Benhall Street

Stratford St Andrew is a small village and a civil parish just off the A12 road, in the East Suffolk district, in the English county of Suffolk. It lies 3 miles south west of Saxmundham, the nearest town. The parish had a population of 185 at the 2011 census.

Farnham is a village and civil parish about 3 miles (4.8 km) south-west of Saxmundham in the English county of Suffolk on the A12 road. Farnham is located west of Friday Street, south of Benhall Low Street and north-east of Stratford St Andrew.

Farnham Manor is a grade II listed house in Farnham, Suffolk, England. It is timber-framed and dates from at least 1602 based on a year marked on plasterwork in the house.

Benhall is a village and civil parish in the East Suffolk district of Suffolk, England. Located to the south of Saxmundham, in 2007 its population was estimated to be 560, reducing to 521 at the 2011 Census.

Glemham Hall is an Elizabethan stately home, set in around 300 acres (120 ha) of park land on the outskirts of the village of Little Glemham in Suffolk, England. It is a Grade I listed building, properly called Little Glemham Hall.

Great Glemham is a village and civil parish in the East Suffolk district, England, a mile and a half to the west of the A12 and roughly equidistant between Framlingham and Saxmundham. The parish takes the shape of an irregular triangle formed by two clay ridges flanking rolling countryside through which runs the channel of a seasonal watercourse, the Gull, flowing NW to SE to join the upper River Alde, which forms the village's eastern boundary. The civil parish had a population of 224 at the 2011 Census. The centre of the village is a Conservation area with numerous historic and listed buildings including its Grade I listed church, The Crown Inn, Crown House and K6 telephone box. The place-name 'Glemham' is first recorded in the Domesday Book of 1086, where it appears as Gl(i)emham, in the manors of Edwin Grim and Spearhafoc of Glaimham. Eilert Ekwall comments: "The first element of the names is possibly Old English glēam 'merriment'..." By analogy with Glandford in Norfolk, 'Glemham' could mean the 'village where sports were held'.Glemham House was built by Samuel Kilderbee in 1814 to the designs of Thomas Hopper and is the seat of the Earls of Cranbrook and Gathorne-Hardy family. With strong connections between the family and Benjamin Britten, the house hosted some of the earlier and more intimate performances of the Aldeburgh Festival of Music and the Arts including a notable recording by Julian Bream and Peter Pears. An earlier Glemham House, located closer to the village itself, had in the late eighteenth century been the home of George Crabbe, the author of the poem The Borough which formed the basis of Britten's 1945 masterpiece Peter Grimes. Britten worked closely with another Glemham resident, the librettist Eric Crozier, on many of his operatic compositions including The Little Sweep. Although set at nearby Iken Hall, the child characters in this work were transplanted from Glemham House, at that time the home of Jock and Fidelity Cranbrook. Both personal friends of the composer, Fidelity was also chair of the newly formed Aldeburgh Festival. Britten and Crozier adopted the names and personas of Jock and Fidelity's children and nephews for the opera, and the opera is "affectionately dedicated to the real Gay, Juliet, Sophie, Tina, Hughie, Jonny and Sammy – the Gathorne-Hardys of Great Glemham, Suffolk."

Sweffling is a village and a civil parish in the East Suffolk district, in the county of Suffolk, England. Nearby settlements include the town of Saxmundham and the village of Rendham. The medieval church of St Mary the Virgin, restored in 1832, is a grade II* listed building.

Rendham is a village and civil parish on the B1119 road, in the East Suffolk district, in the English county of Suffolk. It is near the town Saxmundham and the village Sweffling.

Benhall Green is a village in Suffolk, England. Benhall Green has a ford over the Fromus - which can be treacherous during heavy rains - and several protected wildlife sites, including the Wadd. The village also has a St Mary's Benhall Primary school, rated excellent by Ofsted [1], a new wooden play area, swings and slides, a phone box, and a noticeboard. There is a small farm shop on the A12 just outside the village, the Railway Farm Shop. In the village is a cottage built in 1698 with distinctive pargeting.

SET Saxmundham School (formerly Saxmundham Free School) is a free school in Saxmundham, Suffolk, East Anglia, with approximately 309 pupils. It was rated "good" by Ofsted in May 2014. In March 2018 Ofsted carried out a short inspection of the school where it maintained its "good" rating. It opened in 2012 with 105 pupils out of a total of 312 places available. The school now has 600 places available. In June 2023 the Seckford Education Trust announced it would be closing the school in August 2024.

Little Glemham is a small village on the A12 road, in the East Suffolk district, in the county of Suffolk, England. The population of the parish at the 2011 Census was 187. Nearby settlements include the villages of Wickham Market and Marlesford. Little Glemham has a church, St. Andrew's, a pub and a hall called Glemham Hall. The corresponding village of Great Glemham is a few miles away.

The Norwich Crag Formation is a stratigraphic unit of the British Pleistocene Epoch. It is the second youngest unit of the Crag Group, a sequence of four geological formations spanning the Pliocene to Lower Pleistocene transition in East Anglia. It was deposited between approximately 2.4 and 1.8 million years ago, during the Gelasian Stage. The Norwich Crag is a marginal facies of the thicker, much better developed sedimentary sequence in the southern North Sea basin. It outcrops in the eastern half of the counties of Norfolk and Suffolk, and is also represented in Essex and Hertfordshire. It was deposited in a near-shore environment, and comprises a range of sands, silty clays and flint-rich gravels representing various transgressive and regressive marine episodes. It rests in some places on the Red Crag Formation and in others unconformably on Coralline Crag, Palaeogene formations and Chalk Group bedrock. It is overlain by the Wroxham Crag Formation, and unconformably by the Kesgrave Catchment Subgroup (part of the Dunwich Group) and Mid Pleistocene glacigenic deposits. Norwich Crag fossil fauna and flora have been studied since the 19th century for information about environmental conditions during the early Pleistocene. They provide evidence for a general climatic cooling trend from the Pliocene to the Pleistocene.