BeachcombingSunday 9th April 2000
When I last visited Mappleton in 1991, the sea defences had just been put in place. Boulders the size of large freezers had been shipped in from Scandinavia. They had been arranged in a protective fan at the end of an access track down to the beach and as a narrow breakwater of boulders stretching out to sea. During the last nine years, the breakwater has acted as a barrier to the movement sand and pebbles along the shore. This beach-making material would normally gradually move southwards,as a result of longshore drift.
There is now sufficient beach to protect the village of Mappleton but, on the other side of the breakwater, it's a different story. The beach level is 3 or 4 feet lower. Walk down the shore to the south of the breakwater and the beach begins to peter out altogether. This morning, four or five hours after high tide, there still isn't enough beach showing for us to be able to continue our walk as far as Cowden, just a mile along the coast. Starved of a supply of beach-making materials, this section of coast will now, ironically, be eroded at a faster rate as a result of the new coastal defences.
We found a fossil oyster known as Gryphaea, or 'Devil's Toe-nail', eroded out of the soft cliff.
A Kestrel hovered at the clifftop, where we saw our first Wheatear, a summer visitor. At nearby Hornsea Mere we saw our first Sand Martins.