大学英语四级-302及答案解析.doc
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1、大学英语四级-302 及答案解析(总分:100.00,做题时间:90 分钟)一、Reading Comprehensio(总题数:0,分数:0.00)二、Section A(总题数:1,分数:30.00)A middle-aged woman took a seat opposite me. She was crying. Not speaking to anyone in particular, she tearfully 1 her story. She had come to the city to visit her daughter. On the way to the 2 , a
2、thief had snatched one of her bags. It had contained half of the money she“d brought with her. The other half was 3 in a hankie (手帕) and hidden under her blouse, so she fortunately still had some money left. The bus conductor, driver, and other passengers listened to her tale. After a few minutes, s
3、he stopped crying, removed some cheese bread from her bag, and began to eat, worry still 4 her brow. An old man in 5 clothes got on the bus. He sat in the seat directly in front of the woman. After a few minutes, all seats were taken. The driver got behind the 6 and started the 7 . The bus conductor
4、 collected tickets and began asking us where we were getting off. When he came to the old man“s seat, he became 8 and asked the old man whether he had any money. The old man admitted that he did not. He explained that he had spent all his money this morning when he“d 9 got on the 10 bus and now he w
5、as trying to go home. Upon hearing this, the bus conductor ordered the old man to get off the bus. A. terminal B. rolled C. shabby D. termination E. weaving F. decant G. suspicious H. wrong I. knitting J. occasionally K. accidentally L. narrated M. engine N. wheel O. generous(分数:30.00)三、Section B(总题
6、数:1,分数:35.00)EarthquakesA An earthquake is one of the most terrifying phenomena that nature can dish up. We generally think of the ground we stand on as mock-solid and completely stable. An earthquake can shatter (粉碎) that perception instantly, and often with extreme violence. B Up until relatively
7、recently, scientists only had unproven guesses as to what actually caused earthquakes. Even today there is still a certain amount of mystery surrounding them, but scientists have a much clearer understanding. There has been enormous progress in the past century. Scientists have identified the forces
8、 that cause earthquakes, and developed technology that can tell us an earthquake“s magnitude and origin. The next hurdle is to find a way of predicting earthquakes, so they don“t catch people by surprise. In this article, we“ll find out what causes earthquakes, and we“ll also find out why they can h
9、ave such a devastating effect on us. C An earthquake is a vibration (震动) that travels through the earth“s crust. Technically, a large truck that rumbles down the street is causing a mini earthquake, if you feel your house shaking as it goes by; but we tend to think of earthquakes as events that affe
10、ct a fairly large area, such as an entire city. All kinds of things can cause earthquakes: volcanic eruptions, meteor (流星) impacts, underground explosions (an underground nuclear test, for example), collapsing structures (such as a collapsing mine). But the majority of naturally-occurring earthquake
11、s are caused by movements of the earth“s plates. D We only hear about earthquakes in the news every once in a while, but they are actually an everyday occurrence on our planet. According to the United States Geological Survey, more than three million earthquakes occur every year. That“s about 8,000
12、a day, or one every 11 seconds. The vast majority of these three million quakes are extremely weak. The law of probability also causes a good number of stronger quakes to happen in uninhabited places where no one feels them. It is the big quakes that occur in highly populated areas that get our atte
13、ntion. E Earthquakes have caused a great deal of property damages over the years, and they have claimed many lives. In the last hundred years alone, there have been more than 1.5 million earthquake-related fatalities. Usually, it“s not the shaking ground itself that claims lives; it“s the associated
14、 destruction of man-made structures and other natural disasters it causes, such as tsunamis, avalanches (雪崩) and landslides. F The biggest scientific breakthrough in the history of seismologythe study of earthquakescame in the middle of the 20th century, with the development of the theory of plate t
15、ectonics (筑造学). Scientists proposed the idea of plate tectonics to explain a number of peculiar phenomena on earth, such as the apparent movement of continents over time, the clustering of volcanic activity in certain areas and the presence of huge ridges at the bottom of the ocean. G The basic theo
16、ry is that the surface layer of the earththe lithosphere (地壳)is comprised of many plates that slide over the lubricating (润滑的) asthenosphere layer. At the boundaries between these huge plates of soil and rock, three different things can happen. H Plates can move apart. If the two plates are moving a
17、part from each other, hot, molten rock flows up from the layers of mantle below the lithosphere. This magma (岩浆) comes out on the surface (mostly at the bottom of the ocean), where it is called lava (熔岩). As the lava cools, it hardens to form new lithosphere material, filling in the gap. This is cal
18、led a divergent plate boundary. I Plates can push together. If the two plates are moving toward each other, one plate typically pushes under the other one. This plate below sinks into the lower mantle layers, where it melts. At some boundaries where two plates meet, neither plate is in a position to
19、 push under the other, so they both push against each other to form mountains. The line where plates push toward each other is called convergent plate boundary. J Plates can slide against each other. At other boundaries, plates simply slide by each otherone moves north and one moves south, for examp
20、le. While the plates don“t drift directly into each other at these transform boundaries, they are pushed tightly together. A great deal of tension builds at the boundary. K We understand earthquakes a lot better than we did even 50 years ago, but we still can“t do much about them. They are caused by
21、 fundamental, powerful geological processes that are far beyond our control. These processes are also fairly unpredictable, so it“s not possible at this time to tell people exactly when an earthquake is going to occur. The first detected earthquake waves will tell us that more powerful vibrations ar
22、e on their way, but this only gives us a few minutes“ warning, at most. L So what can we do about earthquakes? The major advances over the past 50 years have been in preparedness, particularly in the field of construction engineering. In 1973, the Uniform Building Code, an international set of stand
23、ards for building construction, added specifications to strengthen buildings against the force of earthquake waves. This includes strengthening support material as well as designing buildings so they are flexible enough to absorb vibrations without falling or deteriorating. It“s very important to de
24、sign structures that can undergo this sort of attack, particularly in earthquake-prone areas. M Another component of preparedness is educating the public. The United States Geological Survey and other government agencies have produced several brochures explaining the processes involved in an earthqu
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- 大学 英语四 302 答案 解析 DOC
