Annery kiln

Weare Giffard is situated near the tidal limit of the River Torridge, and coal and limestone had been brought up-stream by boat for a long time previously to the building of the Rolle Canal in 1823 - 1827. Due to the corrosive properties of quick lime, the product of the kiln, it was essential that kilns should be situated as closely as possible to the agricultural fields on which it was to be spread. Should the quick lime become wet during transport by the farmer to his farm, it would corrode its container and damage the wagon or pack-animal on which it was being transported. Culm, a form of imperfect anthracite, was mined in Devon at Tavistock and Chittlehampton as well as being imported from South Wales via Bideford. The limestone largely came from Caldey Island off the South Wales coas

Annery kiln

Weare Giffard is situated near the tidal limit of the River Torridge, and coal and limestone had been brought up-stream by boat for a long time previously to the building of the Rolle Canal in 1823 - 1827. Due to the corrosive properties of quick lime, the product of the kiln, it was essential that kilns should be situated as closely as possible to the agricultural fields on which it was to be spread. Should the quick lime become wet during transport by the farmer to his farm, it would corrode its container and damage the wagon or pack-animal on which it was being transported. Culm, a form of imperfect anthracite, was mined in Devon at Tavistock and Chittlehampton as well as being imported from South Wales via Bideford. The limestone largely came from Caldey Island off the South Wales coas