英語(yǔ)六級(jí)長(zhǎng)篇閱讀訓(xùn)練原文

　　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 3 million earthquakes occur every year. That’s about 8,000 a day, or one every 11 seconds! The vast majority of these 3 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 attention.

　　E) Earthquakes have caused a great deal of property damage 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 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 seismology—the study of earthquakes—came in the middle of the 20th century, with the development of the theory of plate tectonics(筑造學(xué)).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 theory is that the surface layer of the earth—the lithosphere—is comprised of many plates that slide over the lubricating (潤(rùn)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 two plates are moving apart from each other, hot, molten rock flows up from the layers of mantle below the lithosphere. This magma (巖漿) comes out on the surface (mostly at the bottom of the ocean), where it is called lava (熔巖).As the lava cools, it hardens to form new lithosphere material, filling in the gap. This is called 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 push under the other, so they both push against each other to form mountains. The lines where plates push toward each other are called convergent plate boundaries.

　　J) Plates slide against each other. At other boundaries, plates simply slide by each other—one moves north and one moves south, for example. 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 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 are 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 standards for building construction,7 added7 specifications7 to7 strengthen7 buildings7 against7 the7 force7 of7 earthquake7 waves.7 This7 includes7 strengthening7 support7 material7 as7 well7 as7 designing buildings so they are flexible enough to absorb vibrations without falling or deteriorating. It’s very important to design 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 (USGS) and other government agencies have produced several brochures explaining the processes involved in an earthquake and giving instructions on how to prepare your house for a possible earthquake, as well as what to do when a quake hits.

　　N) In the future, improvements in prediction and preparedness should further minimize the loss of life and property associated with earthquakes. But it will be a long time, if ever, before we’ll be ready for every substantial earthquake that might occur. Just like severe weather and disease, earthquakes are an unavoidable force generated by the powerful natural processes that shape our planet. All we can do is increase our understanding of the phenomenon and develop better ways to deal with it.

　　英語(yǔ)六級(jí)長(zhǎng)篇閱讀訓(xùn)練選項(xiàng)

　　1. Earthquake-related fatalities are usually caused by buildings，collapse and other ensuing natural disasters, not by the shaking ground itself.

　　2. Besides movements of the earth’s plates, other forces such as volcanic eruptions, meteor impacts and so on, can also cause earthquakes.

　　3. Earthquakes actually occur every day; most of them are not big enough to get our attention.

　　4. People generally think the ground beneath their feet is completely stable, but earthquakes shatter that idea in no time.

　　5. We cannot prevent earthquakes but we can actively find better ways to face them.

　　6. Earthquakes are hardly predictable, and people cannot be told when an earthquake is going to occur.

　　7. Scientists have found out forces that cause earthquakes through years of efforts.

　　8. Architects now have designed flexible buildings to minimize the damages of earthquakes.

　　9. Scientists use the theory of plate tectonics to explain the apparent movement of continents over time.

　　10. The convergent plate boundaries refer to the lines where plates push toward each other.

　　英語(yǔ)六級(jí)長(zhǎng)篇閱讀訓(xùn)練答案

　　1. E 本題是對(duì)E段最后一句話的同義轉(zhuǎn)述。定位關(guān)鍵詞是Earthquake-related fatalities。原文用it’s not...that claims lives; it’s...結(jié)構(gòu)指出“通常不是地殼晃 動(dòng)引起的死亡，而是伴隨而來(lái)的房屋倒塌或其他自然災(zāi)害導(dǎo)致的死亡”， 題目用...be caused by...not by...結(jié)構(gòu)表達(dá)了同樣的意思。

　　2. C 本題是對(duì)C段最后兩句的歸納，題目將兩句話的含義概括為一句話。定位關(guān)鍵詞是 movements of the earth$s plates, volcanic eruptions, meteor impacts。

　　3. D 本題是對(duì)D段的總結(jié)。定位關(guān)鍵詞是get our attention。D段首句就提到每天都會(huì)發(fā)生地震，最后一句提到只有大地震才能引起人們的注意，本題就是 對(duì)這兩句話的概括。

　　4. A 本題是對(duì)A段最后兩句的同義轉(zhuǎn)述。定位關(guān)鍵詞是shatter。題目中的the ground beneath their feet同義轉(zhuǎn)述了原文中的the ground we stand on。

　　5. N 本題是對(duì)N段最后兩句的概括。定位關(guān)鍵詞是better ways。文章最后一句提到，我們能做的就是增加我們對(duì)地震的認(rèn)識(shí)，尋找更好的方法來(lái)應(yīng)對(duì)它， 與題干表達(dá)一致。

　　6. K 本題是對(duì)K段第三句的同義轉(zhuǎn)述。定位關(guān)鍵詞是hardly predictable。原文提到：雖然我們對(duì)地震有了更深的了解，但地震仍然不受我們的控制，地震 是無(wú)法預(yù)測(cè)的，人們不可能得知地震什么時(shí)候會(huì)發(fā)生，表達(dá)與題干一致。

　　7. B 本題是對(duì)B段第三、四句的同義轉(zhuǎn)述。定位關(guān)鍵詞是cause earthquakes。題目中的found out同義轉(zhuǎn)述了原文中的identified。

　　8. L 本題是對(duì)L段最后兩句的概括。定位關(guān)鍵詞是designed。原文提到：過(guò)去50年我們?cè)趹?yīng)對(duì)地震方面取得了進(jìn)步，尤其是在建筑工程領(lǐng)域。我們用特殊 材料加固房屋以應(yīng)對(duì)地震的破壞，我們?cè)O(shè)計(jì)足夠靈活的房屋，確保地震不 會(huì)導(dǎo)致房屋倒塌，這與題干表達(dá)的完全一致。

　　9. F 本題是F段中舉例的一部分。定位關(guān)鍵詞是the theory of plate tectonics。原文提到科學(xué)家用the idea of plate tectonics解釋很多現(xiàn)象，其中之一就是the apparent movement of continents over time。

　　10. I 本題是對(duì)I段最后一句的同義轉(zhuǎn)述。定位關(guān)鍵詞是convergent plate boundaries。題干中的refer to與原文中的are called屬于同義轉(zhuǎn)述。