marine clay with darker freshwater deposits from the Minsmere River. History Before 1947 In the Domesday Survey in 1086 Minsmere was known as Menesmara or Milsemere. It is recorded as having six households headed by freemen with one plough team. The manor, which was in the Hundred of Blythling, was held by Roger Bigot. Ranulf de Glanvill, King Henry II's Lord Chief Justice, founded a Premonstratensian abbey on the marshes at Minsmere in 1182. The area was embanked to protect the abbey from the sea and to reclaim farmland, but still suffered several years of severe flooding in the 14th century. The site was abandoned in 1363, and the stone from the buildings was used to rebuild Leiston Abbey at a new location further inland. The remains of the abbey church, fish pond and other buildings can still be detected below ground, but the only visible structure is the ruined chapel of St Mary, built within the nave of the former church. The lower section of the chapel was built soon after the demolition of the abbey in 1363, and the brick upper parts are thought to have been added by former abbot John Green, who lived there as a hermit when he retired from his post in 1527. The site was abandoned in 1537 during the Dissolution of the Monasteries, the only further construction being a pillbox that was built inside the chapel during World War II. The ruins are a scheduled monument of national importance. Peat cutting took place at Minsmere from at least the 12th century, and a 1237 description of the coastline describes Minsmere as a port. In a survey of 1587, an early Tudor period artillery battery, constructed sometime after 1539 at Minsmere, was in ruins; the survey recommended that it be rebuilt. A coastguard station operated at Minsmere in the 1840s in an attempt to control smuggling along this stretch of the coast. In about 1780 a sandbank closed the mouth of the Minsmere River, creating a large freshwater wetland on its inland side. The reeds that grew there were cut for thatching, and access was improved by using sand from the higher alluvial areas to build tracks across the marshes. These marshes were enclosed and drained for agricultural use in 1812 and 1813, following the passing of the relevant Act in 1810, with the main sluice being built to control drainage to the