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Interesting Facts About Brighton

Introduction

Brighton is a seaside resort and one of the two main areas of the city of Brighton and Hove in the county of East Sussex, England. It is located 47 mi (76 km) south of London. Archaeological evidence of settlement in the area dates back to the Bronze Age, Roman and Anglo-Saxon periods. The ancient settlement of “Brighthelmstone” was documented in the Domesday Book (1086). The town’s importance grew in the Middle Ages as the Old Town developed, but it languished in the early modern period, affected by foreign attacks, storms, a suffering economy and a declining population. Brighton began to attract more visitors following improved road transport to London and becoming a boarding point for boats travelling to France. The town also developed in popularity as a health resort for sea bathing as a purported cure for illnesses.

History of Brighton

The first settlement in the Brighton area was Whitehawk Camp, a Neolithic encampment on Whitehawk Hill which has been dated to between 3500 BC and 2700 BC. It is one of six causewayed enclosures in Sussex. Archaeologists have only partially explored it, but have found numerous burial mounds, tools and bones, suggesting it was a place of some importance. There was also a Bronze Age settlement at Coldean. Brythonic Celts arrived in Britain in the 7th century BC, and an important Brythonic settlement existed at Hollingbury Castle on Hollingbury Hill. This Celtic Iron Age encampment dates from the 3rd or 2nd century BC and is circumscribed by substantial earthwork outer walls with a diameter of c. 1,000 ft (300 m). Cissbury Ring, roughly 10 mi (16 km) from Hollingbury, is suggested to have been the tribal “capital”.

General Info

Brighton lies between the South Downs and the English Channel to the north and south, respectively. The Sussex coast forms a wide, shallow bay between the headlands of Selsey Bill and Beachy Head; Brighton developed near the centre of this bay around a seasonal river, the Wellesbourne (or Whalesbone), which flowed from the South Downs above Patcham. This emptied into the English Channel at the beach near the East Cliff, forming “the natural drainage point for Brighton”.

Behind the estuary was a stagnant pond called the Pool or Poole, so named since the medieval era. This was built over with houses and shops from 1793, when the Wellesbourne was culverted to prevent flooding, and only the name of the road (Pool Valley, originally Pool Lane) marks its site. One original house survives from the time of the pool’s enclosure. Behind Pool Valley is Old Steine (historically The Steyne), originally a flat and marshy area where fishermen dried their nets. The Wellesbourne occasionally reappears during times of prolonged heavy rain; author Mark Antony Lower referred to an early 19th-century drawing of the Royal Pavilion showing “quite a pool of water across the Steyne”.