Болингброк: Англияның Линкольншир ауылының тарихы

Village in Lincolnshire, England

Bolingbroke, now called Old Bolingbroke, is a village and civil parish in the East Lindsey district of Lincolnshire, England. Its present boundaries were formed by the amalgamation of the Parishes of Bolingbroke and Hareby in 1739. The population at the 2011 census was 325. Bolingbroke is 3 mile (5 km) west of Spilsby. The village of New Bolingbroke is 6 mile (10 km) to the south west. The Prime Meridian passes through the parish to the west of Old Bolingbroke.

Bolingbroke appears in the Domesday Book of 1086 as "Bolingborc", one of 38 places associated with Stori of Bolingbroke at the time of the Norman conquest. This suggests an Anglo Saxon etymological origin, possibly "Bolingburh" or similar (burh of Bolla's people). William de Roumare, Earl of Lincoln (born circa 1096), may have built Bolingbroke Castle in the 12th century as a motte and bailey castle with wet ditch, to replace an earlier earthwork defence structure which overlooked the village on Dewy Hill. In the early 13th century, a new castle was constructed at the present site by Ranulph de Blondeville, 4th Earl of Chester following his return in 1220 from the 5th Crusade. Later John of Gaunt, the son of Edward III, acquired the castle through his wife, Blanche of Lancaster. In 1367 it was the birthplace of John's son, Henry, known as Henry Bolingbroke, who became King Henry IV of England. The parish church of Old Bolingbroke was rebuilt by Alice de Lacy and John of Gaunt. It was significantly damaged during the siege of the castle in 1643 during the Civil War when the Royalists used the castle to garrison troops prior to the Battle of Winceby (11 October 1643). Only the South Aisle of the 14th century Church remains. A new North Aisle was added during significant renovations by John Fowler in 1889. The last remaining castle structure fell down in 1815. The site became a grassy hillock, which archeologists excavated in the 1970s.

The village sits in a broad valley of the Lincolnshire Wolds, between two streams, that rise in the surrounding hills. These eventually become what is known to the south as Hagnaby Beck. The village is at about 25m above sea level. Only the Lower one is in the parish, the upper one is adjacent to the boundary. The high portions of the parish are composed of the Spilsby Sandstone, which overlays here the deeper Kimmeridge and Ampthill mudstones. Eroded by the streams in the Dales, the Sandstones are removed, exposing in part the mudstone layer, although in general these are covered in the village and the river valley to the south west by the Quaternary post glacial sands and gravels of the Bain Valley formation. The parish boundary is complex, but can be summarised as surrounding the village, which is broadly central, and enclosing the rising ground in all directions. It generally does not include the plateau above the village. No major roads cross the parish, but the village is joined by minor roads to many surrounding settlements. The Prime (Greenwich) Meridian runs through the Parish just west of the village. There are, and were, no railway connections, the nearest stations being historically Spilsby, and now Thorpe Culvert. The Parish Council own and maintain the King George V Playing Field and Ramsden Village Hall, the latter named for John and Eleanor Ramsden who bequeathed the land used for both to the village in 1937. The mobile library visits for an hour a month. The ecclesiastical parish of Old Bolingbroke is part of the Spilsby, Marden Hill, Stickney and Partney Group Parishes of the Deanery of Bolingbroke. The parish church is dedicated to Saint Peter and Saint Paul. There is a second church in the parish in Hareby, also named Saint Peter and Saint Paul. The village's Methodist Chapel in Chapel Lane was built in 1845. It is part of the Mid Lincolnshire Circuit. The congregation became an eco congregation in 2007.