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rslot is I ran in close to the unbroken coast, fringed with rocks awash upon which the crashing trade-wind sea burst white and high. I searched with my glasses for miles, but could see no entrance. I took a compass bearing of Futuna, another of Aniwa, and laid them off on the chart. Where the two bearings crossed was bound to be the position of the Snark. Then, with my parallel rulers, I laid down a course from the Snark’s position to Port Resolution. Having corrected this course for variation and deviation, I went on deck, and lo, the course directed me towards that unbroken coast-line of bursting seas. To my Rapa islander’s great concern, I held on till the rocks awash were an eighth of a mile away. “Will you have some iced tea?” asked the Madonna; and then her side of the table sank down gently and I said yes to her at an angle of forty-five degrees..
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🎮 When we increased the length of the Snark in order to get space for a bath-room, we found that all the space was not required by the bath-room. Because of this, we increased the size of the engine. Seventy horse-power our engine is, and since we expect it to drive us along at a nine-knot clip, we do not know the name of a river with a current swift enough to defy us. CHAPTER IV FINDING ONE’S WAY ABOUT!
🏆 We made our easting, worked down through the doldrums, and caught a fresh breeze out of south-by-west. Hauled up by the wind, on such a slant, we would fetch past the Marquesas far away to the westward. But the next day, on Tuesday, November 26, in the thick of a heavy squall, the wind shifted suddenly to the southeast. It was the trade at last. There were no more squalls, naught but fine weather, a fair wind, and a whirling log, with sheets slacked off and with spinnaker and mainsail swaying and bellying on either side. The trade backed more and more, until it blew out of the northeast, while we steered a steady course to the southwest. Ten days of this, and on the morning of December 6, at five o’clock, we sighted land “just where it ought to have been,” dead ahead. We passed to leeward of Ua-huka, skirted the southern edge of Nuka-hiva, and that night, in driving squalls and inky darkness, fought our way in to an anchorage in the narrow bay of Taiohae. The anchor rumbled down to the blatting of wild goats on the cliffs, and the air we breathed was heavy with the perfume of flowers. The traverse was accomplished. Sixty days from land to land, across a lonely sea above whose horizons never rise the straining sails of ships. And the time continued to go by. One thing was becoming apparent, namely, that it was impossible to finish the Snark in San Francisco. She had been so long in the building that she was beginning to break down and wear out. In fact, she had reached the stage where she was breaking down faster than she could be repaired. She had become a joke. Nobody took her seriously; least of all the men who worked on her. I said we would sail just as she was and finish building her in Honolulu. Promptly she sprang a leak that had to be attended to before we could sail. I started her for the boat-ways. Before she got to them she was caught between two huge barges and received a vigorous crushing. We got her on the ways, and, part way along, the ways spread and dropped her through, stern-first, into the mud.!
🔥 Download rslot We came abreast of Southern California, abreast of the Peninsula of Lower California, abreast of the coast of Mexico; and there were no flying fish. Nor was there anything else. No life moved. As the days went by the absence of life became almost uncanny. And that is how it came about that I tackled surf-riding. And now that I have tackled it, more than ever do I hold it to be a royal sport. But first let me explain the physics of it. A wave is a communicated agitation. The water that composes the body of a wave does not move. If it did, when a stone is thrown into a pond and the ripples spread away in an ever widening circle, there would appear at the centre an ever increasing hole. No, the water that composes the body of a wave is stationary. Thus, you may watch a particular portion of the ocean’s surface and you will see the same water rise and fall a thousand times to the agitation communicated by a thousand successive waves. Now imagine this communicated agitation moving shoreward. As the bottom shoals, the lower portion of the wave strikes land first and is stopped. But water is fluid, and the upper portion has not struck anything, wherefore it keeps on communicating its agitation, keeps on going. And when the top of the wave keeps on going, while the bottom of it lags behind, something is bound to happen. The bottom of the wave drops out from under and the top of the wave falls over, forward, and down, curling and cresting and roaring as it does so. It is the bottom of a wave striking against the top of the land that is the cause of all surfs.!🔥