36 At the Folkestone Warren, Upper Cretaceous Chalk overlays the gault. This is Lower and Middle Chalk, the latter dating back to about 88 million years. Fossils found are mostly echinoids (sea urchins) and brachiopods rather tham ammonites though they do occur in the Lower Chalk. The Folkestone Warren has been the scene of several landslips - a large one taking place in 1915, demolishing houses and a railway line. After heavy rain, a rotational movement takes place along slip-planes in the gault, causing a collapse of the clay and the chalk above it. A later landslip took place in 1940. David Turner Report of Council 1981 The Council of the Club met six times during the year. At the Annual General Meeting in March, the President, Mr. A. Snelling, talked about early man and his stone tools, which included a demonstration of flint knapping. During the year Mr. A. Snelling moved to Cheshire and Mr. A. Boniface agreed to take over until elections could be held at the next A.G.M. Mr. M. Parker took over the job of Membership Secretary. At the end of the year membership stood at 359. Regrettably Council had to decide to raise the subscription rates to £5 per annum for individual adult members, £2 per annum for students under 18 and £6 per annum for family and library membership. The Club organised 33 meetings during the year. Speakers included Col. A. Maitland Emmet on the Smaller Moths of Essex, Mrs. N. Chapman on the