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The boundaries and rivers of the Vale of Belvoir
A coloured contours map showing the approximate boundaries of the Vale of Belvoir. It is a lowland area straddling Leicestershire and Nottinghamshire with Belvoir Castle in the south providing the eponymous landmark. The Vale comprises the valleys of two rivers – the Smite (from its source at Holwell) and Devon (which rises just south of Harston). The topography is typically undulating farmland and includes the settlements of Bingham, Bottesford and numerous villages (see Wikipedia for a list). The Vale stretches northwards from the ironstone escarpment – known to outsiders as the 'Belvoir Ridge' and to locals as the 'Harby Hills' – towards the River Trent but only as far as the Roman Fosse Way (A46) in the west and north-west. In the east the boundary is the watershed between the Devon and Witham; this interfluve also forms the Leicestershire-Lincolnshire boundary. About a month after I had written the previous paragraph I read Michael Honeybone's 1987 book called The Vale of Belvoir. I was pleased to see that he also regards the Fosse Way as the western boundary. He also suggests that the northern boundary was marked by Long Hedge Lane as this was the boundary of the Bingham Wapentake. This makes Flintham the most northerly parish in the Vale. However later in his book Honeybone quite rightly discusses Sibthorpe and Shelton as part of the Vale, contradicting his own boundary. The boundary of Bingham Wapentake almost certainly was created ex novo in AD 950 as Newark, the wapentake to the north, only begins to exist around this time. Before 950, extending back into the Iron Age or maybe earlier, the Vale would have been thought of as extending to the confluence of the Devon with the Trent. I'll be the first admit that villages closest to the Trent – Flintham, Elston, Sibthorpe, Cotham, Hawton, etc – have a topography that 'feels' much more like Trent valley settlements. The terrain is flat with none of the rolling hills which are characteristic of most of the Vale. But administrative units, while respecting watersheds, are bounded by distinctive landmarks not 'topographical feelings'. Prehistoric land units were part or all of a valley. The boundaries were at the top of the watersheds between the valleys. In this article I suggest that the Vale of Belvoir has a similar extent to an Iron Age and Roman estate centred on a probable villa between the modern parishes of Harby and Langar. I am well aware that estate agents do not realise that the Vale of Belvoir is defined by watersheds and the Fosse Way so describe properties in adjoining villages as being in the Vale to enhance their appeal and price. I understand their motives but can only agree to differ on the reality. The boundary between Leicestershire and Nottinghamshire does not follow the ironstone ridge. In this article I suggest why this happened, probably around AD 950 or soon after.
This map prepared by the English Place-Name Society in the 1940s shows the pre-1974 boundary between Leicestershire and Nottinghamshire, highlighted in green. And shows another clear linear boundary, highlighted in pink, where an equal number of parishes form a 'cleaner' demarkation, in part following the former Roman Road known as the Salters Way. While I cannot prove it most likely the pink boundary was the southern extent of the Vale of Belvoir (and Nottinghamshire) until AD 950 or thereabouts.
Origins of names of Smite and DevonDevon (pronounced 'dee-vun' or 'dee-ven' not 'dev-on') is probably from Brythonic *dubno- meaning 'deep' as its upper reaches form a deep ravine. This ravine also gives it name to 'Knipton', the farmstead (Old English tun) in a gnipa (Old Scandinavian word for 'narrow, steep-sided valley').The spelling 'Devon' was adopted in the sixteenth century. Previously it was referred to as the 'Dyvene' or 'Deven'. Yes, the River Devon is cognate with the county name 'Devon' which is derived from the name of a Celtic tribe, the Dumnonii, who inhabited the region during the Iron Age and Roman period. The name 'Dumnonii' seemingly also originates with *dubno-, so meant 'deep valley dwellers'. However the River Devon, flowing through Perthshire, Kinross-shire, and Clackmannanshire, has a different origin.
Holwell Mouth, the source of the Smite, photographed in 1989. Note the rusty colour of the stream bed.
Barrie Cox in his survey of Leicestershire place-names considers that Smite is probably from Old English smitan 'to slide, to slip, to glide'. 'Smite' evolves into the Modern English word meaning 'to strike'. The River Smite near Orston does indeed seem to be a slow-moving watercourse. However a small weir under the bridge on Smite Lane reveals that the flow is much greater than the 'gliding' appearance of the water suggests. Although unique as a river name in Nottinghamshire and Leicestershire, 'smite' is quite a common stream-name elsewhere, and gives its name to the villages of Upper and Lower Smite in Warwickshire. The Smite south of Whatton was crossed by Cokerbek Brigge, revealing an earlier name for the Smite because 'coker' might be from the Brythonic word kukro meaning 'crooked' or 'winding' with Old Scandinavian 'beck' meaning 'stream'. Before the course of the Smite was straightened near settlements such as Whatton and Orston the watercourse was indeed decidedly crooked as the relict watercourses are shown on 1880s OS maps for Orston and Whatton. There is a different Cocker Beck draining into the River Trent at Gunthorpe. The 1940s English Place-Name Society map reproduced earlier on this page shows the name 'R. Devon' in Orston parish. In recent centuries this watercourse has been known as the Smite. I'm not aware of any early documents calling the Smite the Devon. Best guess is that the EPNS cartographer slipped up (the Second World War had just started when he was working on this map, so give him some slack).
For what it's worth, an oral tradition in central Wiltshire holds that drainage ditches and such like were dug by Napoleonic prisoners of war (Alan Latham pers. com. circa 2010). So latest 1815. Or was this something local landowners funded to provide work for farm labourers when there was insufficient labour required on the farms in the lean years of the 1830s and 1840s? Note that the current watercourse of the Smite was modified by Severn Trent during the 1970s or 1980s e.g. by deeping and creating/renewing small weirs. The Smite has a tributary, the River Whippling, which rises south-east of Elton and joins the Smite north-east of Whatton. The origins of the name 'Whippling' have not been ascertained. It certainly does not flow in a whip-like manner. The confluence of the Devon and Smite is near Shelton. Curiously the combined flow is called the Devon even though the Smite is the longer and wider river with the greater catchment area. The Devon flows into the Trent at Farnham – there is now a marina on the opposite bank. Probably no coincidence that the Roman Fosse Way crosses the Devon at this confluence as the gently-sloping banks of the Devon would have made an excellent place to unload flat-bottomed boats whereas the greater flow of the Trent would have needed timber hythes or wharves to be constructed.
Newark on Devon?
It has been suggested (though I don't know the origin) that in Roman times the River Trent did not branch into two upstream of Averham, so there was no watercourse between 'A' and 'B' until more recent centuries. Instead the River Devon ran all the way to the north of what is now Newark (marked 'C'). Most probably a major flood during the middle Anglo-Saxon era (when the weather was wetter than now) created the channel from 'A' to 'B'.
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