Lincolnshire: History
During pre-Roman times, most of Lincolnshire was inhabited by the Corieltauvi people. The language of the area at that time would have been Common Brittonic, the precursor to modern Welsh, Cornish and Breton. The name Lincoln was derived from Lindum Colonia.
Large numbers of Germanic speakers from continental Europe settled in the region following the withdrawal of the Romans. Though these were later identified as Angles, it is unlikely that they migrated as part of an organised tribal group. Thus, the main language of the region quickly became Old English. However, it is possible that Brittonic continued to be spoken in some communities as late as the eighth century.
Modern-day Lincolnshire is derived from the merging of the territory of the Kingdom of Lindsey with that controlled by the Danelaw borough of Stamford. For some time the entire county was called "Lindsey", and it is recorded as such in the 11th-century Domesday Book. Later, the name Lindsey was applied to the northern core, around Lincoln. This emerged as one of the three Parts of Lincolnshire, along with the Parts of Holland in the south-east, and the Parts of Kesteven in the south-west, which each had separate quarter sessions as their county administrations. Lindsey was traditionally split between the North, South and West Ridings of Lindsey.
The area was shaken by 27 February 2008 Lincolnshire earthquake, reaching between 4.7 and 5.3 on the Richter magnitude scale; it was one of the largest earthquakes to affect Britain in recent years.
Lincolnshire is home to Woolsthorpe Manor, birthplace and home of Sir Isaac Newton. He attended The King's School, Grantham. Its library has preserved his signature, carved into a window sill when he was a youth.
The geographical layout of Lincolnshire is quite extensive and mostly separated by many rivers and rolling countryside. The north of the county begins from where the Isle of Axholme is located near the meeting points of the rivers Ouse and Trent near to the Humber. From there, the southside of the Humber estuary forms the border between Lincolnshire and the East Riding of Yorkshire. From there, the south bank of the Humber Estuary where the Humber Bridge crosses the estuary at Barton upon Humber, is used primarily for the shipping ports at Immingham, New Holland and Grimsby. From there, the rest of the southern bank forms the Lincolnshire Coast from Cleethorpes to Mablethorpe and then onto Skegness. From Skegness, the rest of the Lincolnshire Coastline forms the sea boundary and border with Norfolk at the Wash. The coast then at Boston becomes the meeting point of the rivers Welland and Haven in an area known as the "Fosdyke Wash".
The rest of the sea boundary runs from Fosdyke to the east of Sutton Bridge, where the current land boundary with Norfolk is located in a narrow area of reclaimed farmland just to the east of the River Nene, but until as recently as the early 19th century there was no land border between Lincolnshire and Norfolk as it was separated from each other by the "Cross Keys Wash" a former area of estuary and marshland where the River Nene used to flow out into the Wash and could only be crossed at low tide by a causeway or ferry and was the natural boundary between the two counties. …