 
 
              
              A Watercolour 
              by John Davis ©  
                 
                Geologically the Cotswolds is a limestone mass 
                  stretching 100 miles SW by NE with Bath to the south and Chiiping 
                  Campden to the north. The 'wold' iis old English for 
                  'upland common'. These rolling hills are used mainly for sheep 
                  and arable farming. The local breed, 'the Cotswold' can produce 
                  a fleece in excess of 10 Kilos. At one time the area had half 
                  a million sheep and the wool trade with europe was significant. 
                  Flemish weavers were brought to England and the merchants became 
                  wealthier than King. Numerous fine homes and churches were built 
                  from the wealth of this trade. This trade lasted several centuries 
                  but when it was the human devastation was dreadful. It did mean 
                  however that the towns in the Cotswolds have been left undeveloped 
                  as can be seen at places like Chipping Campden. These are now 
                  preservation areas and the villages will remain as they were 
                  built many centuries ago.
                Cotswold Stone
                The famous stone which colours the landscape, 
                  the homes and the buildings is limestone, found commonly across 
                  England, but is dramatically demonstrated in the Cotswolds. 
                  Here the limestone is oolitic (egg-stone' in Greek), which is 
                  soft when first exposed and continues to harden on contact with 
                  the air - a perfect building material, that can be readily sawn 
                  on quarying. It was used extensively in the Middle Ages - the 
                  finest example being St Paul's Cathedral, London. 
                The Thatched and Stone Roofs