Walk 6 Chilbolton, Fullerton, Goodworth Clatford and Upper Clatford
Walk 7 Chilbolton Observatory and Chilbolton Common
Walk 8 Danebury Iron Age hill fort and Longstock
Walk 9 Stockbridge and Marsh Court
Walk 10 Stockbridge Down and Little Somborne
WALKS BETWEEN HOUGHTON AND TOTTON
Walk 11 Houghton and Broughton
Walk 12 Houghton, King’s Somborne and Horsebridge
Walk 13 Stonymarsh, Mottisfont, Kimbridge and Michelmersh
Walk 14 Lockerley, Mottisfont and Dunbridge
Walk 15 Romsey, Fishlake Meadows Nature Reserve and Greatbridge
Appendix A Route summary tables
Appendix B Itinerary planner
Appendix C Accommodation near the Test Way
Appendix D Useful contacts
Appendix E Further reading
Test Way direction post at Mottisfont (Stage 6, Walks 13 & 14)
INTRODUCTION
From Houghton Bridge (Walk 12)
For some, the magic of the River Test is all about fresh water fly-fishing but for others it is simply the lure of a sparkling river famously described as ‘gin clear’. The Test flows majestically the 40 miles (65km) from its source in the hamlet of Ashe near Overton in north Hampshire to the edge of Southampton Water. There is though, so much more to this land of vibrant green – its variety of landscape, gently sloping tree-clad hills, the occasional remnant of a former water meadow or chalk grassland – all set against a backdrop of a fascinating history and geology. Add to that the vast array of wildflowers, plants and wildlife inhabiting the various Sites of Special Scientific Interest (SSSI) – including Stockbridge Down, a haven for many species of butterfly – and it is not difficult to understand the attraction of a place that so completely defines pastoral England.
Chalk streams are a very rare breed among the various types of river that can be found on our planet. Such streams naturally occur in those areas where chalk is the main geological feature. Water seeps through the porous chalk to feed the springs that in turn give rise to rivers such as the Test. The pure water, rich in nutrients, also helps to maintain a plentiful supply of insects on which fish stocks rely (please refer to the section Geology and landscape). There are only about 200 chalk streams worldwide of which 160 are in England and the River Test − also an SSSI − is one of the finest examples.
Some of the area’s history is quite intriguing, notably the murderous story of the Saxon Queen Elfrida and the founding of Wherwell Abbey in the 10th century. The monument known as Deadman’s Plack in Harewood Forest is also a part of that story, albeit from the 19th century. There are an infinite variety of medieval churches with their own particular histories to share; St Mary’s Church in Broughton has the distinction of hosting one of only four ecclesiastical dovecotes that remain in England.
Nor is there any shortage of individual buildings of outstanding architectural quality as the 12th century Romsey Abbey, the resplendent Mottisfont Abbey (now owned by the National Trust) and the unique Whitchurch Silk Mill bear witness. There is also the dramatic impact of our forebears − the imposing Danebury Iron Age hill fort being one example. You can also discover the delights of the many charming villages brimming with flint and thatch and individual ‘hostelries’ to match.
Romsey Abbey (Stage 7/Walk 15)
The spate of canal construction that took place in the late 18th and early 19th centuries and the railway ‘mania’ that followed have also left their distinctive mark. At the ivy covered remains of the former Fullerton Junction station you can imagine that in the heyday of the Andover and Redbridge railway (generally known as the ‘Sprat and Winkle’) the scene then would have been very different from the sense of tranquillity that can now be enjoyed. Some of the old track bed also forms part of the Test Way (TW).
The TW begins in the North Wessex Downs Area of Outstanding Natural Beauty (AONB) in West Berkshire and then runs in parallel with the Wiltshire county boundary for a short distance before crossing into Hampshire at Combe Wood. It then continues through rolling chalk downland traversing Harewood Forest either side of Longparish – which is also where the TW first meets the River Test. From the hamlet of Fullerton at the half-way point, the route joins the old track bed of the former 'Sprat and Winkle' railway, becoming flat and fairly straight as it makes its way to Mottisfont. The penultimate stage to Romsey includes Squabb Wood and the final stage to Eling Wharf at Totton crosses the unique tidal estuary Lower Test Nature Reserve.
Last but not least, there are the 15 circular walks, which vary in length from 3.75 miles (6km) to 8.5 miles (13.75km). A few have uphill challenges (usually with rewarding views) but none are overly difficult, so when taken together with the individual stages of the TW, there is something for everyone. Ten of the walks also interweave with parts of the TW so it is possible in the course of those walks for you to achieve the best of both worlds!
Wherwell thatch (Walk 5)
Brief history of the Test Valley
Dating from the Neolithic period (4500–2200BC) there is evidence of farming activity in large parts of the Test Valley. There are relics from the Bronze Age (2200–750BC) including barrows or burial mounds, 14 of which are to be found at Stockbridge Down (Walk 10). During the Iron Age (750BC–AD43), a number of hill forts were constructed in and around the Test Valley including Danebury (Walk 8) and Woolbury Ring at the top of Stockbridge Down.
The Romans who invaded in AD43 and remained until the beginning of the fifth century have also left their imprint. There is a trace of a Roman road across Bransbury Common (Walk 4) and in Harewood Forest (Stage 4). The Anglo-Saxon period (AD450–1065) saw the development of a number of settlements, particularly Romsey (Stage 7 and Walk 15) as a prominent trading centre due to its location and ecclesiastical influence.
In medieval times the chalk downland areas were used intensively for rearing sheep – one of the most economically important activities during that period. The power inherent in the River Test spawned numerous water mills particularly around Whitchurch (Walk 2) where they were used in the production of cloth and at Laverstoke, especially in the making
