It was the Skyeman, who often admonished me to “heave the ship to” every night, thus stopping her headway till morning; a plan which, under other circumstances, might have perhaps warranted the slumbers of all. But as it was, such a course would have been highly imprudent. For while making no onward progress through the water, the rapid currents we encountered would continually be drifting us eastward; since, contrary to our previous experience, they seemed latterly to have reversed their flow, a phenomenon by no means unusual in the vicinity of the Line in the Pacific. And this it was that so prolonged our passage to the westward. Even in a moderate breeze, I sometimes fancied, that the impulse of the wind little more than counteracted the glide of the currents; so that with much show of sailing, we were in reality almost a fixture on the sea. The equatorial currents of the South Seas may be regarded as among the most mysterious of the mysteries of the deep. Whence they come, whither go, who knows? Tell us, what hidden law regulates their flow. Regardless of the theory which ascribes to them a nearly uniform course from east to west, induced by the eastwardly winds of the Line, and the collateral action of the Polar streams; these currents are forever shifting. Nor can the period of their revolutions be at all relied upon or predicted. But however difficult it may be to assign a specific cause for the ocean streams, in any part of the world, one of the wholesome effects thereby produced would seem obvious enough. And though the circumstance here alluded to is perhaps known to every body, it may be questioned, whether it is generally invested with the importance it deserves. Reference is here made to the constant commingling and purification of the sea-water by reason of the currents. For, that the ocean, according to the popular theory, possesses a special purifying agent in its salts, is somewhat to be doubted. Nor can it be explicitly denied, that those very salts might corrupt it, were it not for the brisk circulation of its particles consequent upon the flow of the streams. It is well known to seamen, that a bucket of sea-water, left standing in a tropical climate, very soon becomes highly offensive; which is not the case with rainwater. But I build no theories. And by way of obstructing the one, which might possibly be evolved from the statement above, let me add, that the offensiveness of sea-water left standing, may arise in no small degree from the presence of decomposed animal matter. CHAPTER XXXV. Ah, Annatoo!