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Covehithe is a village and civil parish in the East Suffolk district of the English county of Suffolk. It lies on the North Sea coast around four miles (six kilometres) north of Southwold and seven miles (eleven kilometres) south of Lowestoft .
Thatched church seen within the ruins. St Andrew's Church is a partly redundant Anglican church in the hamlet of Covehithe in the English county of Suffolk.It is recorded in the National Heritage List for England as a designated Grade I listed building, [1] Part of the church is in ruins and this is under the care of the Churches Conservation Trust. [2]
Benacre NNR consists of areas of open water lagoons and reed beds along the Suffolk coast including Benacre Broad, Covehithe Broad and Easton Broad and extending as far south as Reydon. The reserve features extensive reedbeds, woodland and heathland, as well as pits created by gravel extraction.
Benacre is a village and civil parish in the East Suffolk district of the English county of Suffolk.The village is located about 5 + 3 ⁄ 4 miles (9 km) south of Lowestoft and 1 + 1 ⁄ 2 miles (2 km) north-east of Wrentham, between the main A12 road and the North Sea coast.
The manor, which was combined with Covehithe to form the manor of South Cove and North Hales, was held by a variety of owners until it was bought by the Blois family in the late 17th century. [c] [18] [22] [23] A second manor, named Polfrey or Blueflory-Cove, was owned by the Gooch baronets of Benacre Hall by the start of the 19th century.
Fanny Emily Farr was born in 1847 in Covehithe, Suffolk, England, the daughter of the Rev. John Farr, rector in Gillingham, Norfolk, and Emily Caroline Cobbold Farr, daughter of brewer John Cobbold and poet Elizabeth Cobbold. She was educated at Queen's College and Bedford College in London. In 1877, she married the Rev. Frank Penny.
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Cold climate indicator species include Astarte borealis and Yoldia myalis from Baventian deposits at Covehithe. [22] Some species have distinct biostratigraphic value. The absence of Macoma balthica is considered to be an indicator distinguishing Norwich Crag molluscan assemblages from those of the later Wroxham Crag.