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.
Wednesday 22 July 2026
Lickey Hills
Leader:Ray Pratt, WGCG
Field Meeting Registration
Landscape and Geology of the Lickey Hills Country Park with Ray Pratt of the Warwickshire Geology and Geoconservation Group
The geology of the Lickey Hills has been mulled over by numerous geologists over the past 200. Despite this there still remains plenty of debate regarding the geological history of the structure.
The Lickey Ridge is a fault-bounded horst exposing an inlier of Ordovician ortho-quartzite, flanked by Late Carboniferous, Permian and Triassic deposits. Folding within the horst is complicated and made possible by interbedded clay-rich layers of volcanic origin. Sedimentary structures are preserved and there are rare trace fossils At the northern end of the ridge the Ordovician ortho-quartzites are unconformably overlain by Silurian sandstone
Picture: BGS Photo: Southern end of Cock Hill (Rubery Hill)