woodloes Quarry LGS 81 (W3W: ///admire.golden.continues, SP 276 679)18:15-18:45 Examine and discuss the geology of the quarry faces18:45-19:00 Return to cars and drive to Anchor Pub Car Park19:30 Congregate at Leek Wooton bus stop on Warwick Road for exposure 2.19:45 Head to Anchor pub for food & drinks https://www.anchorleekwootton.co.uk/

These exposures are of the Middle Triassic Helsby Sandstone Formation, known locally as the Warwick Sandstone, and nicely supplement the spectacular exposures of the Helsby Sandstone at Guys Cliffe, revealing complex bedding structures and beautifully preserved calcified fossil root structures. Participants will discuss the type of river deposits represented by the sandstones and what the root structures tell us about sand bar stabilisation and Triassic water tables.

To register for this trip, send an email to: julieharrald@googlemail.com

Please indicate if you will be participating in the walk or just meeting up in Leek Wooton

For the event flyer please click here

EMGS and WGCG Joint Residential Field Trip - Nick Chidlaw
2026-09-11 14:00 - 2026-09-13 15:30
EMGS: Residential Field Trip: Friday 11th – Sunday13th September 2026 Conducted Jointly with WGCG: Led by Nick Chidlaw‘South Malverns to Cleeve Hill’

Itinerary:

Friday p.m (c.2 – 5 p.m) – Gullet Quarry and Hangman Hill.Circular walk viewing Gullet Quarry, along crest of Swinyard Hill, to Hangman’s Hill to see aspects of the late Pre-Cambrian Malverns Complex & Warren House Volcanics and contrasting views of the Welsh Borderland and Severn Valley / Cotswold landscapes (subject to weather conditions). (approx. 3-4km.)

Gullet Quarry

Saturday a.m. p.m. (timings t.b.c.)Visit two contrasting Severn River cliff exposures in the Severn Vale:Late Triassic at Garden Cliff, Westbury (approx. 1km.); and,Early Jurassic at Hock Cliff (approx. 2km.). Picnic lunch taken en route (details t.b.c.)

Hock Cliff

Sunday (c.9:30 a.m to 3:30 p.m) – Cleeve Hill Traverse of Cleeve Hill to examine mid-Jurassic limestones (approx. 3km.).This will involve transferring all participants using some vehicles from our assembly point finish about at the golf clubhouse (north side of hill) to a car park by the radio masts on Cleeve Common (south side of hill).Picnic lunch en route with further use of the clubhouse facilities nearby.

Cleeve Hill

Participants will be expected to be suitably prepared for whatever weather conditions arise, and sufficiently mobile / fit for the walking involved……mostly on rough tracks and footpaths. In wet conditions Hock Cliff can get very muddy; Garden Cliff and the Malverns less so. Malvern terrain includes some steep sections.

Participants will also be required to make their own travel and accommodation arrangements.

Tewksbury is the focal point for this trip. The price will be £5 for a half day (Friday) and £10 per full day. Total trip £25.

To register email julieharrald@googlemail.com

For full details, click here to view the event flyer.

Etruria Marl: what it is; how it formed; why it’s special - Dr Bernard Besley
2026-09-17 19:15 - 21:00
In the English Midlands the term ‘Marl’ has meant, from time immemorial, any clay from which bricks can be made. The Etruria Marl is thus not a marl in the geological sense of the word, but a raw material formed by the red mudrocks of the Westphalian Etruria Formation, a marginal alluvial red-bed facies of the Langsettian to Bolsovian Productive Coal Measures. Etruria Marl is one of the most important heavy ceramic clays in the UK, being the dominant source of clay suitable for making high strength engineering bricks. It is favoured by the industry for its ease and flexibility of working, its low embodied CO2 content and its fast and fuel-efficient firing characteristics.

The ‘Marl’ of the Etruria Formation is a kaolinite-dominated, iron-rich silty claystone deposited at equatorial latitudes during a period of high global atmospheric oxygen. Its mineralogical characteristics derive from lateritic weathering in fault-bounded uplifts created during the first phase of Variscan deformation. Progressive deformation and uplift led to the northward spread of this facies into the southern part of the Pennine Basin, with complex intra-formational unconformities creating a syn-orogenic molasse. Depositional environments included alluvial plains with meandering channels and alluvial fans. Throughout the Etruria Formation hiatal periods are marked by complex palaeosols which lead to marked variability in the bulk composition of the clay.

While the Etruria Marl is best known in its type area in North Staffordshire, it has been – and still is – extensively worked in Warwickshire. Here its stratigraphic relationships have been poorly understood, but new borehole and seismic data allow some light to be cast on the sedimentological and tectonic events that accompanied its deposition.

The distinctive ceramic properties of the Marl derived from its ‘residual’ composition. The dominant kaolinite allows for the formation of a mullite-dominated ceramic matrix, while a small proportion of illite allows easy workability and prevents the clay from having refractory properties. A unique feature is the high iron content, which, apart from allowing the production of aesthetically pleasing fired products, allows partial melting at a late stage in firing on application of a reducing atmosphere. This stimulates the growth of fibrous mullite, producing the immensely strong semi-vitrified brick known as a ‘Staffordshire Blue’. The combination of high strength and low permeability made the Staffordshire Blue a major material for heavy civil engineering construction in the age before reinforced concrete.

The last 10 years have seen a renewed interest in Etruria Marl, following recognition that calcined kaolinite forms a pozzolanic material that is a viable feedstock for the production of LC3 cement. This cement formulation allows for a c. 45% reduction in the CO2 emissions in cement making, and is seen as an important contributor to the decarbonisation of that industry.

The talk will outline the general palaeogeographic and sedimentological evolution of the Etruria Formation, followed by a whirlwind tour of its properties and applications in ceramic and cement manufacture. If time allows, it will conclude with a review of the resource position as it relates to major substitution of ‘conventional’ cement raw materials by Etruria Marl.

Biography

Bernard studied at the University of Oxford, receiving a BA in Geology in 1976. He then came to Keele as a Ph.D. student working on the sedimentology and stratigraphy of red beds in the Westphalian of Central England, in collaboration with the National Coal Board. Between 1980 and 1985 he worked for Shell UK Ltd as an exploration geologist, undertaking wellsite duties in the North Sea and being involved in regional play fairway analysis and detailed prospect mapping leading to the discovery of the Galleon and Ketch gas fields in the UK Southern North Sea. In 1985 he returned to Keele as Lecturer in Sedimentology, where he continued his work into regional controls on late Carboniferous basin development in NW Europe. In 1996 he returned to the oil industry, spending another 5 years with Shell before setting up a freelance consultancy business. In that time he has worked on clastic hydrocarbon reservoirs of all ages and environments, being mainly concerned with the process of translating sedimentological models into numerical reservoir static models that can be used in a meaningful way for reservoir engineering purposes. He has also undertaken several stratigraphic and quality assessments of brick clays in the Late Carboniferous of the English Midlands, being an authority on the geology of the Etruria Formation. Since leaving Keele in 1996 he has continued his association with the Keele geoscience department through his Honorary Fellowship.

Venue:St Francis Of Assisi RC Church, 110 Warwick Rd, Kenilworth CV8 1HLhttps://maps.app.goo.gl/9CGWRNdgFfttDKtd7

WGCG Bridgnorth Field Trip - Led by Stuart Burley, Mike Allen & Ray Pratt
2026-10-04 10:30 - 16:00
Bridgnorth, straddling the Severn Valley in a spectacular setting, is well known for its striking topography, defined by the Bridgnorth Sandstone Formation, a bright orange-red, soft sandstone of Permian age, some ≈ 256-260 million years ago. The succession is composed of well-sorted, quartz arenite sandstones organised into large scale sets of cross-strata and has long been interpreted as an aeolian dune deposit (e.g. Shotton, 1937). It is one of several lower Permian aeolian dune-field (‘erg’) successions present within the United Kingdom and adjacent offshore regions and is thought to be broadly time-equivalent to the desert sandstones of the Kinnerton Sandstone Formation in Cheshire and the Rotliegend Group in the Southern North Sea Basin, including the Leman Sandstone, which formed the main gas-bearing interval. The Bridgenorth Sandstone Formation is considered to be the time equivalent of the Clent Breccias, and possibly the Kenilworth Sandstone Formation.

The Permo-Triassic successions of the West Midlands mainly overlie Carboniferous basement rocks that were deformed during the Variscan Orogeny and partly eroded during early Permian sub-aerial exposure. The Bridgnorth Sandstone Formation occurs in the Stafford Basin, a major half-graben structure filled principally by Permian-Triassic deposits of continental origin. It forms part of a chain of interconnected rift basins that extend from Lancashire in the north to Warwickshire and beyond in the south, forming a large rift basin system in which a variety of non-marine environments developed including large ergs, small isolated dune fields, sandsheets, basin margin alluvial fans and, in the case of the Irish Sea Basin, a large interior-draining playa lake. The Variscan highlands occupied an equatorial latitude and the Stafford Basin lay approximately 400 km further north under the influence of a semi-arid to arid climatic regime. Aridity was maintained because the region occupied an interior continental position within the Pangaea supercontinent, away from any maritime influence, and because it lay in the rain shadow of the Variscan mountain chain that stretched east-west through Europe.

Within the Stafford Basin, the Bridgnorth Sandstone formed as the product of the migration of straight-crested and crescentic dunes that coalesced laterally to form elongate ridges (‘draa’). Many bedform slip faces were orientated transverse to the palaeo-wind with bedform migration occurring to the west. Along slope winds modified the dunes on a seasonal basis. The Stafford Basin contains only 200-300 m of Permian strata. By analysing the shape slip face orientations of these fossilised dunes the predominant wind direction when the dunes were formed can be determined. Analysis indicates winds blew from the east and south-east which is consistent with sub-tropical trade winds found at 20 degrees north of the equator today.

Overlying the Bridgenorth Sandstone Formation is the basal conglomerate of the Kidderminster Formation (formerly known as the Bunter Pebble Beds) within the Sherwood Sandstone Group. These conglomerates were laid down approximately 250 million years ago during the early Triassic. They represent massive high-energy river systems that swept across the region during periods of flash flooding, eroding deeply into the landscape.

On this field trip we will learn how to recognise aeolian dune sandstones and compare the Bridgnorth Sandstone Formation with the depositional characteristics of the Kenilworth Sandstone Formation.

To register for this trip please email julieharrald@googlemail.com

For more details please view the event flyer by clicking here

Day Field Meeting: Smestow Valley and Wightwick Bank - Led by Andrew Harrison and Julie Schroder
2026-10-11 10:30 - 16:00
Following a recent BCGS geo-conservation effort, a quarried passage provides an excellent exposure of the Early Triassic Wildmoor Sandstone (Olenikian-Anisian). Deposited in the Staffordshire basin, these well sorted fluvial sandstones display excellent sedimentological features revealing the depositional setting. The phot (left) shows a depression behind the face of the quarried Wildmoor Sandstone exposing a fill of Quaternary till.

To get a flavour for the geology to be visited please take a look at a 2-minute video of the cutting that was made during the geo-conservation activity at this location. https://youtu.be/0lLNtNE9NNA

The morning will involve 30 minutes of walking in the Smestow Valley Nature Reserve where we will discuss the geomorphology, biodiversity and local history before visiting a geological exposure to examine the Wildmoor Sandstone. Note there are some small glacial erratics to be found near the exposure.

In the afternoon we will visit the Mount Hotel and Wightwick Manor to see the recently ‘re-discovered’ glacial erratics from Charles Benjamin Mander’s late 19th century ‘bouldery’ and learn about their connection with the Wightwick Manor erratics. (There will be a substitute in the unlikely event that the Mount Hotel is unavailable.) This will be followed by a visit to see the formal display and other erratics at Wightwick Manor, with time to visit their cafe to round off the day’s activities. Finish c.4.00 pm. For more details on the afternoon visits please refer to articles published in recent BGSS newsletters.

Click to access BCGS_Newsletter293.pdf

Click to access BCGS_Newsletter294.pdf

To register for this trip please email Julie Harrald julieharrald@googlemail.com

Geology & Industrial Archaeology of Harlech – Allison Barraclough
2026-10-15 19:15 - 21:00
More details to follow.

Venue:St Francis Of Assisi RC Church, 110 Warwick Rd, Kenilworth CV8 1HLhttps://maps.app.goo.gl/9CGWRNdgFfttDKtd7

Ask a Geologist - Under Dippy!
2026-10-17 10:00 - 16:00
To celebrate Earth Science Week 2026, the Warwickshire Geological Conservation Group (WGCG) is hosting a special “Ask a Geologist” session. Join us right beneath the tail of Dippy the Diplodocus at the Herbert Art Gallery & Museum in Coventry. WGCG geological experts will be at hand to discuss geology in our everyday lives, geological careers, and geological science in general. Come along and examine specimens in super detail with our blue tooth microscope. We will have a number of rocks, minerals and fossils on hand to be viewed and discussed, a number of posters, geological references and free brochures of nearby geology trails.

This is a drop in event, no need to book ahead.

Venue:Herbert Art Gallery & Museumhttps://maps.app.goo.gl/3w57Gv8vonQH8sxT9

Geology of Stonehenge - Peter Worsley
2026-11-19 19:15 - 21:00
A talk on the geology of Stonehenge by Peter Worsley.

More details to follow.

Venue:St Francis Of Assisi RC Church, 110 Warwick Rd, Kenilworth CV8 1HLhttps://maps.app.goo.gl/9CGWRNdgFfttDKtd7

WGCG Christmas Social
2026-12-12 14:00 - 17:00
The next Christmas Social of Warwickshire Geological Conservation Group will be on Saturday 12th December at Kenilworth Senior Citizens’ Club, Abbey End, Kenilworth CV8 1QJ at 7.00pm. This year will feature wine tasting.

Details TBC.
