Field Meetings

Travel is by members’ cars, or possibly other transport if the numbers are sufficient, with costs shared between members at a standard rate. When a visit requires specific equipment – for instance hard hats, torches, wellingtons, high visibility jackets – you will be notified in advance. You will also be required to confirm that you have read the risk assessment for the visit.

Field Meeting Booking
Booking can be done either at lecture meetings or by clicking on the "Field Meeting Registration" link when it is shown in the details below. For one day meetings, the cut off time for booking is 12 noon on the day before the meeting. The longer field meetings will usually have earlier booking cut off times. The booking link will not be available until booking opens and will disappear once the booking closing time has passed.

All attendees need to sign a Risk Assessment Document
Safety on field meetings is taken very seriously. Should you be unsure about either the risks involved or your ability to participate, you must seek advice from the leader. Please make sure you understand the risk assessment offered by the leader of the meeting and that you have the safety equipment specified. You must declare, at the time of booking, any disabilities or medical conditions that may affect your ability to safely attend this field meeting. In order to ensure the safety of all participants, the RGS reserves the right to limit or refuse attendance at field meetings.
By signing up to a field meeting you are confirming you have read this safety briefing note, are accepting the risks and responsibilities and are permitting the RGS to keep your contact details for the duration of the trip.


2025-10

Sunday 12 October 2025

Sedimentology and diagenesis of the Arden Sandstone (Triassic), Warwickshire

Leader: Stuart Burley (Warwickshire Geological Conservation Group)
Field Meeting Registration


The Arden Sandstone Formation of central and western England is a thin arenaceous unit in the Late Triassic Mercia Mudstone Group. Sedimentological and palaeontological data point to lacustrine depositional conditions, in contrast to the red desert mudstones above and below which were deposited as continental dryland desert floodplains. The Arden Sandstone records deposits of the lake margins and may be the high stand lateral equivalent of the halite and gypsum deposits which formed in the lake centre. The Arden Sandstone in these outcrops is up to 7 m in thickness. It is typically fine grained, cross stratified and contains a fauna which includes clam shrimps, crustaceans and bivalves, in addition to the fish and reptiles.

Picture: From Canal & River Trust SSSI panel


Programme 2025

The programme for 2025 as currently proposed is also available as a pdf document.

Other programmes

Previous years programmes and other programme information can be found on the About us page.