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Red hill (salt making)
Red Hill is an archaeological term for a small mound with a reddish colour found in the coastal and tidal river areas of East Anglia and Essex. Red Hills are formed as a result of generations of salt making, deriving their colour from the rubble of clay structures used in the salt-making process that have been scorched red by fires used to evaporate sea water to make salt cakes.〔〔DR Wilson, ''Air Photo Interpretation'' (Tempus, 2000)〕 They date from the Bronze Age, Iron Age and into the Roman period.〔
==Archaeological investigation==
Small red mounds had been a noticeable feature of the coastal landscape in Essex and East Anglia for many centuries,〔 but the first archaeological investigation〔Fawn, A.J., Evens, K.A., McMaster, I., Davies, G.M.R. (1990) 'The Red Hills of Essex; Salt making in Antiquity' Published by Colchester Archaeological Group. (ISBN 0 9503905 1 8)〕 into Red Hills and their function wasn’t until 1879, when William Stopes excavated a group of them near Peldon, on the Essex mainland opposite Mersea Island.〔Stopes, H. (1879) 'The Salting Mounds of Essex' in Archaeological Journal XXXVI〕 Originally Stopes thought that the mounds were Medieval in date, and were used for producing alkalis for glass making.〔 However other investigations, such as those by Revd J.C. Atkinson, who compared them to similar mounds in Yorkshire, saw the mounds as prehistoric or Roman in date.〔 In 1906 the Essex Archaeological Society and Essex Field Club created the ''Red Hills Exploration Committee'' to identify the purpose, age and extent of the Red Hills, undertaking excavations at Langenhoe and Goldhanger, and later in 1909 at Canewdon on the River Crouch.〔Reader, F.W. (1908) 'Report of the Red Hills Exploration Committee 1906-7'. Proceedings of the Society of Antiquities XXII, 2nd Series〕〔Reader, F.W. (1910) 'Report of the Red Hills Exploration Committee 1908-9'. Proceedings of the Society of Antiquities XXIII 2nd Series〕 Conclusions as to the exact nature of the type of activity carried out at the Red Hills were still lacking however, with archaeologist Flinders Petrie suggesting that the sites were where kelp and seaweed had been burned in order to create alkali solutions for soap and glass,〔 whilst other archaeologists suggested pottery kilns.〔 However some early comparisons to salt-processing sites in Brittany in the early Twentieth century lead to tentative suggestions that salt was at the heart of the Red Hills' purpose,〔Wilmer, H. (1908). 'Late Celtic remains of the coast of Brittany comparable to the Red Hills' in Reader, F.W. (1908) 'Report of the Red Hills Exploration Committee 1906-7'. Proceedings of the Society of Antiquities XXII, 2nd Series〕 with further excavations in Britain of sites similar to the Red Hills of Essex and East Anglia at Ingoldmells in Lincolnshire and Hook in Hampshire choosing this interpretation over the alkali explanation.〔 Ernest Linder's 1937-1941 excavations of Red Hills at Canvey Island in South Essex began to draw upon salt-making as the main suggestion for what had been occurring at these mounds.〔〔Linder, E. (1939) 'The Red Hills of Canvey Island' in Essex Naturalist XXV1, III〕 During the 1950s, 1960s, 1970s and 1980s further excavations were carried out around Southend-on-Sea〔Helliwell, L. (1960) 'Finds, Accessions and Fieldwork 1955-59', Transactions of the Essex Archaeological Society XXV Pt.3〕 and Canvey Island in South Essex,〔 around the Dengie peninsula and Maldon in central Essex,〔 and around Harwich and the Blackwater and Colne estuaries in North-East Essex.〔 Red Hills and salt making at Salthouse (Norfolk) were also described by Hoskins.〔WG Hoskins, ''Fieldwork in Local History'', (Faber & Faber Ltd. 1967, pp. 154-158)〕 During these investigations much information was gathered both on the date and purpose of the Red Hills.〔
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