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The Parish of Stevington in General

View from West End looking east December 2009
View from West End looking east December 2009


Volume III of The Victoria County History for Bedfordshire was published in 1912. At that date the parish of Stevington contained 1,820 acres of which roughly a third was arable and most of the rest grassland. The main crops were wheat, beans, barley, oats and clover.

The ground mainly slopes south-west to north-east, the highest point, 303 feet above sea-level being in the west of the parish and the lowest, just over a hundred feet in the east near the River Great Ouse. The church stands at about 140 feet above sea-level and the windmill at about 180 feet. Hart Farm barns stand at nearly 200 feet.

The geology is complex. The solid, or underlying, geology consits of four different types of rock, all laid down in the warm, shallow seas of the Jurassic Period. the four types are as follows:

  • Great Oolite Group - an interbedded formation of limestone with clay minerals known as argillaceous because of their silvery appearance. This was laid down between 164 and 169 million years ago. This underlies the river and its immediate surroundings as far as the church.
  • a mixed sandstone and mudstone called Kelleways Formation. This was deposited between 159 and 164 million years ago. This underlies the area east of the village, Court Lane around Ashford Lodge and Silver Street beneath the farthest houses from the cross. It also underlies part of the west of West End;
  • a limestone called Cornbrash Formation. This was laid down between 159 and 169 million years ago. This lies beneath the crossroads of Park Road with Court Lane, and forms a U-shape relative to the village. It crosses Court Lane just south of Ashford Lodge and crosses Park Road just east of Farley Way - it underlies most of the northern part of Silver Street; it also underlies part of the west of West End;
  • a mudstone called Oxford Clay Formation. This was laid down between 154 and 164 million years ago. This underlies the eastern part of West End.

Superficial geology is the material laying above the solid geology. It was all deposited within the last two million years. Along the river is an alluvium of sand, gravel, clay and silt and in the eastern part of West End is a glacial till. Otherwise the soil reflects the nature of the solid geology below, sand or clay.

 Stevington sign December 2009
Stevington sign December 2009


The name of Stevington means "Styfa's people's farm", Styfa being an Anglo-Saxon personal name. The name has had a few variations over the centuries, as seen below:

  • Stiuentone: 1086-1316;
  • Styuenton: 1086-1316;
  • Stiuiton: 1196l
  • Stiuinton: 1227-1282;
  • Stiuington: 1247-1287;
  • Stiuingdon: 1276;
  • Steventon: 1284-1392;
  • Stevintone: 1302-1346;
  • Stevyntone: 1302-1346;
  • Stevyngton: 1315-1515;
  • Styvyngton: 1349-1350;
  • Stephynton: 1521

 The Village Cross December 2008
The Village Cross December 2008

Administrative History

Stevington is an ancient parish in the Willey Hundred. It underwent a small boundary change in 1948 [CDP58] when a small portion of it was transferred to Turvey. Stevington is bounded by Pavenham to the north, Oakley to the north-east, Bromham to the south-east, Turvey to the west and Carlton and Chellington to the north-west.

 Stevington about 1900 [Z1306/112]
Stevington about 1900 [Z1306/112]


The population of Stevington has been fairly consistent in the last two hundred years. However, they do show the pattern fairly typical of most Bedfordshire rural parishes - rising to a peak in 1871 then declining as people left the countryside to migrate to towns as agricultural mechanisation cut the number of jobs available. From a low in 1961 figures have been rising as new housing has been built:

  • 1801: 415;
  • 1811: 436;
  • 1821: 485;
  • 1831: 500;
  • 1841: 602;
  • 1851: 586;
  • 1861: 606;
  • 1871: 735;
  • 1881: 624;
  • 1891: 601;
  • 1901: 536;
  • 1911: 479;
  • 1921: 467;
  • 1931: 479;
  • 1951: 409;
  • 1961: 386;
  • 1971: 589;
  • 1981: 604;
  • 1991: 555;
  • 2001: 581;
  • 2011: 552.