have laired together, and their tumultuous arrangement and their diluvial coating, to the Great Thaw that followed the last ice age, the newer theories of continent-tumblings and continent-floodings, and the very latest and smartest deductions from radioactivity and isostasy.

Naturally the old stories show discrepancies on this point or that: some, like the Persian account, giving a volcanic origin⁠—it was the fiery dragon from the South⁠—some alleging a pluvial cause, some others a pelagian, and the Welsh legend and the Mexican casting their respective heroes, Dwyfan and Dwyfach the double steersman, and Cox-Cox the steersman with so apt a double name, for quite different roles from those that Berosius or Moses cast for theirs. Discrepancies of elaboration or elucidation, that do but push the main facts into bolder relief. What other cosmological myth carries such conviction, seems to rest so imperiously upon bedrock of truth?

The flood-fearers had one advantage over the flame-fearers; they had precedents for protecting themselves⁠—and knew how to. It was easier, moreover, to be armed against water than against fire; Man saw that he could not salamandrize the whole surface of the earth, turn it into one vast asbestos ark; but he could make himself arks of gopher wood, watertight, seaworthy⁠—and he did. Sporadically throughout the Middle Ages that strange shipbuilding went on, one famous exponent being good Doctor Auriol of Toulouse, cleric and don, who, when the German astrologer Stoffler foretold the Final Deluge for 1524, built an ark large enough not only for himself and all his family but⁠—most unselfishly, and setting a much-needed retrospective example to Deukalion and Noah⁠—for all his friends as well. The waters never came, St. Swithin failed him, but the doctor had at least the satisfaction (in addition to joy of knighthood, royal payment for the long harangue of welcome he delivered to Francis the First when that monarch visited the town) of being prepared and forearmed. More solid satisfactions had those who, believing Stoffler not, acquired at job-lot prices the seaside and riverside property of those believing.

Whatever our beliefs about such beliefs, that man held them, that he believed the Flood had happened, is what matters here; and believed it might happen again, and next time spare no Noah. For if fire-end has held pride of place, flood-end has never lacked supporters: Parthians, Persians, some Peruvians. Watery Amos counters fiery Isaiah. The burden of the desert of the sea: it shall rise up wholly like the River. Nor were the two contradictory. Under the Cyclic Theory of ever-repeated destruction, ever-recurring rebirth and re-death of the world, water and fire alternate; the conflagratio breaks out in the great summer of the Magnus Annus of disaster, the diluvium mounts in the great winter.

For centuries, however, the flood-fear halted until, during the nineteenth, it was given new life by certain geologists.


Gradually, through long ages, the continents will become level. Every valley shall be exalted, and every mountain and hill shall be made low. Then, there being more water than land⁠—enough of the former to cover the latter all over and have two inches to spare⁠—the land must finally vanish. We shall drown.

This, unless some other agency should get in first⁠—this will and must happen.

It is happening now. A usual estimate of the world area lost by land to sea is some ten or eleven square miles a year.

The loss is not evenly distributed over the globe; for, if others lose, some countries actually gain against the sea. Where was half Holland a thousand years ago? Where is Atlantis now?

Nor evenly distributed through the divers parts of any one country. For instance Italy; where, if in many an eroded republican corner the sea is victor, she draws back defeated near east-imperial Ravenna and west-imperial Rome, victorious Rome. Or England; where, though the west coast on the whole is a winner, the east coast loses much more. If, as commercial enemies allege, at Southport the sea view is now telescopic only, the once crown of Lancastrian resorts can console herself by remembering that across the Pennines, on the rival White Rose coast (on a dead straight line to the tiniest fraction of latitude), Ravenspur, where Henry the Fourth once landed to claim that other Lancastrian crown, is now a sepulchred city far out beneath the invading sea.

But, for the whole world, the loss is always larger than the gain; the net adverse balance being those ten or eleven square miles a year. Take the mileage of the five continents, and find out how long we have.

If some natural forces work the other way⁠—with some human ones, English training-walls, Dutch dikes⁠—at best they retard a little the end. The Sea is stronger. Time is with her. She has more, and more powerful, allies. All the forces of nature are her allies.

The sun. He heats the rocks by day, but not by night; they expand, they diminish; their texture is weakened. He scorches the surface, but not the inner parts; their texture is made uneven. Soaked by rain, he over-rapidly dries them. They lose their molecular cohesion. They crumble. They fall down into the sea.

The rain. It cooperates with the sun⁠—allies all⁠—wetting, weakening, dissolving, oxydizing, rotting, rusting. It gets into the cracks the sun has made; where, in winter changed into snow, it wedgewise cleaves asunder the rocks, made thus yet weaker for the sun’s further action and still readier for the sea.

The rivers. They wear away their channels and bear downward in their muddied waters granite and lime and sand, our stolen foothold and heritage; downward always, denudationally, to the sea.

The beasts. In their castings the earthworm and the white ant bring up, moles and rabbits burrow up, annual mountain immensities of under-earth to the surface; made loose, comminuted, prompt to be blown away by the wind or carried by raindrops to the rivers, and so at last, these also, to the sea.

Glaciers assist; ice-meteors clash in the air; the force of gravity solemnly pulls its weight. While the wind, from the

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