A Month in Yorkshire. Walter White
and Drayton—Fluvial Parliament—Hull—The Thieves’ Litany—Docks and Drainage—More Dutch Phenomena—The High Church—Thousands of Piles—The Citadel—The Cemetery—A Countryman’s Voyage to China—An Aid to Macadam.
As the Vivid steamed past the Spurn lighthouse, I looked curiously at the low sandy spit on which the tall red tower stands, scarcely as it seems above the level of the water, thinking that my first walk would perhaps lead thither. At sight of the Pharos, and of the broad estuary alive with vessels standing in, the Yorkshiremen on board felt their patriotism revive, and one might have fancied there was a richer twang in their speech than had been perceptible in the latitude of London. A few who rubbed their hands and tried to look hearty, vowed that their future travels should not be on the sea. The Vivid is not a very sprightly boat, but enjoys or not, as the case may be, a reputation for safety, and for sleeping-cabins narrower and more stifling than any I ever crept into. But one must not expect too much when the charge for a voyage of twenty-six hours is only six and sixpence in the chief cabin.
Not without reason does old Camden remark of the Humber, “it is a common rendezvous for the greatest part of the rivers hereabouts,” for it is a noble estuary, notwithstanding that water and shore are alike muddy. It is nearly forty miles long, with a width of more than two miles down to about three leagues from the lighthouse, where it widens to six or seven miles, offering a capacious entrance to the sea. The water has somewhat of an unctuous appearance, as if overcharged with contributions of the very fattest alluvium from all parts of Yorkshire. The results may be seen on the right, as we ascend. There spreads the broad level of Sunk Island, a noteworthy example of dry land produced by the co-operation of natural causes and human industry. The date of its first appearance above the water is not accurately known; but in the reign of Charles II. it was described as three thousand five hundred acres of “drowned ground,” of which seven acres were enclosed by embankments; and was let at five pounds a year. A hundred years later fifteen hundred acres were under cultivation, producing a yearly rental of seven hundred pounds to the lessee; but he, it is said, made but little profit, because of the waste and loss occasioned by failure of the banks and irruptions of the tides. In 1802 the island reverted to the Crown, and was re-let on condition that all the salt marsh—nearly three thousand acres—which was “ripe for embankment,” should be taken in, and that a church and proper houses should be built, to replace the little chapel and five cottages which ministered as little to the edification as to the comfort of the occupants. In 1833 the lease once more fell in, and the Woods and Forests, wisely ignoring the middlemen, let the lands directly to the ‘Sunk farmers,’ as they are called in the neighbourhood, and took upon themselves the construction and maintenance of the banks. A good road was made, and bridges were built to connect the Island with the main, and as the accumulations of alluvium still went on, another ‘intake’ became possible in 1851, and now there are nearly 7000 acres, comprising twenty-three farms, besides a few small holdings, worth more than 12,000l. of annual rent. It forms a parish of itself, and not a neglected one; for moral reclamation is cared for as well as territorial. The clergyman has a sufficient stipend; the parishioners supplemented the grants made by Government and the Council of Education, and have now a good schoolhouse and a competent schoolmaster.
The Island will continue to increase in extent and value as long as the same causes continue to operate; and who shall set limits to them? Already the area is greater than that described in the last report of the Woods and Forests, which comprehends only the portion protected by banks. The land when reclaimed is singularly fertile, and free from stones, and proves its quality in the course of three or four years, by producing spontaneously a rich crop of white clover. Another fact, interesting to naturalists, was mentioned by Mr. Oldham in a report read before the British Association, at their meeting in Hull. “When the land, or rather mud-bank, has nearly reached the usual surface elevation, the first vegetable life it exhibits is that of samphire, then of a very thin wiry grass, and after this some other varieties of marine grass; and when the surface is thus covered with vegetation, the land may at once be embanked; but if it is enclosed from the tide before it obtains a green carpet, it may be for twenty years of but little value to agriculture, for scarcely anything will grow upon it.”
This is not the only place on the eastern coast where we may see artificial land, and banks, dikes, and other defences against the water such as are commonly supposed to be peculiar to the Netherlands.
The windows of Cleathorpes twinkling afar in the morning sun, reveal the situation of a watering-place on the opposite shore much frequented by Lincolnshire folk. Beyond rises the tall and graceful tower of Grimsby Docks, serving at once as signal tower and reservoir of the water-power by which the cranes and other apparatus are worked, and ships laden and unladen with marvellous celerity. These docks cover a hundred acres of what a few years ago was a great mud-flat, and are a favourable specimen of what can be accomplished by the overhasty enterprise of the present day. Grimsby on her side of the river now rivals Hull on the other, with the advantage of being nearer the sea, whereby some miles of navigation are avoided.
Turning to the right again we pass Foul Holme Sand, a long narrow spit, covered at half-tide, which some day may become reclaimable. A little farther and there is the church of Paghill or Paul, standing on a low hill so completely isolated from the broken village to which it belongs, that the distich runs:
“High Paul, and Low Paul, Paul, and Paul Holme,
There was never a fair maid married in Paul town.”
The vessel urges her way onwards across swirls and eddies innumerable which betray the presence of shoals and the vigorous strife of opposing currents. The spring tides rise twenty-two feet, and rush in with a stream at five miles an hour, noisy and at times dangerous, churning the mud and shifting it from one place to another, to the provocation of pilots. It is mostly above Hull that the changes take place, and there they are so sudden and rapid that a pilot may find the channel by which he had descended shifted to another part of the river on his return a few days afterwards. There also islands appear and disappear in a manner truly surprising, and in the alternate loss or gain of the shores may be witnessed the most capricious of phenomena. Let one example suffice: a field of fourteen acres, above Ferriby, was reduced to less than four acres in twenty years, although the farmer during that time had constructed seven new banks for the defence of his land.
Some notion of the enormous quantity of mud which enters the great river may be formed from the fact that fifty thousand tons of mud have been dredged in one year from the docks and basins at Hull. The steam-dredge employed in the work lifts fifty tons of mud in an hour, pours it into lighters, which when laden drop down with the tide, and discharge their slimy burden in certain parts of the stream, where, as is said, it cannot accumulate.
Stukely, who crossed the estuary during one of his itineraries, remarks: “Well may the Humber take its name from the noise it makes. My landlord, who is a sailor, says in a high wind ’tis incredibly great and terrible, like the crash and dashing together of ships.” The learned antiquary alludes probably to the bore, or ager as it is called, which rushes up the stream with so loud a hum that the popular mind seeks no other derivation for Humber. Professor Phillips, in his admirable book on Yorkshire, cites the Gaelic word Comar, a confluence of two or more waters, as the origin; and Dr. Latham suggests that Humber may be the modified form of Aber or Inver. Drayton, in Polyolbion, chants of a tragical derivation; and as I take it for granted, amicable reader, that you do not wish to travel in a hurry, we will pause for a few minutes to listen to the debate of the rivers, wherein “thus mighty Humber speaks:”
“My brave West Riding brooks, your king you need not scorn,
Proud Naiades neither ye, North Riders that are born,
My yellow-sanded Your, and thou my sister Swale
That dancing come to Ouse, thro’ many a dainty dale,
Do greatly me enrich, clear Derwent driving down
From Cleveland; and thou Hull, that highly dost renown,
Th’ East Riding by thy rise, do homage to your king,
And let the sea-nymphs thus of mighty Humber sing;
That full an hundred