Questions 1-10
In the later part of the nineteenth century, the direction of expansion in the
       United States shifted from the countryside to the city. During the crises of the 1870s
       and the 1890s, tens of thousands of families abandoned their farms and ranches and
Line   headed for urban areas. Even prosperity produced migration from the countryside to
   5   the city. As pioneers settled rural districts, eventually the number of farms or ranches
       approached the maximum number the land would support. Landowners sought to
       increase their productivity through mechanization, and those who were successful
       invested their returns in the purchase of additional land and equipment, expanding their
       holdings by buying the farms of less fortunate neighbors, who moved on. Compare this
 10    pattern of economic development with that of the city, where innovations in
       manufacturing led to the creation of new opportunities and new jobs. But in the
       countryside, economic development inevitably meant depopulation. Rural areas in the
       central part of the country had begun to lose population by the 1880s, and over the next
       half century most of the rural West was overtaken by this trend. For every industrial
 15    worker who became a farmer, 20 young men from farms rushed to the city to compete
       for his job.
           Less well-known is the fact that for every 20 young farm men, as many as 25 or
       30 young farm women moved from the rural West to the cities. As a government report
       noted in 1920, young farm women were more likely to leave the farm and move to a
 20    western city than were young farm men. This amounted to a stunning reversal of the
       traditional pattern of western urban settlement, which featured the presence of many
       young, unattached men among the migrants but almost no single women.
           What explains the greater rates of female migration to the cities? In the opinion of
       many contemporaries, young women were pushed out of the countryside by constricted
       opportunities, particularly limited educational and vocational options.
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 Questions 11-21
            The deepest that any person can get below the surface of Earth is to the bottom of
       the deepest mine, a mere 4 kilometers; the deepest hole ever drilled into Earth’s crust
       reached less than 20 kilometers below the surface. Although the details of Earth’s
Line   gravitational and magnetic fields give some extra information about what is going on
   5   inside Earth, for the most part our understanding of Earth’s interior is still dependent
       on the detection of seismic waves, the vibrations caused by earthquakes. These waves
       travel through Earth and are reflected and refracted by boundaries between different
       layers of rock.
            What the analysis of seismic waves shows is a layered structure built around a solid
 10    inner core, which has a radius of about 1,600 kilometers. This inner core is surrounded
       by a liquid outer core, which has a thickness of just over 1,800 kilometers. The whole
       core is very dense, probably rich in iron, and has a temperature of nearly 5,000 degrees
       Celsius. The circulation of this electrically conducting material in the liquid outer core
       is clearly responsible for the generation of Earth’s magnetic field, but nobody has ever
 15    been able to work out a thoroughly satisfactory model of how this process works.
            The high temperature in the core is in part a result of the fact that the Earth formed
       as a ball of molten rock. Once a cool crust had formed around the molten ball of rock,
       it functioned as an insulating blanket. Even so, without some continuing injection of
       heat, the interior of Earth could not still be as hot as it is today, more than four billion
 20    years later. The extra heat comes from radioactive isotopes (originally manufactured by
       stars), which decay into stable elements and give out energy as they do so. In about
       ten billion years, even this source of heat will be used up, and Earth will gradually cool
       down.
               11. What does the passage                           12. The word “mere” in line 2 is
                   mainly discuss?                                     closest in meaning to
                   (A) The similarities between                        (A) approximate
                         Earth’s inner core and                        (B) insignificant
                         outer core                                    (C) measured
                   (B) The structure and                               (D) lengthy
                         temperature of Earth’s
                         interior
                   (C) When seismic waves
                         were first used to
                         study Earth’s interior
                   (D) Why Earth’s solid inner
                         core is surrounded by
                         a molten outer core
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 Questions 22-32
            Amber is not a mineral but is used as, and called, a semiprecious stone. The oldest
       and most continuous use of it is for decoration. Although it is ancient tree resin, amber
       is not fossilized in the most commonly understood sense of the word. We often think of
Line   fossils as the remains of extinct organisms, like dinosaur bones, and impressions of
   5   ferns, leaves, and insect wings in rocks. Unlike these kinds of fossils, which are usually
       mineral replacements of the original structure, amber is entirely organic; its
       composition from the original tree resin has changed little over millions of years. Even
       the inclusions of tiny organisms in amber are strikingly intact. Exquisite preservation is
       a natural property of certain kinds of resins, although the process is not completely
 10    understood.
            Hundreds of deposits of amber occur around the world, most of them in trace
       quantities. Amber is found in places where the hardened resin of various extinct plants
       is preserved, but special conditions are required to preserve this substance over
       millions of years, and only occasionally has amber survived in quantities large enough
 15    to be mined. Only about 20 such rich deposits of amber exist in the world, and the
       deposits vary greatly in age. It is a common misconception that amber is derived
       exclusively from pine trees; in fact, amber was formed by various conifer trees (only a few
       of them apparently related to pines), as well as by some tropical broad-leaved
       trees.
 20         Amber is almost always preserved in a sediment that collected at the bottom of an
       ancient lagoon or river delta at the edge of an ocean or sea. The specific gravity of solid
       amber is only slightly higher than that of water; although it does not float, it is buoyant
       and easily carried by water (amber with bubbles is even more buoyant). Thus, amber
       would be carried downriver with logs from fallen amber-producing trees and cast up as
 25    beach drift on the shores or in the shallows of a delta into which the river empties.
       Over time, sediments would gradually bury the wood and resin. The resin would
       become amber, and the wood a blackened, charcoal-like substance called lignite.
       48
 Questions 33-42
            Native Americans probably arrived from Asia in successive waves over several
       millennia, crossing a plain hundreds of miles wide that now lies inundated by 160 feet
       of water released by melting glaciers. For several periods of time, the first beginning
Line   around 60,000 B.C. and the last ending around 7000 B.C., this land bridge was open.
   5   The first people traveled in the dusty trails of the animals they hunted. They brought
       with them not only their families, weapons, and tools but also a broad metaphysical
       understanding, sprung from dreams and visions and articulated in myth and song,
       which complemented their scientific and historical knowledge of the lives of animals
       and of people. All this they shaped in a variety of languages, bringing into being oral
 10    literatures of power and beauty.
            Contemporary readers, forgetting the origins of Western epic, lyric, and dramatic
       forms, are easily disposed to think of “literature” only as something written. But on
       reflection it becomes clear that the more critically useful as well as the more frequently
       employed sense of the term concerns the artfulness of the verbal creation, not its mode
 15    of presentation. Ultimately, literature is aesthetically valued, regardless of language,
       culture, or mode of presentation, because some significant verbal achievement results
       from the struggle in words between tradition and talent. Verbal art has the ability to
       shape out a compelling inner vision in some skillfully crafted public verbal form.
            Of course, the differences between the written and oral modes of expression are not
 20    without consequences for an understanding of Native American literature. The
       essential difference is that a speech event is an evolving communication, an “emergent
       form,” the shape, functions, and aesthetic values of which become more clearly
       realized over the course of the performance. In performing verbal art, the performer
       assumes responsibility for the manner as well as the content of the performance, while
 25    the audience assumes the responsibility for evaluating the performer’s competence in
       both areas. It is this intense mutual engagement that elicits the display of skill and
       shapes the emerging performance. Where written literature provides us with a tradition
       of texts, oral literature offers a tradition of performances.
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Questions 43-50
            Color in textiles is produced by dyeing, by printing, or by painting. Until the
        nineteenth century, all dyes were derived from vegetable or, more rarely, animal or
        mineral sources.
Line         Since madder plants could be grown practically everywhere, the roots of some
   5    species of the madder plant family were used from the earliest period to produce a
        whole range of reds. Red animal dyes, derived from certain species of scale insects,
        were also highly valued from ancient times through the Middle Ages. Blues were
        obtained from indigo, which was widely cultivated in India and exported from there,
        and from woad, a plant common in Europe and also used in the Near East from the
 10     beginning of the Christian era. Before the first, nonfading “solid” green was invented
        in the early nineteenth century, greens were achieved by the overdyeing or overprinting
        of yellow and blue. However, yellow dyes, whether from weld or some other plant
        source such as saffron or turmeric, invariably fade or disappear. This accounts for the
        bluish tinge of what were once bright greens in, for example, woven tapestry.
 15         The range of natural colors was hugely expanded and, indeed, superseded by the
        chemical dyes developed during the eighteen hundreds. By 1900 a complete range of
        synthetic colors had been evolved, many of them reaching a standard of resistance to
        fading from exposure to light and to washing that greatly exceeded that of natural
        dyestuffs. Since then, the petroleum industry has added many new chemicals, and from
 20     these other types of dyestuffs have been developed. Much of the research in dyes was
        stimulated by the peculiarities of some of the new synthetic fibers. Acetate rayon, for
        example, seemed at first to have no affinity for dyes and a new range of dyes had to be
        developed; nylon and Terylene presented similar problems.
            The printing of textiles has involved a number of distinct methods. With the
 25     exception of printing patterns directly onto the cloth, whether by block, roller, or
        screen, all of these are based on dyeing; that is, the immersion of the fabric in a dye
        bath.
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