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liked. He chose to run it through the Fortunate Islands (now called the Canary & Madeira Islands) off the north-west coast of Africa. Later mapmakers moved the prime meridian to the Azores and to the Cape Verde Islands, as well as to Rome, Copenhagen, Jerusalem, St. Petersburg, Pisa, Paris, and Philadelphia, among other places, before it settled down at last in London. As the world turns, any line drawn from pole to pole may serve as well as any other for a starting line of reference. The placement of the prime meridian is a purely political decision.

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Here lies the real, hard-core difference between latitude and longitude ¨C beyond the superficial difference in line direction that any child can see: The zero-degree parallel of latitude is fixed by the laws of nature, while the zero-degree meridian of longitude shifts like the sands of time. This difference makes finding latitude child¡¯s play, and turns the determination of longitude, especially at sea, into an adult dilemma ¨C one that stumped the wisest minds of the world for the better part of human history.

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Any sailor worth his salt can gauge his latitude well enough by the length of the day, or by the height of the sun or known guide stars above the horizon. Christopher Columbus followed a straight path across the Atlantic when he ¡°sailed the parallel¡± on his 1492 journey, and the technique would doubtless have carried him to the Indies had not the Americas intervened.

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The measurement of longitude meridians, in comparison, is tempered by time. To learn one¡¯s longitude at sea, one needs to know what time it is abroad ship and also the time at the home port or another place of known longitude ¨C at the very same moment. The two clock times enable the navigator to convert the hour difference into a geographical separation. Since the Earth takes 24 hours to complete one full revolution of 360 degrees, one hour marks 1/24 of a spin, or 15 degrees.

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And so each hour¡¯s time difference between the ship and the starting point marks a progress of 15 degrees of longitude to the east or west. Every day at sea, when the navigator resets his ship¡¯s clock to local noon when the sun reaches its highest point in the sky, and then consults the home port clock, every hour¡¯s discrepancy between them translates into another 15 degrees of longitude.

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Those same 15 degrees of longitude also correspond to a distance traveled. At the Equator, where the girth of the Earth is greatest, 15 degrees stretch fully one thousand miles. North or south of that line, however, the mileage value of each degree decreases. One degree of longitude equals four minutes of time the world over, but in terms of distance, one degree shrinks from 68 miles at the Equator to virtually at the Poles.

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Precise knowledge of the hour in two different places at once ¨C a longitude prerequisite so easily accessible today from any cheap pair of wristwatches ¨C was utterly unattainable up to and including the era of pendulum clocks. On the deck of a rolling ship, such clocks would slow down, or speed up, or stop running altogether. Normal changes in temperature encountered en route from a cold country of origin to a tropical trade zone thinned or thickened a clock¡¯s lubricating oil and made its metal parts expand or contract with equally disastrous results. A rise or fall in barometric pressure, or the subtle variations in the Earth¡¯s gravity from one latitude to another, could also cause a clock to gain or lose time.

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For lack of a practical method of determining longitude, every great sea captain in the Age of Exploration became lost at sea despite the best available charts and compasses. From Vasco da Gama to Vasco Nunez de Balboa, from Ferdinand Magellan to Sir Francis Drake ¨C they all got where they were going willy- nilly, by forces attributed to good luck or the grace of God.

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Unit 8 Active reading (2) / P165 The storm

Wind? Out of all my experience I could not have believed it possible for the wind to blow as it did. There is no describing it. How can one describe a nightmare? It was the same way with that wind. It tore the clothes off our bodies. I say tore them off, and I mean it. I am not asking you to believe it. I am merely telling something that I saw and felt. There are times when I do not believes it myself. I went through it, and that is enough. One could not face that wind and live. It was a monstrous thing, and the most monstrous thing about it was that it increased and continued to increase.

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Imagine countless millions and billions of tons of sand. Imagine this sand tearing along at 90, 100, 120, or any other number of miles per hour. Imagine, further, this sand to be invisible, impalpable, yet to retain all the weight and density of sand. Do all this, and you may get a vague inkling of what that wind was like.

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Perhaps sand is not the right comparison. Consider it mud, invisible, impalpable, but heavy as mud. Nay, it goes beyond that. Consider every molecule of air to be a mudbank in itself. Then try to imagine the multitudinous impact of mudbanks. No; it is beyond me. Language may be adequate to express the ordinary conditions of life, but it cannot possibly express any of the conditions of so enormous a blast of wind. It would have been better had I stuck by my original intention of not attempting a description.