I walk in all weathers and always carry a camera. I like to record what I see and the changes I notice even if the conditions are not always favorable, as on this occasion. This March day on Charlton Down was marked by hazy sun, cold wind, and the merest hint of spring. Ploughed fields were white with chalk and flint nodules. Short shoots sprouted from the furrows. Sugar beet greened some fields. Trees bare but for lichen cast weak shadows on the turned soil, while neat laid hedges divided the vista. Farms and barns topped the horizons. Rusting agricultural equipment stood isolated along the pathways. A rolling misty landscape of intersecting curves surrounded my hill-top village.
The first selection of photographs taken at Kimmeridge Bay in Dorset, England, yesterday (27 March 2015) showing details of the natural patterns, textures, and colours of the rocks. The rocks are described as rhythmically inter-bedded blocky, organic-poor mudstone and fissile, organic rich shale.
For information about the geology of this location look at:
John C. W. Cope Geology of the Dorset Coast, Geologists’ Association Guide No. 22, Geologists’ Association, 2012, pp 159-167, ISBN978 0900717 61 1.
M. A Woods (compiler) Geology of south Dorset and south-east Devon and its World Heritage Coast, British Geology Survey, NERC, 2011, pp 61 – 67, ISBN 978 085272654 9.
One rainy morning I walked the coastal path along the terrace at the foot of Rhossili Down in Gower. Clouds shrouded the slopes of the Down above me. Ahead of me, Burry Holms and Llangennith Burrows were part concealed by mist. Below me, the tide was going out – far out. The sand on the beach was still wet from the waves and the rain. Slowly the cloud cover thinned and allowed a filtered light to penetrate. The pale light was reflected by the shore, high-lighting the sea-sculpted rows of ridges and ripples in gentle gleaming silver. A stream cascading from the height of the Down worked its way down to the beach, where it spread out in a fan of interweaving channels that cut across the parallel ridges on its way to the water’s edge. Coloured sediments carried by the stream tinted the silvery patterns and made them seem opalescent.
Dark streaks drawn into abstract designs by the swash and back-swash of waves sometimes decorate the succession of driftlines on the sandy beach at Rhossili Bay as the sea recedes. The blue tinge of the darker areas makes me wonder whether they are composed of comminuted fragments of blue-black mussel shells.