21) In the early 18th century there was an alternative road from Old Stratford through Passenham and Wicken, which followed a course closer to the river, thus avoiding Deanshanger. (fn. 22) Although described in 1747 as the best known way and the general highway by which most waggons and travellers went from Old Stratford to Buckingham, (fn. 23) it had disappeared by 1779 (fn. 24) and was probably stopped up when the common fields of Wicken through which it ran were inclosed in 1757. (fn. 25) In the early 18th century two by-roads ran north from these main roads to Wicken village, from where other lanes continued north towards Whittlebury. The main east-west route through the village linked Wicken with Deanshanger and Leckhampstead. (fn. 26) By the early 19th century parts of the north-south route to the south of the village had disappeared or declined into footpaths, leaving the roads from Deanshanger, Whittlebury and Leckhampstead as the main links between Wicken and its neighbours. (fn. 27)
The Buckingham branch of the Grand Junction Canal passed through the southern part of the parish on its way from Old Stratford to Buckingham. Originally projected in 1793 as a scheme to canalise the Ouse from Buckingham to Passenham, from where a short artificial cut would continue to the sidecut aleady agreed on from the main line of the Grand Junction at Cosgrove to a wharf near Watling Street at Old Stratford, (fn. 28) the branch was finally built as a deadwater canal throughout. Digging at Wicken began in October 1800 and the first boat passed from Old Stratford to Buckingham on 7 May 1801. (fn. 29) In July that year Mrs. Prowse of Wicken Park took two of her nieces on a trip on the canal through her estate, and in August she watched the canal company committee pass by on their way from Paddington to Buckingham. (fn. 30) The nearest public wharfs serving Wicken were at Deanshanger, about a mile away. (fn. 31) The branch fell into disuse in the early 20th century and was largely filled in, although in the 1990s a Buckingham Arm Canal Society was established to press for its rebuilding.
LANDCSAPE AND SETTLEMENT
The Impact of Whittlewod.
The pattern of settlement and land usage in Wicken has been considerably influenced by the position of the parish at the southern edge of Whittlewood Forest. Although in 1289 a proposal to reinclose the park at Wick Hamon was investigated by a swainmote court presided over by John de Tingewick, keeper of Whittlewood, implying that the township then lay within the forest, (fn. 32) the detailed perambulation made ten years later, which established the boundary of the forest until the 17th century, clearly places both Wick Hamon and Wick Dive outside Whittlewood. (fn. 33) In 1639, as part of Charles I's attempts to enlarge the forest far beyond the traditional limits, Henry Lord Spencer, the rector and two freeholders were fined for a grant of disafforestation relating to 1,800 a. of land in Wicken and Leckhampstead, and 100 a. of wood in the latter parish. (fn. 34) In reality, as an early 17th-century map of Whittlewood makes clear, no part of either parish was properly within the forest, whose south-western boundary at that date, as in 1299, was marked by Kings Brook. (fn. 35)
A good deal of woodland survived at the northern end of Wicken in the early 17th century, extending over the border into Leckhampstead, most of which was still in existence a century later. (fn. 36) By the early 19th century Wicken Wood had been slightly further reduced in size, although there were still 236 a. of woodland in the parish as a whole, including several parcels to the south-west of the village, detached from the main area further north. Even as late as this, Sir Charles Mordaunt, the owner of the Wicken Park estate, successfully claimed an 18 ft. freeboard along much of the parish boundary with Leckhampstead (including some stretches that were no longer wooded on the Wicken side as well as those that were). (fn. 37) The claim was also accepted by the Ordnance Survey in the 1880s, which accounts for the unusual me