Lincolnshire Wolds

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The Lincolnshire Wolds are a range of low hills in Lincolnshire, England. The hills run roughly parallel with the North Sea coast, from the Humber Estuary just west of the town of Barton-upon-Humber in North Lincolnshire, towards the flat Lincolnshire Fens in the south-east of the county as far south as the East Lindsey village of East Keal.<ref name=NCA43>Template:Cite web</ref> The Wolds form the highest land in eastern England between Yorkshire and Kent.<ref name=OS>Ordnance Survey maps:
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Natural England define a Lincolnshire Wolds National Character Area covering an area of Template:Convert.<ref name=NCA43/> Within this, an area of Template:Convert is designated as the Lincolnshire Wolds National Landscape, an Area of Outstanding Natural Beauty.

Geology

The Wolds are formed largely from a series of pure marine limestones formed during the Cretaceous period, known collectively as the Chalk Group. The chalk overlies a series of other sedimentary strata of late Jurassic/early Cretaceous age. The strata dip gently to the east and form a scarp which runs southeast from Barton upon Humber via Caistor before it loses its identity north of Spilsby. To the north of the Humber Gap, the same formations continue as the Yorkshire Wolds.<ref name=NCA43/> The rock succession in stratigraphic order i.e. youngest/uppermost first, is this:

  • White Chalk Subgroup
    • Burnham Chalk formation
    • Welton Chalk Formation
  • Grey Chalk Subgroup
    • Ferriby Chalk Formation
    • Hunstanton Chalk Formation

The thin Hunstanton Chalk and the Ferriby Chalk formations form much of the west facing Wolds scarp but it is the overlying Welton Chalk Formation which forms the greater part of the easterly dip-slopes with the Ferriby Chalk extensively exposed within the dry dip-slope valleys. The Burnham Chalk Formation forms an indistinct secondary scarp to the east of the main scarp between Barton and Louth. In the north between South Ferriby and Grasby, the lower part of the scarp is formed from the Kimmeridge Clay Formation. A series of other rock layers intervene from the Caistor area southwards, uppermost of which are the green-brown Carstones:

Lower/early Cretaceous

  • Carstone Formation (sandstone)
  • Roach Formation (interbedded mudstone and limestone) (present from Stenigot southwards)
  • Tealby Formation (mudstone - but including the 'Tealby Limestone Member')
  • Claxby Ironstone Formation

Upper/late Jurassic

The numerous dry valleys cut into the dip-slope are typically floored by head, locally derived clay, silt, sand and gravel. The western valleys were created during recent glacial periods through the action of water over frozen ground whilst many in the east represent subglacial drainage.<ref>Template:Cite web</ref> During the last ice age (Devensian), ice encroached upon the Wolds from the northeast and entered the Humber gap from the east but did not cover the Wolds, hence there is no Devensian age glacial till on these hills. However, an earlier ice age left extensive spreads of till across the central and southern areas.<ref>Template:Cite book</ref> Sections of the main scarp, notably at Saxby All Saints and between Nettleton and Walesby have been subject to landslip.<ref>Template:Cite web</ref>

Geography

The Wolds comprise a series of low hills incised by characteristic dry open valleys.

File:Lincolnshire Wolds.jpg
View from Red Hill in August

The Lincolnshire Wolds can be divided into four distinct areas:<ref name=NCA43/>

  1. the main area of chalk hills in the north,
  2. the north west scarp,
  3. an area of ridges and valleys in the south west,
  4. the claylands in the south east.

The Red Hill nature reserve near the village of Goulceby is notable for the unusual red colour of its soil and underlying chalk.

Wolds Top is the highest point in the whole of Lincolnshire and is marked by a trig point just north of the village of Normanby le Wold, at approximately Template:Convert above sea level (Template:Gbm4ibx).<ref name=OS/>

Other hills include:

The Wolds provide views across the flat Fens and salt marshes of Lindsey and Holland: it is possible, from various points on the Wolds, to see all of the larger structures in the north and east of the county: the Belmont mast, Boston Stump, Grimsby Dock Tower, the Humber Bridge, Lincoln Cathedral, St James' Church in Louth (known locally as the 'Cathedral of the Wolds', though it holds only parish church status), the radar station near Normanby, Tattershall Castle and the wind turbines on the coast near Mablethorpe.

Waterways

Name Length Source Source Elevation (m) Mouth Mouth Elevation (m) Notes
River Bain Ludford 130 River Witham, Dogdyke 2 Partly concurrent with the Horncastle Canal south of Horncastle.
Great Eau North Sea, Saltfleet Haven 0
River Lud North Sea, North Coates 0 Also known as the Louth Navigation due to its canalisation.
River Lymn Belchford 91 North Sea, Gibraltar Point 0
River Rase Tealby 118 River Ancholme, Bishopbridge 6
River Waring Belchford 100 River Bain, Horncastle 28

National Landscape

The Lincolnshire Wolds were designated an Area of Outstanding Natural Beauty (AONB) in 1973, and adopted the "National Landscape" branding in 2023.<ref>Template:Cite web</ref> The Wolds AONB covers 560 square kilometres,<ref>Template:Cite web</ref> and is managed by the Lincolnshire Wolds Countryside Service.<ref>Template:Cite web</ref>

The Wolds AONB cuts across the council boundaries of Lincolnshire County Council, East Lindsey District Council, West Lindsey District Council and North East Lincolnshire Council.<ref name=OS/><ref name=NCA43/> The boundaries of the AONB are marked by tourist signs incorporating stylized hills and trees, placed on roads leading into the area.

People and places

The Wolds are sparsely populated and have a rural character. They are 'ringed' by several small market towns that lie around their edge:<ref name=OS/>

Many of the place-names in the Wolds indicate a strong Viking influence in the area's history. There is also an abundance of mediaeval 'lost villages' – settlements abandoned due to changes in land use, soil exhaustion and disease.

Several notable roads and paths run over the Wolds. Caistor High Street, the path of a Roman road and now the route of the B1225, runs from Caistor to Baumber near Horncastle. The ancient Bluestone Heath Road follows the course of an ancient drove road from west to east across the Wolds, and several "A" roads also run through the AONB.<ref name=OS/>

The Wolds are now promoted as a tourist destination: the area's connection with Tennyson (who was born in Somersby) is being exploited,<ref>Template:Cite web</ref><ref>Template:Cite web</ref> and farmers are being encouraged to diversify into the tourism industry. The roads of the Wolds are particularly popular with motorcyclists, and the area is home to Cadwell Park, one of the UK's top race circuits.<ref>Template:Cite web</ref><ref>Template:Cite web</ref>

The area is also popular with walkers: the Viking Way long-distance footpath runs from Barton-upon-Humber in North Lincolnshire across the Lincolnshire Wolds and into Rutland,<ref>Template:Cite web</ref><ref>Template:Cite web</ref> and there is a youth hostel in the middle of the Wolds at Woody's Top near the village of Tetford.<ref>Template:Cite web</ref><ref>Template:Cite web</ref>

References

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