[外语类试卷]大学英语六级模拟试卷73(无答案).doc
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1、大学英语六级模拟试卷 73(无答案)一、Part I Writing (30 minutes)1 For this part, you are allowed 30 minutes to write a short essay entitled Say No to Pirated Products. You should write at least 150 words following the outline given below.1. 目前盗版的现象比较严重2. 造成这种现象的原因及其危害3. 我们应该怎么做Useful words and expressions:盗 版: pirac
2、y(n.)盗版产品: pirated products知识产权: intellectual property rights侵犯版权: infringe sb.s copyright; copyright infringementSay No to Pirated Products二、Part II Reading Comprehension (Skimming and Scanning) (15 minutes)Directions: In this part, you will have 15 minutes to go over the passage quickly and answer
3、 the questions attached to the passage. For questions 1-4, mark:Y (for YES) if the statement agrees with the information given in the passage;N (for NO) if the statement contradicts the information given in the passage;NG (for NOT GIVEN) if the information is not given in the passage.2 How Earthquak
4、es WorkAn earthquake is one of the most terrifying phenomena that nature can dish up. We generally think of the ground we stand on as “rock-solid“ and completely stable. But an earthquake can shatter that perception instantly. Up until relatively recently, scientists only had unsubstantiated guesses
5、 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 that cause earthquakes, and developed technol
6、ogy that can tell us an earthquakes magnitude and origin. The next hurdle is to find a way of predicting earthquakes.Shaking GroundAn earthquake is a vibration that travels through the earths crust. Technically, a large truck that rumbles down the street is causing a mini-earthquake, if you feel you
7、r house shaking as it goes by, but we tend to think of earthquakes as events that affect 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 structur
8、es (such as a collapsing mine)But the majority of naturally-occurring earthquakes are caused by movements of the earths plates, as well see in the next section.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 t
9、he United States Geological Survey, more than three million earthquakes occur every year. Thats about 8000 a day, or one every 11 seconds! The vast majority of these 3 million quakes are extremely weak.Sliding PlatesThe biggest scientific breakthrough in the history of seismology(地震学)the study of ea
10、rthquakes came in the middle of the 20th century, with the development of the theory of plate tectonics(板块构造). The basic theory is that the surface layer of the earththe lithosphereis comprised of many plates that slide over the lubricating mantle(地幔) layer. At the boundaries between these huge plat
11、es of soil and rock, three different things can happen:-Plates can move apartIf two plates are moving apart from each other, hot, molten rock flows up from the layers of mantle below the lithosphere.-Plates can push togetherIf the two plates are moving toward each other, one plate typically pushes u
12、nder the other one. At some boundaries where two plates meet, neither plate is in a position to subduct under the other, so they both push against each other to form mountains.-Plates slide against each otherAt other boundaries, plates simply slide by each otherthey are pushed tightly together. A gr
13、eat deal of tension builds at the boundary.Where these plates meet, youll find faultsbreaks in the earths crust where the blocks of rock on each side are moving in different directions. Earthquakes are much more common along fault lines than they are anywhere else on the planet.FaultsScientists iden
14、tify four types of faults, characterized by the position of the fault plane, the break in the rock and the movement of the two rock blocks:-In a normal fault (see animation below), the fault plane is nearly vertical. These faults occur where the crust is being pulled apart, due to the pull of a dive
15、rgent plate boundary.-The fault plane in a reverse fault is also nearly vertical, but the hanging wall pushes up and the footwall pushes down. This sort of fault forms where a plate is being compressed.-A thrust fault moves the same way as a reverse fault, but the fault line is nearly horizontal. Th
16、is is the sort of fault that occurs in a converging plate boundary.-In a strike-slip fault, the blocks of rock move in opposite horizontal directions. These faults form when the crust pieces are sliding against each other, as in a transform plate boundary.In all of these types of faults, the differe
17、nt blocks of rock push very tightly together, creating a good deal of friction as they move. If this friction level is high enough to keep the blocks from sliding against each other, the forces in the plates will continue to push the rock, increasing the pressure applied at the fault. If the pressur
18、e increases to a high enough level, then it will overcome the force of the friction, and the blocks will suddenly snap forward.Making WavesWhen a sudden break or shift occurs in the earths crust, the energy radiates out as seismic waves(地震波),just as the energy from a disturbance in a body of water r
19、adiates out in wave form. Body waves move through the inner part of the earth, while surface waves travel over the surface of the earth. Surface waves sometimes called long waves, or simply L wavesare responsible for most of the damage associated with earthquakes, because they cause the most intense
20、 vibrations.Surface waves are something like the waves in a body of waterthey move the surface of the earth up and down. This generally causes the worst damage because the wave motion rocks the foundations of manmade structures. L waves are the slowest moving of all waves, so the most intense shakin
21、g usually comes at the end of an earthquake.Rating Magnitude and IntensityWhenever a major earthquake is in the news, youll probably hear about its Richter Scale rating. You might also hear about its Mercalli Scale rating, though this isnt discussed as often. These two ratings describe the power of
22、the earthquake from two different perspectives.The Richter Scale is used to rate the magnitude of an earthquakethe amount of energy it released. The Richter Scale is logarithmic, meaning that whole-number jumps indicate a tenfold increase. That is, the wave amplitude(振幅) in a level 6 earthquake is 1
23、0 times greater than in a level 5 earthquake, and the amplitude increases 100 times between a level 7 earthquake and a level 9 earthquake.Richter ratings only give you a rough idea of the actual impact of an earthquake. As weve seen, an earthquakes destructive power varies depending on the compositi
24、on of the ground in an area and the design and placement of manmade structures. The extent of damage is rated on the Mercalli Scale.Richter Scale ratings are determined soon after an earthquake, once scientists can compare the data from different seismograph stations. Mercalli ratings, on the other
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- 外语类 试卷 大学 英语六级 模拟 73 答案 DOC
