orders (especially at a later date the Cistercians) began to settle
after about the middle of the 7th century. At Medeshampstead
(i.e. Peterborough), Ely, Crowland, Ramsey, Thorney, Spalding,
Peakirk, Swineshead, Tattershall, Kirkstead, Bardney,
Sempringham, Bourne and numerous other places, they made
settlements and built churches, monasteries and abbeys. In
spite of the incursions of the predatory Northmen and Danes in
the 9th and 10th centuries, and of the disturbances consequent
upon the establishment of the Camp of Refuge by Hereward the
Wake in the fens of the Isle of Ely in the 11th century, these
scattered outposts continued to shed rays of civilization across
the lonely Fenland down to the dissolution of the monasteries in
the reign of Henry VIII. Then they, too, were partly overtaken
by the fate which befell the rest of the Fens; and it was only in
the end of the 18th and the beginning of the 19th century that the
complete drainage and reclamation of the Fen region was finally
effected. Attempts on a considerable scale were indeed made to
reclaim them in the 17th century, and the work as a whole forms
one of the most remarkable chapters of the industrial history of
England. Thus, the reclamation of the Witham Fens was taken
up by Sir Anthony Thomas, the earl of Lindsey, Sir William
Killigrew, King Charles I., and others in 1631 and succeeding
years; and that of the Deeping or Welland Fens in 1638 by Sir
W. Ayloff, Sir Anthony Thomas and other “adventurers,” after
one Thomas Lovell had ruined himself in a similar attempt in the
reign of Queen Elizabeth. The earl of Lindsey received 24,000
acres for his work. Charles I., declaring himself the “undertaker”
of the Holland Fen, claimed 8000 out of its 22,000 acres
as his share.
A larger work than these, however, was the drainage of the fens of the Nene and the Great Ouse, comprehending the wide tract known as the Bedford level. This district took name from the agreement of Francis, earl of Bedford, the principal landholder, and thirteen other adventurers, with Charles I. in 1634, to drain the level, on condition of receiving 95,000 acres of the reclaimed land. A partial attempt at drainage had been made (1478–1490) by John Morton, when bishop of Ely, who constructed Morton’s Leam, from Peterborough to the sea, to carry the waters of the Nene, but this also proved a failure. An act was passed, moreover, in 1602 for effecting its reclamation; and Lord Chief-Justice Popham (whose name is preserved in Popham’s Eau, S.E. of Wisbech) and a company of Londoners began the work in 1605; but the first effectual attempt was that of 1634. The work was largely directed by the Dutch engineer Cornelius Vermuyden, who had begun work in the Fens in 1621, and was knighted in 1628.
Three years after the agreement of the earl of Bedford and his partners with the king, after an outlay of £100,000 on the part of the company, the contract was annulled, on the fraudulent plea that the works were insufficient; and an offer was made by King Charles to undertake its completion on condition of receiving 57,000 acres in addition to the amount originally agreed on. This unjust attempt was frustrated by the breaking out of the civil war; and no further attempt at drainage was made until 1649, when the parliament reinstated the earl of Bedford’s successor in his father’s rights. After an additional outlay of £300,000, the adventurers received 95,000 acres of reclaimed land, according to the contract, which, however, fell far short of repaying the expense of the undertaking. In 1664 a royal charter was obtained to incorporate the company, which still exists, and carries on the concern under a governor, 6 bailiffs, 20 conservators, and a commonalty, each of whom must possess 100 acres of land in the level, and has a voice in the election of officers. The conservators must each possess not less than 280 acres, the governor and bailiffs each 400 acres. The original adventurers had allotments of land according to their interest of the original 95,000 acres; but Charles II., on granting the charter, took care to secure to the crown a lot of 12,000 acres out of the 95,000, which, however, is held under the directors, whereas the allotments are not held in common, though subject to the laws of the corporation. The level was divided in 1697 into three parts, called the North, Middle, and South Levels—the second being separated from the others by the Nene and Old Bedford rivers.
These attempts failed owing to the determined opposition of the native fenmen (“stilt-walkers”), whom the drainage and appropriation of the unenclosed fenlands would deprive of valuable and long-enjoyed rights of commonage, turbary (turf-cutting), fishing, fowling, &c. Oliver Cromwell is said to have put himself at their head and succeeded in stopping all the operations. When he became Protector, however, he sanctioned Vermuyden’s plans, and Scottish prisoners taken at Dunbar, and Dutch prisoners taken by Blake in his victory over Van Tromp, were employed as the workers. Vermuyden’s system, however, was exclusively Dutch; and while perfectly suited to Holland it did not meet all the necessities of East Anglia. He confined his attention almost exclusively to the inland draining and embankments, and did not provide sufficient outlet for the waters themselves into the sea.
Holland and other Fens on the west side of the Witham were finally drained in 1767, although not without much rioting and lawlessness; and a striking account of the wonderful improvements effected by a generation later is recorded in Arthur Young’s General View of the Agriculture of the County of Lincoln (London, 1799). The East, West and Wildmore Fens on the east side of the Witham were drained in 1801–1807 by John Rennie, who carried off the precipitation which fell on the higher grounds by catch-water drains, on the principle of the Roman Car Dyke, and improved the outfall of the river, so that it might the more easily discharge the Fen water which flowed or was pumped into it. The Welland or Deeping Fens were drained in 1794, 1801, 1824, 1837 and other years. Almost the only portion of the original wild Fens now remaining is Wicken Fen, which lies east of the river Cam and south-east of the Isle of Ely.
The Fen Rivers.—The preservation of the Fens depends in an intimate and essential manner upon the preservation of the rivers, and especially of their banks. The Witham, known originally as the Grant Avon, also called the Lindis by Leyland (Itinerary, vol. vii. p. 41), and in Jean Ingelow’s High Tide on the Lincolnshire Coast, is some 80 m. long, and drains an area of 1079 sq. m. It owes its present condition to engineering works carried out in the years 1762–1764, 1865, 1881, and especially in 1880–1884. In 1500 the river was dammed immediately above Boston by a large sluice, the effect of which was not only to hinder free navigation up to Lincoln (to which city sea-going vessels used to penetrate in the 14th and 15th centuries), but also to choke the channel below Boston with sedimentary matter. The sluice, or rather a new structure made in 1764–1766, remains; but the river below Boston has been materially improved (1880–1884), first by the construction of a new outfall, 3 m. in length, whereby the channel was not only straightened, but its current carried directly into deep water, without having to battle against the often shifting sandbanks of the Wash; and secondly, by the deepening and regulation of the river-bed up to Boston. The Welland, which is about 70 m. long, and drains an area of 760 sq. m., was made to assume its present shape and direction in 1620, 1638, 1650, 1794, and 1835 and following years. The most radical alteration took place in 1794, when a new outfall was made from the confluence of the Glen (30 m. long) to the Wash, a distance of nearly 3 m. The Nene, 90 m. long, and draining an area of some 1077 sq. m., was first regulated by Bishop Morton, and it was further improved in 1631, 1721, and especially, under plans by Rennie and Telford, in 1827–1830 and 1832. The work done from 1721 onward consisted in straightening the lower reaches of the stream and in directing and deepening the outfall. The Ouse (q.v.) or Great Ouse, the largest of the fenland rivers, seems to have been deflected, at some unknown period, from a former channel connecting via the Old Croft river with the Nene, into the Little Ouse below Littleport; and the courses of the two streams are now linked together by an elaborate network of artificial drains, the results of the great engineering works carried out in the Bedford Level in the 17th century. The old channel, starting from Earith, and known as the Old West river, carries only a small stream until, at a point above Ely, it joins the
