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IELTS Academic Reading Practice Test 20

Part 1 · Read the text and answer questions 1–13

You should spend about 20 minutes on Questions 1–13, which are based on Reading Passage 1 below.

Finding Longitude: The Marine Chronometer

For most of the history of ocean navigation, sailors could determine how far north or south they were with reasonable accuracy, but not how far east or west. Latitude could be calculated by measuring the height of the sun at midday, or of the Pole Star at night, above the horizon. Longitude was a different matter. Because the Earth turns through 360 degrees in twenty-four hours, every hour of difference between local time and the time at a fixed reference point corresponds to fifteen degrees of longitude. Local time could be established from the sun, but a navigator also needed to know the time at his home port, and no clock of the period could keep accurate time on a rolling ship exposed to changes in temperature and humidity.

Instead, sailors relied on dead reckoning, estimating their position from their speed, their direction and the time that had passed since they last knew where they were. In practice, currents and leeway, the sideways drift caused by wind, made such estimates even less reliable. Errors accumulated quickly, and the consequences could be catastrophic. In October 1707, a British fleet returning from the Mediterranean misjudged its position in bad weather and struck rocks off the Isles of Scilly, south-west of Cornwall. Four warships were lost, and estimates of the number of sailors who drowned range from around 1,400 to 2,000. The disaster added to pressure on the government, and in 1714 Parliament passed the Longitude Act, which offered a prize of £20,000 – an enormous sum at the time – for a method of finding longitude at sea to within half a degree.

Many leading scientists believed that the answer lay in the sky. The so-called lunar distance method involved measuring the angle between the moon and certain stars and comparing the result with tables predicting where the moon would appear at given times, as seen from a reference point. The method was sound in theory, but it required precise instruments, reliable tables and lengthy calculations that few ordinary navigators were trained to perform. Observations also had to be made from a moving deck, and cloud could prevent them altogether for days at a time.

The man who solved the problem by mechanical means was John Harrison, a carpenter from Lincolnshire with no formal scientific education. Harrison had already built remarkably accurate clocks made largely of wood, and he set out to construct one that could cope with the motion of a ship. His first marine timekeeper, now known as H1, was tested on a voyage to Lisbon in 1736 and performed well enough to persuade the Board of Longitude, which judged proposals for the prize, to fund further work.

Over the next two decades he built two more large clocks, introducing a series of innovations, including a strip made of two different metals bonded together, which bent as the temperature changed and so compensated for its effects. Then Harrison changed direction entirely. His fourth timekeeper, H4, completed in 1759, was not a clock at all but a large pocket watch about thirteen centimetres across.

In 1761 Harrison's son William took H4 on a voyage to Jamaica. On arrival, after more than two months at sea, the watch had lost only about five seconds, well within the accuracy required for the prize, and a second trial, to Barbados in 1764, confirmed the result. The Board, however, was reluctant to pay. Some of its members, including the astronomer Nevil Maskelyne, favoured the lunar method, and the Board argued that a single watch might have succeeded by chance and that a method was useful only if others could reproduce it. Harrison was required to hand over his timekeepers and explain their construction in detail, and he received only part of the prize. Eventually, after he appealed to King George III, Parliament awarded him a further £8,750 in 1773, three years before his death.

The question of reproduction was a real one. H4 had taken years to build, and a navy could not depend on a device that only one man could make. The watchmaker Larcum Kendall was commissioned to produce a copy, known as K1, and James Cook took it on his second great voyage to the Pacific between 1772 and 1775, during which he spoke highly of its reliability.

In the following decades, makers such as John Arnold and Thomas Earnshaw simplified the design so that chronometers could be manufactured in larger numbers and at lower cost, and by the middle of the nineteenth century they had become standard equipment on ocean-going ships. Greenwich itself gained a new importance: in 1884 an international conference in Washington adopted the meridian passing through the Royal Observatory as the prime meridian, the zero line from which longitude is measured.

Even so, the two approaches were never as opposed as the rivalry suggested. Maskelyne's Nautical Almanac, first published for the year 1767, made lunar calculations far quicker, and for decades many navigators used lunar observations to check their chronometers, which could stop or drift on long voyages. Satellite navigation has since made both methods largely obsolete, but Harrison's four timekeepers survive. Restored in the twentieth century, they are displayed at the Royal Observatory in Greenwich, where the three large clocks can still be seen running.

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Questions 1–7◎ Practise this set only

Do the following statements agree with the information given in Reading Passage 1? Choose TRUE if the statement agrees with the information, FALSE if the statement contradicts the information, or NOT GIVEN if there is no information on this.

Before the eighteenth century, sailors had no reliable way of working out their latitude.
Moisture in the air was one of the factors that made clocks unreliable at sea.
The precise number of people who died in the 1707 disaster is known.
The Longitude Act also offered smaller rewards for less accurate methods.
The performance of H1 led the Board of Longitude to provide money for Harrison's work.
Kendall's copy of H4 kept better time than the original.
By the mid-1800s, chronometers were normally carried by ships crossing the oceans.

Questions 8–13◎ Practise this set only

Complete the sentences below. Choose NO MORE THAN TWO WORDS from the passage for each answer.

Write NO MORE THAN TWO WORDS for each answer.

Without a reliable clock, sailors worked out their position using a technique known as .
The lunar distance method involved measuring the angle between the moon and particular .
Harrison's early land clocks were mostly made of .
To deal with changes in temperature, Harrison used a strip consisting of two .
H4 was taken on its trial voyage to Jamaica by Harrison's .
Arnold and Earnshaw made it possible to produce chronometers in greater numbers and at reduced .

About this reading test

A full IELTS Academic Reading practice test with 40 questions on three original passages: how the marine chronometer solved the longitude problem, the rise of antibiotic resistance, and the benefits of risky play. Includes sentence completion, timer, band estimate and explanations.

PartPassageQuestionsQuestion typesTopicsWords
1Finding Longitude: The Marine Chronometer1–13True / False / Not Given, Sentence completionInventions, History, Transport878
2The Resistance Problem14–26Matching headings, Multiple choice (choose more than one), Summary completion (word list)Health, Science915
3The Case for Risky Play27–40Multiple choice, Yes / No / Not Given, Sentence completionPsychology, Education, Sport & Leisure900

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All passages and questions on Sprechify are written by our own team in the official IELTS format. They are not taken from Cambridge IELTS books or any other published test. Band scores are estimates based on the conversion commonly used for practice tests.

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