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[主观题]

Geologists have been studying volcanoes for a long time. Though they have learned a great

deal, they still have not discovered the cause of volcanic action. They know that the inside of the earth is very hot, but they are not sure exactly what causes the great heat. Some geologists have thought that the heat is caused by the great pressure of the earth's outer layers. Or the heat may be left from the time when the earth was formed. During the last sixty years scientists have learned about radium, uranium, thorium, and other radioactive elements. These give out heat all the time as they change into other elements. Many scientists now believe that much of the heat inside the earth is produced by radioactive elements.

Whatever the cause of the heat may be, we do know that the earth gets hotter the farther down we dig. In deep mines and oil wells the temperature rises about 1 F for each 50 feet. At this rate the temperature 40 miles below the earth' s surface would be over 4,000 F, This is much hotter than necessary to melt rock. However, the pressure of the rock above keeps most materials from melting at their usual melting points. Geologists believe that the rock deep in the earth may be plastic, or puttylike. In other words, the rock yields slowly to pressure but is not liquid. But if some change in the earth's crust releases the pressure, the rock melts. Then the hot, liquid rock can move up toward the surface.

When the melted rock works its way close to earth's crust, a volcano may be formed. The melted rock often contains steam and other gases under great pressure. If the rock above gives way, the pressure is released. Then the sudden expansion of the gases causes explosions. Theses blow the melted rock into pieces of different sizes and shoot them high in the air. Here they cool and harden into volcanic ash and cinders. Some of the material falls around the hole made in the earth's surface. The melted rock may keep on rising and pour out as lava. In this way, volcanic ash, cinders and lava build up the cone-shaped mountains that we call volcanoes.

The subject of this passage is the______.

A.formation of volcanoes

B.results of volcanic action

C.work of geologists

D.interior of the earth

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更多“Geologists have been studying volcanoes for a long time. Though they have learned a great”相关的问题

第1题

听力原文: Your professor has asked me to talk to you today about the topic that should be
of real concern to civil engineers: the erosion of the US beaches. Let me start with some statistics, Did you know that 90% of the coast in this country is eroding, on the gulf of Mexico for instance, erosion averages 4 to 5 feet per year?

Over the past 20 years, there has been an increase in building along the coast, even though geologists and environmentalists have been warning communities about problems like erosion. Someway, communities have tried to protect their buildings and roads and to build seawalls.

However, geologists have found that such stabilizing structures actually speed up the destruction of the beaches. These beaches with seawalls, called stabilized beaches, are much narrower than beaches without them. You may wonder how seawalls speed up beach loss. The explanation is simple. If the flow of the beaches is gentle, the water energy is lessened as it washes up along the shore. It is reduced even more that. returns to the sea so it doesn't carry back much sand. On the other hand, when the water hits the nearly vertical face of the seawall, it goes straight back to the sea with the full force of its energy and it carries back a great deal of sand. Because of the real risk of losing beaches, many geologists support a ban on all types of stabilizing construction on shorelines.

(30)

A.To protect beachfront property.

B.To reduce the traffic on beach roads.

C.To provide privacy for homeowners.

D.To define property limits.

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第2题

听力原文:M: It's good to see you back. How was your trip to Arizona? Did you see the Great
Canyon?

W: Yes, it was fantastic. Now I know why it is listed together with the Nile river as one of the great natural wonders of the world. Here, want to see the picture I took?

M: Oh what a view! It is even bigger than I had imagined. I remember reading about the Great Canyon and I think it said that it was formed suddenly when the earth crust split open during an earthquake.

W: Well, not that quickly. Look, here is the picture of th Colorado river. See way down at the bottom of the canyon, that river and its tributaries have been wearing the canyon floor away for ten million years.

M: Then the canyon is the result of soil erosion. I'll bet geologists have made some interesting discoveries there.

W: Not only the geologists, archaeologists have also found the bones of extinct animals in caves in the canyon walls. In a cave one hundred and forty feet above the river, they found drift wood that dated back as far as thirty-seven thousand years.

M: That means the river must have been a hundred and forty feet higher up when it carried the drift wood into the cave.

W: It's very possible, but of course who knows. The Great Canyon is full of mysteries. Wouldn't you like to go to Arizona some day?

M: You bet I would.

Where has the woman been?

A.To Colonado.

B.To Anzona.

C.To the Nile River.

D.To the Museum of Natural History.

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第3题

听力原文:M: It's good to see you back. How was your trip to Arizona? Did you see tile Grea
t Valley?

W: Yes, it was fantastic. Now I know why it is listed together with the Nile river as one of the great natural wonders of the world. Here, want to see the picture I took?

M: Oh, what a view! It is even bigger than I had imagined. I remember reading about the Great Valley and I think it said that it was formed suddenly when an earthquake took place.

W: Well, not that quickly. Look, the river has been wearing the valley floor away for ten million years.

M: Then the valley is the result of soil changes. I'll bet geologists have made some interesting discoveries there.

W: Not only the geologists, archaeologists have also found the bones of extinct animals in caves in the valley walls, ha a cave one hundred and forty feet 'about the river, they found driftwood that dated back as far as thirty seven thousand years.

M: That means the river must have been a hundred and forty feet higher up when it carried the driftwood into the cave.

W: It's very possible, but of course who knows. The Great Valley is full of mysteries. Wouldn't you like to go to Arizona some day?

M: You bet I would.

(23)

A.To Colorado.

B.To Arizona.

C.To the Nile River.

D.To the Museum of Natural History.

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第4题

听力原文:M: It's good to see you back. How was your trip to Arizona? Did you see the Grand
Canyon?

W: Yes, it was fantastic. Now I know why it is listed together with the Nile River as one of the great natural wonders of the world. Here, want to see the picture I took?

M: Oh, what a view! It is even bigger than I had imagined. I remember reading about the Grand Canyon and I think it said that it was formed suddenly when the earth's crust split open during an earthquake.

W: Well, not that quickly. Look, here is the picture of Colorado river. See way down at the bottom of the canyon, that fiver and its tributaries have been wearing the canyon floor away for ten million years.

M: Then the canyon is the result of swale erosion. I'll bet geologists have made some interesting discoveries here.

W: Not only the geologists, archaeologists have found the bones of extinct animals in caves in the canyon wails. In a cave one hundred and forty feet above the river, they found drift wood than dates back as far as thirty seven thousand years.

M: That means the river must have been a hundred and forty feet higher up when it carried the driftwood into the cave.

W: It's very possible, but of course who knows. The Grand Canyon is full of mysteries. Wouldn't you like to go to Arizona some day?

M: You bet I would.

(20)

A.To the Nile River.

B.To the museum of Natural History,

C.To Colorado.

D.To Arizona.

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第5题

听力原文:Your professor has asked me to talk to you today about the topic that should be o

听力原文: Your professor has asked me to talk to you today about the topic that should be of real concern to civil engineers: the erosion of the US beaches. Let me start with some statistics, Did you know that 90% of the coast in this country is eroding, on the gulf of Mexico for instance, erosion averages 4 to 5 feet per year? Over the past 20 years, there has been an increase in building along the coast, even though geologists and environmentalists have been warning communities about problems like erosion. Someway, communities have tried to protect their buildings and roads and to build seawalls. However, geologists have found that such stabilizing structures actually speed up the destruction of the beaches. These beaches with seawalls, called stabilized beaches, are much narrower than beaches without them. You may wonder how seawalls speed up beach loss. The explanation is simple. If the flow of the beaches is gentle, the water energy is lessened as it washes up along the shore. It is reduced even more that returns to the sea so it doesn't carry back much sand. On the other hand, when the water hits the nearly vertical face of the seawall, it goes straight back to the sea with the full force of its energy and it carries back a great deal of sand. Because of the real risk of losing beaches, many geologists support a ban on all types of stabilizing construction on shorelines.

(30)

A.To protect beachfront property.

B.To reduce the traffic on beach roads.

C.To provide privacy for homeowners.

D.To define property limits.

点击查看答案

第6题

Earthquakes are the most lethal of all natural disasters. What causes them? Geologists exp
lain them in terms of a theory known as plate tectonics. Continents are floating apart from each other, this is referred to as the continental drift. About sixty miles below the surface of the sea, there is a semimolten bed of rock over which plates, or slabs, carry continents and sea floors at a rate of several inches a year. As the plates separate from each other, a new sea floor is formed by the molten matter that was formerly beneath. Volcanic islands and large mountain ranges are created by this type of movement. The collision of plates causes geological instability such as that in California called the San Andreas Fault, located between the Pacific and North American plates. The plates there are constantly pushing and pulling adjacent plates, thereby creating constant tremors and a potential for earthquakes in the area.

Geologists would like to be able to predict earthquakes accurately. Using laser beams, seismographs, gravity-measuring devices, and radio telescopes, they are presently studying the San Andreas Fault to determine the rate of strain and the amount of ground slippage. Calculations indicate that sometime within the next ten years, California will be struck by a major earthquake.

In spite of the geologists' theory of plate tectonics, there are still gaps in man's understanding and knowledge of the causes of earthquakes. Powerful earthquakes have occurred in places where plate boundaries are hundreds of miles away. In the 1800s, New Madrid, Missouri and Charleston, South Carolina, were shaken by earthquakes that no one had foreseen.

Certain areas of the world are quake prone. Italy, Yugoslavia, and Algeria have experienced many quakes. In November 1980, Naples was struck by an especially devastating quake. China and Japan have also been hit by horrendous quakes. In 1923, Tokyo and Yokohama were reduced to rubble by gigantic tremors that were followed by fires, tornadoes, and finally a thirty-four-foot tsunami, or tidal wave, which was caused by the earth's drop into the waters of Tokyo Bay. More than 150,000 people died in that earthquake.

What effects have geologists' predictions of earthquakes had? The Chinese in Haicheng in 1974 were warned that an earthquake might occur within the next year or two. With the help of amateur seismologists' observations of animal behavior. and the rise and fall of water in wells and measurements of quantities of radioactive gas in water, professional geologists were able, in January 1975, to predict an earthquake within the next six months. On February 4, Haicheng was destroyed, but because its residents have been evacuated, very few people were killed. In California, where earthquake is an ever present menace, building codes now require quakeproof structures, and Civil Defense units have intensified their training in how to deal with disaster should it strike or, perhaps more accurately, when it strikes. Should predictions of a quake within the next ten years be accurate, many Californians may be able to save both their lives and their property.

Continental drift is the concept that ______.

A.continents are drawing nearer to each other

B.continents are separating

C.continents are 60 miles apart from each other

D.new continents are developing beneath the sea

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第7题

EarthquakeCan Scientists Predict Killer Earthquakes?The date was November 23,1980.People n

Earthquake

Can Scientists Predict Killer Earthquakes?

The date was November 23,1980.People near Naples,in Southern Italy,felt the earth roll and shake. Earthquake! Suddenly buildings came tumbling down. Cracks appeared in the earth.Within minutes,entire towns were destroyed.Thousands of people were dead.Thousands more were injured.

As rescuers searched through the rubble,many people must have wondered,if only the victims had known ahead of time,many lives could have been saved.

Actually,an Italian scientist did predict that such a quake would happen.In 1977 Dr.M.Caputo of the Universite Degiles Studi in Rome warned that a large quake would soon strike the east of Naples.Unfortunately,he couldn't predict the exact time and date of the quake.

Dr.Caputo made his general prediction after talking with scientists at 54 earthquake-monitoring stations throughout Italy.He learned that many earthquakes had recently rocked different areas around Naples.But none had occurred in one particular spot east of Naples for many years.Dr. Caputo felt that the area was long overdue for a large quake.And it was.

Earthquake Strikes in Gap

The quake occurred in a region that Dr.Caputo called a seismic gap.A seismic gap is an area in an active earthquake region where no earthquake or seismic activity has been recorded in a long time.Seismic gaps are located where two large plates in the earth have become stuck.

When the plates slide past each other,they sometimes became locked in place.A similar thing happens when you make a running leap on a sidewalk while wearing sneakers.When you 1and on both feet,the sneakers grab onto rough surface.Friction tends to hold your feet back while the rest of your body goes forward.You may end up falling flat on your face.

In the case of plates,however,the uneven surfaces between the plates cause the plates to remain locked in place for years.Huge pressure builds up behind each plate.Periodically,a shudder,or tremor,is recorded as some of this energy is released.

Finally,after about 50 years,rock in the seismic gap either suddenly breaks or moves under the great stress.This sudden release of energy sends shock waves through the rock layers above.The ground shakes,sidewalks crack,and buildings tumble.A mighty quake has struck.

Gaps Used to Predict Quakes

Many geologists have used what is called the seismic gap technique to accurately predict earthquakes.The technique was first developed by Soviet earthquake expert Dr.V.Fodotov during his studies of ancient and recent Japanese earthquakes.Dr.Fodotov was marking the location,size,and date of all known quakes in Japan when he noticed a striking pattern.

All major earthquakes were found to occur in only a few isolated spots in Japan.Each of these spots,he noted,experienced a major quake only once every 50 to 60 years.Dr.Fodotov concluded that spots that hadn't had a quake in more than 50 years were “ripe” for a quake.The Russian scientist named these locations seismic gaps.

In the past several years,geologists from other countries have found seismic gaps in other parts of the world.After making detailed studies of past quakes in these regions,the geologists were able to make an accurate prediction of when a quake would occur.

How Do Animals Know When an Earthquake Is Coming?

Scientists who try to predict earthquakes have gotten some new helpers recently-animals.

That's right,animals.Scientists have begun to catch on to what farmers have known for thousands of years.Animals often seem to know in advance that an earthquake is coming,and they show their fear by acting in strange ways.Before a Chinese quake in1975,snakes awoke from their winter sleep early only to freeze to death in the cold air.Cows broke their

A.no prediction had been made

B.no correct prediction had been made

C.no one had predicted the precise date

D.no one had cared about Dr.Caputo's prediction

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第8题

Standing on the rim of the Grand Canyon(大峡谷), gazing across this giant would in the Ear

Standing on the rim of the Grand Canyon(大峡谷), gazing across this giant would in the Earth's surface, a visitor might assume that the canyon had been caused by some ancient convulsing (震动). In fact, the events that produced the canyon, far from being sudden and catastrophic, simply add up to the slow and orderly process of erosion.

Many millions of years ago, the Colorado Plateau in the Grand Canyon area contained 1000 more feet of rock than it does today and was relatively level. The additional material consisted of some 14 layered formations of rock. In the Grand Canyon region these layers were largely worn away over the course of millions of years.

Approximately 65 million years ago the plateau's flat surface in the Grand Canyon area bulged upward from internal pressure, geologists refer to this bulging actions upwading(弯曲上升); it was followed by a general elevation of the whole Colorado Plateau, a process that is still going on. As the plateau gradually rose, shallow rivers that winded across it began to run more swiftly and cut more definite courses. One of these rivers, located east of the up- ward, was the ancestor of the Colorado. Another river system, called the Hualapai, flowing west of the upward, extended itself eastward by cutting back into the upward, it eventually connected with the ancient Colorado and captured its waters. The new river then began to carve out the 277-mile-long trench that eventually became the Grand Canyon. Geologists estimate that this initial cutting action began no earlier than 10 million years ago.

Since then, the Canyon forming has been cumulative. To the corrosive force of the river itself have been added other factors. Heat and cold, rain and snow, along with the varying resistance of the rocks, increase the opportunities for erosions, the Canyon walls crumble, the river acquires a cutting tool. Tons of debris, rainfall running off the high plateau creates feeder streams that carve side canyons. Pushing slowly backward into the. plateau, the side canyons expose new rocks, and the pattern of erosion continues.

The passage mainly discusses______.

A.patterns of erosion in different mountain ranges

B.forces that made the Grand Canyon

C.the increasing pollution of the Colorado River

D.the sudden appearance of the Grand Canyon

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第9题

Standing on the rim of the Grand Canyon, gazing across this giant would in the earth's sur
face, a visitor might assume that the canyon had been caused by some ancient convulsion. In fact, the events that produced the canyon, far from being sudden and cataclysmic, simply add up to the slow and orderly process of erosion.

Many millions of years ago the Colorado Plateau in the Grand Canyon area contained 10,000 more feet of rock than it does today and was relatively level. The additional material consisted of some 14 layered formations of rock. In the Grand Canyon region these layers were largely worn away over the course of millions of years.

Approximately 65 million years ago the plateau's flat surface in the Grand Canyon area bulged upward from internal pressure: geologists refer to this bulging action as upwarping; it was followed by a general elevation of the whole Colorado Plateau, a process that is still going on. As the plateau gradually rose, shallow rivers that meandered across it began to run more swiftly and cut more definite courses. One of these rivers located east of the upwarp, was the ancestor of the Colorado. Another river system called the Hualapai, flowing west of the upwarp, extended itself eastward by cutting back into the upwarp; it eventually connected with the ancient Colorado and captured its waters. The new river then began to carve out the 277-mile-long trench that eventually became the Grand Canyon. Geologists estimate that this initial cutting action began no earlier than 10 million years ago.

Since then the canyon forming has been cumulative. To the corrosive force of the river itself have been added other factors. Heat and cold, rain and snow, along with the varying resistance of the rocks, increase the opportunities for erosion. The canyon walls crumble; the river acquires a cutting tool, tons of debris; rainfall running off the high plateau creates feeder streams that carve side canyons. Pushing slowly backward into the plateau, the side canyons expose new rocks, and the pattern of erosion continues.

What does the passage mainly discuss?

A.Patterns of erosion in different mountain ranges.

B.Forces that made the Grand Canyon.

C.The increasing pollution of the Colorado River.

D.The sudden appearance of the Grand Canyon.

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第10题

【T4】A.HANDLE B.ON C.CONTINUED TO A.THE TREND WAS NATURALLY MOST OBVIOUS IN THOSE

【T4】

A.HANDLE

B.ON

C.CONTINUED TO A.THE TREND WAS NATURALLY MOST OBVIOUS IN THOSE AREAS OF SCIENCE BASED ESPECIALLY【T1】______A MATHEMATICAL OR LABORATORY TRAINING

B.AMATEURS, ON THE OTHER HAND, HAVE【T2】______PURSUE LOCAL STUDIES

C.ONE MAN COULD CONTINUE TO【T3】______THE INFORMATION SPECIALIZATION CAN BE SEEN AS A RESPONSE TO THE PROBLEM OF AN INCREASING ACCUMULATION OF SCIENTIFIC KNOWLEDG

E.BY SPLITTING UP THE SUBJECT MATTER INTO SMALLER UNITS,【T4】_____AND USE IT AS THE BASIS FOR FURTHER RESEARC

H.BUT SPECIALIZATION WAS ONLY ONEOF A SERIES OF RELATED DEVELOPMENTS IN SCIENCE AFFECTING THE PROCESS OF COMMUNICATIO

N.ANOTHER WAS THE GROWING PROFESSIONALISATION OF SCIENTIFIC ACTIVITY. NO CLEAR-CUT DISTINCTION CAN BE DRAWN BETWEEN PROFESSIONALS AND AMATEURS IN SCIENCE:EXCEPTIONS CAN BE FOUND TO ANY RUL

E.NEVERTHELESS, THE WORD "AMATEUR" DOES CARRY A CONNOTATION THAT THE PERSON CONCERNED IS NOT FULLY INTEGRATED INTO THE SCIENTIFIC COMMUNITY AND, IN PARTICULAR, MAY NOT FULLY SHARE ITS VALUES.THE GROWTH OF SPECIALIZATION IN THE NINETEENTH CENTURY, WITH ITS CONSEQUENT REQUIREMENT OF A LONGER, MORE COMPLEX TRAINING, IMPLIED GREATER PROBLEMS FOR AMATEUR PARTICIPATION IN SCIENC

E.【T5】______, AND CAN BE ILLUSTRATED IN TERMS OF THE DEVELOPMENT OF GEOLOGY IN THE UNITED KINGDO

M. A COMPARISON OF BRITISH GEOLOGICAL PUBLICATIONS OVER THE LAST CENTURY AND A HALF REVEALS NOT SIMPLY AN INCREASING EMPHASIS ON THE PRIMACY OF RESEARCH, BUT ALSO A CHANGING DEFINITION OF WHAT CONSTITUTES AN ACCEPTABLE RESEARCH PAPER.THUS, IN THE NINETEENTH CENTURY, LOCAL GEOLOGICAL STUDIES REPRESENTED WORTHWHILE RESEARCH IN THEIR OWN RIGHT; BUT, IN THE TWENTIETH CENTURY,LOCAL STUDIES HAVE INCREASINGLY BECOME ACCEPTABLE TO PROFESSIONALS ONLY IFTHEY INCORPORATE, AND REFLECT ON, THE WIDER GEOLOGICAL PICTUR

E.【T6】______ IN THEOLD WAY.THE OVERALL RESULT HAS BEEN TO MAKE ENTRANCE TO PROFESSIONAL GEOLOGICAL JOURNALS HARDER FOR AMATEURS, A RESULT THAT HAS BEEN REINFORCED BY THE WIDESPREAD INTRODUCTION OF REFEREEING, FIRST BY NATIONAL JOURNALS IN THE NINETEENTH CENTURY AND THEN BY SEVERAL LOCAL GEOLOGICAL JOURNALS IN THE TWENTIETH CENTURY.AS A LOGICAL CONSEQUENCE OF THIS DEVELOPMENT, SEPARATE JOURNALS HAVE NOW APPEARED AIMED MAINLY TOWARDS EITHER PROFESSIONAL OR AMATEUR READERSHIP.A RATHER SIMILAR PROCESS OF DIFFERENTIATION HAS LED TO PROFESSIONAL GEOLOGISTS COMING TOGETHER NATIONALLY WITHIN ONE OR TWO SPECIFIC SOCIETIES, WHEREAS THE AMATEURS HAVE TENDED EITHER TO REMAIN IN LOCAL SOCIETIES OR TO COME TOGETHER NATIONALLY IN A DIFFERENT WAY.

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