Hemley

Bucklesham Mill River – sometimes referred to simply as Mill River – is a tributary of the River Deben in Suffolk, England. It is 11.3 km (7.0 mi) long and with the Newbourne Stream which flows into it at Newbourne it constitutes the Bucklesham Mill River Water Body with a catchment area of 46.298 km2 (17.876 sq mi). The river gets its name from the Bucklesham watermill, located on Watermill Road where it crosses the river leading to Newbourne. The river rises at a number of locations on the outskirts of Ipswich and after flowing through diverse varieties of landscape it reaches the River Deben at Kirton Creek: The river acts as a natural wildlife corridor linking several County Wildlife Sites: The Mount Brightwell Gazing Meadows Valley Farm Meadow

Newbourne is a village and civil parish in the East Suffolk district of Suffolk, England. It lies on the peninsula between the River Orwell and the River Deben, to the east of Ipswich and south of Woodbridge.

Ramsholt Cliff is a 2.1-hectare (5.2-acre) geological Site of Special Scientific Interest north-west of Ramsholt in Suffolk. It is a Geological Conservation Review site, and it is in the Suffolk Coast and Heaths Area of Outstanding Natural Beauty.This site is very important historically because it was the basis for the distinction of the Pliocene Coralline Crag Formation as a new stratigraphical division by the nineteenth-century geologist, Edward Charlesworth. The well preserved fossils include several unusual species.Most of this steeply sloping site on the bank of the River Deben is inaccessible, but a footpath runs along the top and a track leads to a small area of bank.

Waldringfield is a village and civil parish in the East Suffolk district, in the county of Suffolk, England. It is situated on the bank of the River Deben within the Suffolk Coast and Heaths Area of Outstanding Natural Beauty, 4 miles (6.4 km) south of the town of Woodbridge and 8 miles (12.9 km) east of the county town of Ipswich. All Saints' Church dates from the 14th century. Restored in the 19th century, it is a grade II* listed building.Waldringfield Heath, between the village and Martlesham on the edge of Ipswich, is the site of Waldringfield Golf Club.It also has a yacht club called Waldringfield Yacht Club. A probable Early Pliocene macaque molar from the Red Crag Formation in Waldringfield, represents one of the oldest and northernmost records of the genus in Europe reported to date.

Deben Estuary is a 981.1-hectare (2,424-acre) biological Site of Special Scientific Interest (SSSI) covering the River Deben and its banks 12 kilometres (7.5 miles) from its mouth north of Felixstowe to Woodbridge in Suffolk. It is a Ramsar internationally important wetland site and a Special Protection Area under the European Union Directive on the Conservation of Wild Birds. It is also in the Suffolk Coast and Heaths Area of Outstanding Natural Beauty. It partly overlaps two geological SSSIs, Ferry Cliff, Sutton and Ramsholt Cliff.The site has been designated an SSSI for its overwintering waders and wildfowl, and for its diverse saltmarshes. It has internationally important overwintering redshanks and nationally important numbers of dark-bellied brent geese, shelducks and black-tailed godwits. The estuary also has three nationally rare plants and a nationally rare mollusc.

Kirton is a village and a civil parish in the shire county of Suffolk, England, situated off the A14 road, about 4.5 km (2.8 mi) from Felixstowe and around 10 km (6.2 mi) from Ipswich. The closest train station to Kirton is Trimley. According to the 2011 census, Kirton had a population of 1,146. It is located between the River Deben and the River Orwell. The village of Kirton covers a total area of 8.3 km2 (3.2 sq mi). As the county of Suffolk lacks quarries, many of the buildings are made from flint, clay and timber.Kirton and Falkenham share the Parish Council, the school, the Village Hall, and most of the organisations. Kirton has a church and it also has access to a primary school.

Newbourne Springs is a 15.7-hectare (39-acre) biological Site of Special Scientific Interest in Newbourne in Suffolk. It is owned by Anglian Water and managed by the Suffolk Wildlife Trust.Most of this site is a narrow valley with a fast-flowing stream with alder carr and fen. Drier and more acidic soils have grassland, woodland, scrub and bracken heath. The site is actively managed, producing diverse flora and many breeding and migratory birds such as treecreepers, nuthatches and sedge warblers.There is access from Woodbridge Road, which goes through the site.

Rockhall Wood Pit, Sutton is a 5.3-hectare (13-acre) geological Site of Special Scientific Interest west of Shottisham in Suffolk. It is a Geological Conservation Review site both for its quaternary and neogene deposits.This site has excellent exposures of the Pliocene Coralline Crag Formation, with a vertical sequence of diagenetic changes and rich fossil fauna. It is described by Natural England as probably the most important Pliocene site in Britain.This site is private land, but part has been converted by Geo Suffolk into a 'Pliocene Forest', with trees similar to ones which would have grown in Suffolk four million years ago.

Ramsholt is a small village and civil parish within the East Suffolk district, located in the county of Suffolk, England. It is situated on the northern shore of the River Deben. In 2001 the parish had a population of 32. The parish church of All Saints is one of 38 surviving round-tower churches in Suffolk and is a Grade II* listed building.The village economy revolves around the pub next to the river dock.Ramsholt was a historic fishing town before Felixstowe docks.

Falkenham is a village and a civil parish in the East Suffolk district, in the English county of Suffolk, near the village of Kirton and the towns of Ipswich and Felixstowe. The population of the civil parish as of the 2011 census was 170.

Waldringfield Pit is a 0.8-hectare (2.0-acre) geological Site of Special Scientific Interest between Martlesham Heath and Waldringfield in Suffolk. It is a Geological Conservation Review site.This site exposes a sequence of Pleistocene deposits, with the early Red Crag overlain by Waldringfield Gravels, the lowest unit of the Kesgrave Sands and Gravels, which were deposits on the bed of the River Thames before it was diverted south by the Anglian Glaciation around 450,000 years ago. Waldringfield Pit is the type site for the Waldringfield Gravels.The site is private land with no public access.

Colneis is a hundred of Suffolk, consisting of 16,712 acres (67.63 km2).Running from the south-east outskirts of Ipswich to the North Sea coast, the hundred is made up of the land between the estuaries of the rivers Orwell and Deben. It is one of the smallest in Suffolk, being only about four miles (6.4 km) wide and ten miles (16 km) long between its border with Carlford Hundred and the cliffs at Felixstowe. It lies within the Colneis Deanery, in the Archdeaconry of Suffolk. It was one of seven Saxon hundreds grouped together as the Wicklaw Hundreds.Listed as Colneyse in the Domesday Book, the origin of the name is not known for sure, though the suffix -ness, meaning "headland" seems probable. The col may be the old name of the Deben before its renaming after Debenham.The name survives as that of a Junior School in Felixstowe.