iously separate parishes, Wick (or Wyke) Dive and Wick Hamon, which were already distinct estates in 1066. (fn. 5) The union has been commemorated annually ever since by a special service, with cakes and ale, in the village on the Thursday in Holy week. (fn. 6) The boundary between Wick Dive and Wick Hamon is apparently marked by the stream which flows from west to east through the village of Wicken to join Kings Brook at Deanshanger. (fn. 7) Wick Hamon lay to the south of this brook, Wick Dive to the north, and each parish had its own church in its respective portion of Wicken village. (fn. 8) The regular outer boundary of the modern parish, as well as the common first element of the two medieval parish names, (fn. 9) suggests that at some date before the Norman Conquest the whole area had formed a single estate that was later partitioned. The only boundary change since 1587 occurred in 1956. (fn. 10)
The south-eastern corner of the parish lies about 250 ft. above sea level. From the river valley the land rises gently to reach about 360 ft. at the north-west corner, about three miles away. The parish is roughly a mile and a half wide on its other axis, although it narrows to a point in the north-west. Large areas of alluvium occupy the flood plain of the Ouse and the higher land to the south of the village and in the west is covered Boulder Clay. In the valley formed by the small stream which runs through the centre of the parish broad patches of Oolitic Limestone are exposed. (fn. 11) Baker described the soil as a cold white clay, or in some parts a brown stone brash loam, overlying limestone. (fn. 12) An earlier writer commented on the excellence of the water supply and the availability of building stone, gravel and sand, as well as 'a good vein of marble'. (fn. 13)
In 1301 40 households were assessed to the lay subsidy in the vill of Wick Dive; there is no entry on the roll for Wick Hamon, (fn. 14) which may be included in this total. In the 1520s the two townships together contained about 35 households asses