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The Lincolnshire Wolds which also includes the Lincolnshire Wolds National Landscape are a range of low hills in the county of Lincolnshire, England which runs roughly parallel with the North Sea coast, from the Humber Estuary just west of the town of Barton-upon-Humber in North Lincolnshire down in a south easterly direction towards the flat Lincolnshire Fens in the south-east of the county ...
The route begins at Candlesby and runs 14 miles (23 km) northbound to Caistor, following closely an ancient ridge trail across the spine of the wold. It climbs to a height of 98 metres (320 feet) above sea level near Tetford, and, on a fine day, provides a view of the hamlets, fields, hills and landmarks of the area, such as Lincoln Cathedral, Boston Stump and the North Sea.
Tetford is in the Lincolnshire Wolds, a designated Area of Outstanding Natural Beauty, running from Louth in the north, to Horncastle in the south. The village is 6.5 miles (10.5 km) north-east from Horncastle, 10 miles (16 km) south from Louth and 8 miles (13 km) north-west from Spilsby.
Wolds Top, also known as Normanby Hill, [2] is the highest point of the Lincolnshire Wolds. The summit elevation is 168 m (551 ft). [ 1 ] It lies just under a mile to the north of the village of Normanby le Wold and three miles to the south of the small market town of Caistor in Lincolnshire .
The Wolds comprise a series of low hills and steep valleys that are in the main underlain by calcareous (chalk and limestone) and sandstone rock laid down in the Cretaceous and Jurassic periods. One exception to this is the North Leicestershire / South Nottinghamshire Wolds, which are underlain by sometimes chalky glacial till ('Oadby Till').
South Willingham is a village and civil parish in the East Lindsey district of Lincolnshire, England, and partly within the Lincolnshire Wolds Area of Outstanding Natural Beauty, . It is situated 1 mile (2 km) south of the A157 Lincoln to Louth road, 15 miles (24 km) west of Lincoln, where the central Lincolnshire Vale and the Lincolnshire ...
Every Dec. 6, kids around Wisconsin look forward to receiving treats and gifts from St. Nicholas. Here's where the tradition comes from.
Hubbard's Hills is a glacial overspill channel formed as the last ice age ended about 40,000 years ago. A marginal lake of meltwater trapped between glacial ice sheet and the Lincolnshire Wolds poured over a chalk ridge and gouged a 125-foot-deep (38 m), steep-sided valley.
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