Nowhere that I have been to in the world does the land fade into the sea so inconspicuously.
The coasts of western England are like the death of a western man in battle—violent and heroic. The land dares all, and plunges into a noisy sea. This coast of Eastern England is like the death of one of these eastern merchants here—lethargic, ill-contented, drugged with ease. The dry land slips, and wallows into a quiet, very shallow water, confused with a yellow thickness and brackish with the weight of inland water behind.
I have heard of the great lakes, especially of the marshes at the mouth of the Volga, in the Caspian, where the two elements are for miles indistinguishable, and where no one can speak of a shore; but here the thing is more marvellous, because it is the true sea. You have, I say, the true sea, with great tides, and bearing ships, and seaports to which the ships can go; and on the other side you have, inhabited, an ancient land. There should be a demarcation between them, a tide mark or limit. There is nothing. You cannot say where one begins and the other ends. One does not understand the Fens until one has seen that shore.
The sand and the mud commingle. The mud takes on little tufts of salt grass barely growing under the harsh wind. The marsh is cut and wasted into little islands covered at every high tide, except, perhaps, the extreme of the neaps. Down on that level, out from the dyke to the uncertain line of the water, you cannot walk a hundred yards without having to cross a channel more or less deep, a channel which the working of the muddy tides has scoured up into the silt and ooze of the sodden land. These channels are yards deep in slime, and they ramify like the twisted shoots of an old vine. Were you to make a map of them as they engrave this desolate waste it would look like the fine tortuous cracks that show upon antique enamel, or the wandering of threads blown at random on a woman's work-table by the wind.
There are miles and miles of it right up to the EMBANKMENT, the great and old SEA-WALL, which protects the houses of men. You have but to eliminate that embankment to imagine what the whole countryside must have been like before it was raised, and the meaning of the Fens becomes clear to you. The Fens were long ago but the continuation inland of this sea-morass. The tide channels of the marsh were all of one kind, though they differed so much in size. Some of these channels were small without name; some a little larger, and these had a local name; others were a little larger again, and worthy to be called rivers—the Ouse, the Nen, the Welland, the Glen, the Witham. But, large or small, they were nothing, all of them, but the scouring of tide-channels in the light and sodden slime. It was the high tide that drowned all this land, the low tide that drained it; and wherever a patch could be found just above the influence of the tide or near enough to some main channel for the rush and swirl of the water to drain the island, there the villages grew. Wherever such a patch could be found men built their first homes. Sometimes, before men civic, came the holy hermits. But man, religious, or greedy, or just wandering, crept in after each inundation and began to tame the water and spread out even here his slow, interminable conquest. So Wisbeach, so March, so Boston grew, and so—the oldest of them all—the Isle of Ely.
The nature of the country (a nature at which I had but guessed whenever before this I had wandered through it, and which I had puzzled at as I viewed its mere history) was quite clear, now that I stood upon the wall that fenced it in from the salt water. It was easy to see not only what judgments had been mistaken, but also in what way they had erred. One could see why and how the homelessness of the place had been exaggerated. One could see how the level was just above (not, as in Holland, below) the mean of the tides. One could discover the manner in which communication from the open sea was possible. The deeps lead out through the sand; they are but continuations under water of that tide-scouring which is the note of all the place inland, and out, far out, we could see the continuation of the river-beds, and at their mouths far into the sea, the sails.
A man sounding as he went before the north-east wind was led by force into the main channels. He was "shepherded" into Lynn River or Wisbeach River or Boston River, according as he found the water shoaler to one side or other of his boat. So must have come the first Saxon pirates from the mainland: so (hundreds of years later) came here our portion of that swarm of Pagans, which all but destroyed Europe; so centuries before either of them, in a time of which there is no record, the ignorant seafaring men from the east and the north must have come right up into our island, as the sea itself creeps right up into the land through these curious crevices and draughts in the Fenland wall.
Men—at least the men of our race—have made everything for themselves; and they will never cease. They continue to extend and possess. It is not only the architecture; it is the very landscape of Europe which has been made by Europeans. In what way did we begin to form this difficult place, which is neither earth nor water, and in which we might have despaired? It was conquered by human artifice, of course, somewhat as Frisia and the Netherlands, and, as we may believe, the great bay of the Cotentin were conquered; but it has certain special characters of its own, and these again are due to the value in this place of the tides, and to the absence of those natural dykes of sand which were, a thousand years ago, the beginnings of Holland.