out from behind one of the stones at sunset, and try to grab the horse's reins before vanishing. This, although terrifying the animals, seems not to have perturbed the man unduly. However, he ordered that the stone in question be laid upon his grave after his death, in an attempt at 'laying' the apparition. James Reynolds died in 1941 and, in accordance with his wishes, the boulder now lies atop his grave, his wife Ann Elizabeth also being interred there in 1967. There is no record as to whether or not the 'exorcism' was successful, and indeed, a local woman who knew the Reynolds could not confirm the story. The other stone of the pair can now be seen lying against the north wall of the churchyard. Orben Beck is a tiny pond of half an acre located in a cliff-top caravan park and only yards from the sea. Depths range from six to twelve feet. The pond is popular with anglers and holds a variety of coarse fish. Abbey Farmhouse is a Grade II listed building and is located on the Eastern side of Beeston Regis Common. Within the parish is Beeston Hall School, the largest boarding preparatory school in East Anglia. Beeston Regis Hall was once a family home of the Wyndham Ketton-Cremers on the Beeston Regis Estate, part of the much larger Felbrigg Estate, the family seat. In 1940 a German bomb hit the school, causing slight damage. The Hall was leased to Thomas Tapping and his wife Bessie, who opened the private Beeston Hall School in 1948. In 1967 the school became an incorporated trust, and in 1970, following the death of Robert Wyndham Ketton-Cremer, the last squire of Felbrigg, the school acquired the freehold and about of land. Over the years the school has expanded; it is the biggest employer in the parish. It has also acquired other surrounding land including Beeston Hall Common, which it purchased from the parish of Beeston Regis. Beeston Hill (Beeston Bump) Beeston Hill, or Beeston Bump as it is called locally, is a cliff-top hill which overlooks the sea and the village. At 207 feet (63m) high, it is the dominating feature of the parish. The hill, part of Cromer Ridge, was once two symmetrical round flat-topped hills in the shape of giant molehills: geological features known as kames. The two hills were left behind when glaciers retreated northwards