GEOSUFFOLK RIGS
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GEOCONSERVATION: PRACTICAL SITE-MANAGEMENT AT SUTTON KNOLL B. HALL Barry Hall, a GeoSuffolk committee member, began by describing how he had latterly become involved with Geoconservation in Suffolk following an earlier association with the county via his work with the Meteorological Office and various postings to local RAF stations. Using his knowledge from a subsequent career in horticulture he explained how the principles, tools and techniques commonly associated with gardening are equally applicable to the conservation of geological sites of special scientific interest, otherwise SSSI’s. However, the word ‘conservation’ had to be used carefully as it implied keeping something in a steady state of preservation which was clearly not feasible with regard to a constantly weathering exposure. The phrase ‘site-management’ was preferred as it described the best possible presentation and maintenance of an exposure. Sutton Knoll, near Woodbridge, an island of Coralline Crag specific only to Suffolk and surrounded by younger Red Crag deposits, was first encountered on a field trip in May 2003. Towards the end of the day the group had stopped on a track around the SW side of the knoll, just outside of the SSSI itself, opposite the so-called ‘Chicken Pit’. Following a climb over a low fence and a scramble through elder, bramble and nettle the Coralline Crag was located hidden beneath dense vegetation and it transpired that many years before an unusual assemblage of well preserved shells had been found nearby. It could be argued that this is how geology should be with the sudden unexpected discovery against all odds having a definite appeal. However, for known sites or for sites of choice, the benefits of a different approach would be advocated, different certainly from the twice annual flail that hitherto had masqueraded as management. The alternative, simply stated, would be clearly visible exposures with easy access at all times that included suitable viewing areas able to accommodate small groups. The ‘at all times’ was the real challenge as the value of any hand or machine clearance would always be wasted if simply allowed to overgrow again. It was suggested that any gardeners present would appreciate just how quick that could be. Initial work, somewhat experimental at that stage, commenced in October 2004 by marking out and clearing by hand a 10 x 4 metre section of that previously hidden Coralline Crag well in advance of proposed JCB excavation. The prime need was to find out what it took to keep it clear. Also, close by and unseen on that first visit, was an old excavation showing the contact between the Red Crag and the London Clay beneath. Although the sides and a metre wide parapet were cleared of nettle and bramble there had been a long wait for the seasonal pond to drain off before digging out the accumulated pond bottom and aquatic flora. A surprise had been the discovery of closely packed crag infilled borings of the piddock Zirfaea crispata in the London Clay, which were quite rare. A sample had been preserved in the Ipswich Museum. Thereafter, to connect both these fresh exposures, a 150 m path had been cut from the entrance gate through the nettle and bramble which had then gradually grassed over from frequent mowing. Trans. Suffolk Nat. Soc. 43 (2007)