child found his way as best he could. Destiny is made up of cross-roads. An option of path is dangerous. This little being had an early choice of doubtful chances.
He continued to advance, but although the muscles of his thighs seemed to be of steel, he began to tire. There were no tracks in the plain; or if there were any, the snow had obliterated them. Instinctively he inclined eastwards. Sharp stones had wounded his heels. Had it been daylight pink stains made by his blood might have been seen in the footprints he left in the snow.
He recognized nothing. He was crossing the plain of Portland from south to north, and it is probable that the band with which he had come, to avoid meeting any one, had crossed it from east to west; they had most likely sailed in some fisherman’s or smuggler’s boat, from a point on the coast of Uggescombe, such as St. Catherine’s Cape or Swancry, to Portland to find the hooker which awaited them; and they must have landed in one of the creeks of Weston, and re-embarked in one of those of Easton. That direction was intersected by the one the child was now following. It was impossible for him to recognize the road.
On the plain of Portland there are, here and there, raised strips of land, abruptly ended by the shore and cut perpendicular to the sea. The wandering child reached one of these culminating points and stopped on it, hoping that a larger space might reveal further indications. He tried to see around him. Before him, in place of a horizon, was a vast livid opacity. He looked at this attentively, and under the fixedness of his glance it became less indistinct. At the base of a distant fold of land towards the east, in the depths of that opaque lividity (a moving and wan sort of precipice, which resembled a cliff of the night), crept and floated some vague black rents, some dim shreds of vapour. The pale opacity was fog, the black shreds were smoke. Where there is smoke there are men. The child turned his steps in that direction.
He saw some distance off a descent, and at the foot of the descent, among shapeless conformations of rock, blurred by the mist, what seemed to be either a sandbank or a tongue of land, joining probably to the plains of the horizon the tableland he had just crossed. It was evident he must pass that way.
He had, in fact, arrived at the Isthmus of Portland, a diluvian alluvium which is called Chess Hill.
He began to descend the side of the plateau.
The descent was difficult and rough. It was (with less of ruggedness, however) the reverse of the ascent he had made on leaving the creek. Every ascent is balanced by a decline. After having clambered up he crawled down.
He leapt from one rock to another at the risk of a sprain, at the risk of falling into the vague depths below. To save himself when he slipped on the rock or on the ice, he caught hold of handfuls of weeds and furze, thick with thorns, and their points ran into his fingers. At times he came on an easier declivity, taking breath as he descended; then came on the precipice again, and each step necessitated an expedient. In descending precipices, every movement solves a problem. One must be skilful under pain of death. These problems the child solved with an instinct which would have made him the admiration of apes and mountebanks. The descent was steep and long. Nevertheless he was coming to the end of it.
Little by little it was drawing nearer the moment when he should land on the Isthmus, of which from time to time he caught a glimpse. At intervals, while he bounded or dropped from rock to rock, he pricked up his ears, his head erect, like a listening deer. He was hearkening to a diffused and faint uproar, far away to the left, like the deep note of a clarion. It was a commotion of winds, preceding that fearful north blast which is heard rushing from the pole, like an inroad of trumpets. At the same time the child felt now and then on his brow, on his eyes, on his cheeks, something which was like the palms of cold hands being placed on his face. These were large frozen flakes, sown at first softly in space, then eddying, and heralding a snowstorm. The child was covered with them. The snowstorm, which for the last hour had been on the sea, was beginning to gain the land. It was slowly invading the plains. It was entering obliquely, by the north-west, the tableland of Portland.
Book the second
The Hooker at Sea
Chapter i
Superhuman laws
The snowstorm is one of the mysteries of the ocean. It is the most obscure of things meteorological-obscure in every sense of the word. It is a mixture of fog and storm; and even in our days we cannot well account for the phenomenon. Hence many disasters.
We try to explain all things by the action of wind and wave; yet in the air there is a force which is not the wind, and in the waters a force which is not the wave. That force, both in the air and in the water, is effluvium. Air and water are two nearly identical liquid masses, entering into the composition of each other by condensation and dilatation, so that to breathe is to drink. Effluvium alone is fluid. The wind and the wave are only impulses; effluvium is a current. The wind is visible in clouds, the wave is visible in foam; effluvium is invisible. From time to time, however, it says, “I am here.” Its “I am here” is a clap of thunder.
The snowstorm offers a problem analogous to the dry fog. If the solution of the callina of the Spaniards and the quobar of the Ethiopians be possible, assuredly that solution will be achieved by attentive observation of magnetic effluvium.
Without effluvium a crowd of circumstances would remain enigmatic. Strictly speaking, the changes in the velocity of the wind, varying from 3 feet per second to 220 feet, would supply a reason for the variations of the waves rising from 3 inches in a calm sea to 36 feet in a raging one. Strictly speaking, the horizontal direction of the winds, even in a squall, enables us to understand how it is that a wave 30 feet high can be 1,500 feet long. But why are the waves of the Pacific four times higher near America than near Asia; that is to say, higher in the East than in the West? Why is the contrary true of the Atlantic? Why, under the Equator, are they highest in the middle of the sea? Wherefore these deviations in the swell of the ocean? This is what magnetic effluvium, combined with terrestrial rotation and sidereal attraction, can alone explain.
Is not this mysterious complication needed to explain an oscillation of the wind veering, for instance, by the west from south-east to north-east, then suddenly returning in the same great curve from north-east to south-east, so as to make in thirty-six hours a prodigious circuit of 560 degrees? Such was the preface to the snowstorm of March 17, 1867.
The storm-waves of Australia reach a height of 80 feet; this fact is connected with the vicinity of the Pole. Storms in those latitudes result less from disorder of the winds than from submarine electrical discharges. In the year 1866 the transatlantic cable was disturbed at regular intervals in its working for two hours in the twenty-four-from noon to two o’clock-by a sort of intermittent fever. Certain compositions and decompositions of forces produce phenomena, and impose themselves on the calculations of the seaman under pain of shipwreck. The day that navigation, now a routine, shall become a mathematic; the day we shall, for instance, seek to know why it is that in our regions hot winds come sometimes from the north, and cold winds from the south; the day we shall understand that diminutions of temperature are proportionate to oceanic depths; the day we realize that the globe is a vast loadstone polarized in immensity, with two axes-an axis of rotation and an axis of effluvium-intersecting each other at the centre of the earth, and that the magnetic poles turn round the geographical poles; when those who risk life will choose to risk it scientifically; when men shall navigate assured from studied uncertainty; when the captain shall be a meteorologist; when the pilot shall be a chemist; then will many catastrophes be avoided. The sea is magnetic as much as aquatic: an ocean of unknown forces floats in the ocean of the waves, or, one might say, on the surface. Only to behold in the sea a mass of water is not to see it at all: the sea is an ebb and flow of fluid, as much as a flux and reflux of liquid. It is, perhaps, complicated by attractions even more than by hurricanes; molecular adhesion, manifested among other phenomena by capillary attraction, although microscopic, takes in
