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(单词翻译:双击或拖选)
Earth's Surfaces Are Always Moving 地球表面一直在运动
From VOA Learning English, this is Science in the News.
I’m Anna Matteo.
And I’m Christopher Cruise.
Scientists who study the Earth tell us the continents and ocean floors are always moving. This movement sometimes can be violent, causing death and destruction. Today, we examine what causes earthquakes and volcanic1 activity.
The first pictures of Earth taken from space showed a solid ball covered by brown and green landmasses and blue-green oceans. It appeared as if the Earth had always looked that way -- and always would.
Yet the surface of the Earth is not as solid or as permanent as had been thought. Scientists found that the surface of our planet is always in motion. Continents move about the Earth like huge ships at sea, floating on pieces of the Earth’s outer skin, or crust. New crust is created as melted rock pushes up from inside the planet. Old crust is destroyed as it moves toward the hot rock and melts.
In the 20th century, scientists began to understand that the Earth is a great, living and moving structure. Some experts say this understanding is one of the most important revolutions in scientific thought.
The knowledge of the Earth’s continual motion is based on the work of scientists who study the movement of the continents. This process is called “plate tectonics.” Earthquakes and volcanic activity are a result of that process.
Scientists say the surface of the Earth is cracked like a huge eggshell. They call these pieces “tectonic plates.” As many as 20 such plates cover the Earth. They sometimes hit each other, and sometimes move away from each other. Because some continents are above two plates, the continents move when the plates do.
The movement of tectonic plates can cause earthquakes and volcanoes. Understanding this movement can help predict where earthquakes will take place. Research shows that about 90 percent of all earthquakes happen along a few lines in several places around the Earth. These lines follow underwater mountains, where hot liquid rock flows up from deep inside the Earth. Sometimes, the melted rock comes out with a great burst of pressure. This forces apart pieces of the Earth’s surface in a violent earthquake.
Some earthquakes take place at the edges of continents. Pressure increases as two plates move against each other. When this happens, one plate moves past the other, suddenly causing the Earth’s surface to split open.
One example of this pressure is found on the west coast of the United States. Part of California is on what is known as the Pacific plate. The other part of the state is on what is known as the North American plate.
Scientists say the Pacific plate is moving toward the northwest, while the North American plate is moving toward the southeast. These two huge plates come together at what is called a fault line. This line between the plates in California is called the San Andreas Fault. It is along or near this fault line that most of California’s earthquakes take place, as the two tectonic plates move in different directions.
The city of Los Angeles is about 50 kilometers from the San Andreas Fault. Many smaller fault lines can be found throughout the Los Angeles area.
Scientists began making major discoveries about plate tectonics in the 20th century. One of those scientists was Alfred Wegener of Germany. One hundred years ago, he proposed that the continents had moved and were still moving.
Mr. Wegener said the idea came to him when he saw that the coasts of South America and Africa fit together like two pieces of a puzzle. He suspected that the two continents might have once been one, and then split apart.
He believed the continents had once been part of a huge area of land that he called “Pangaea.” He said the huge continent had split more than 200 million years ago. And, he said the pieces were still floating apart.
Alfred Wegener investigated the idea that continents move. He noted2 that a line of mountains that appears from east to west in South Africa looks almost exactly the same as a line of mountains in Argentina -- on the other side of the Atlantic Ocean. He found fossil remains3 of the same plant in parts of Africa, South America, India, Australia and even Antarctica.
Mr. Wegener said the mountains and fossils were evidence that all the land on Earth was united at some time in the distant past.
Mr. Wegener also noted differences between the continents and the ocean floor. He said the oceans were more than just low places that had filled with water. Even if the water
was removed, he said, a person would still see differences between the continents and the ocean floor.
Also, the continents and the ocean floor are not made of the same kind of rock.
The continents are made of a granite4-like rock. Granite is made when hot, liquid rock cools and hardens under the Earth’s surface. The ocean floor is basalt rock, a mixture of silicon5 and magnesium6.
The German scientist said the lighter7 continental8 rock floated up through the heavier basalt rock of the ocean floor.
Support for Mr. Wegener’s ideas did not come until the 1950s. Two American scientists found that the continents moved as new sea floor was created under the Atlantic Ocean. Harry9 Hess and Robert Dietz said a thin valley in the Atlantic was a place where the ocean floor splits. They said hot melted material flows up from deep inside the Earth through the split. As the hot material reaches the ocean floor, it spreads out, cools and hardens. It becomes new ocean floor.
The Americans proposed that the floor of the Atlantic Ocean is moving away from each side of the split and expanding. The movement is very slow -- a few centimeters a year. In time, they said, the moving ocean floor is blocked when it comes up against the edge of a continent. Then it is forced down under the continent, deep into the Earth, where it is melted again. Harry Hess said the Pacific Ocean was getting smaller.
He and Robert Dietz said this spreading does not make the Earth bigger. As new ocean floor is created, an equal amount is destroyed.
The two scientists said Alfred Wegener was correct. The continents do move as new material from the center of the Earth rises, hardens and pushes older pieces of the Earth away from each other.
They called their theory “sea floor spreading.” The theory explains that as the sea floor spreads, the tectonic plates are pushed and pulled in different directions.
New research also supports Mr. Wegener’s ideas. Scientists in Britain recently reported that large amounts of water may be trapped under the ocean plates near northern Japan. Their findings were published in the journal Geology.
A strong earthquake hit Japan in March of 2011. The quake and resulting tsunami10 waves killed almost 16,000 people. A team of researchers from the University of Liverpool studied the tectonic plates in the area where the earthquake took place. Their report says that when two plates meet, one may bend and end up underneath11 the other. During this process, it says, ocean water gets trapped below the plates and goes down past the Earth’s crust to its mantle12.
The researchers said a large hole lies near the fault lines in Japan. They said the hole could be as much as 150 kilometers deep. Water gets carried down the hole. The report says there could be 3? times more water in the Earth’s mantle than there is in all the oceans.
The idea of plate tectonics explains both volcanoes and earthquakes. Many of the world’s volcanoes are found at the edges of plates. The large number of volcanoes around the Pacific plate has earned this area the name “Ring of Fire.”
Volcanoes are also found in the middle of plates, where there is a well of melted rock. Scientists call these wells “hot spots.” A hot spot does not move. However, as the plate moves over it, a line of volcanoes is formed.
The Hawaiian Islands were created in the Pacific Ocean as the plate moved slowly over a hot spot. This process is continuing, as the plate continues to move.
Similar to earthquakes, volcanos can cause destruction and displace populations. Because of this, scientists are also hoping to learn more about volcanic activity.
Recently, the United States National Science Foundation provided financial support for research on volcanos. Geoscientists from the University of Oregon and the University of California Davis studied Mt. Hood13 in Oregon.
The scientists say that volcanos become active when the rock or magma inside becomes as hot as 750 degrees Celsius14. The volcano becomes active when the hot magma from the Earth’s crust rises and meets cooler solid magma. This can happen in as little as a few months’ time.
The American scientists believe the magma at Mt. Hood had been stored in the volcano for at least 20,000 years, or even as long as 100,000 years. They say that modern technology should be able to sense when the magma is getting warmer, and could possibly explode. This could prevent disasters when volcanos erupt around the world.
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volcanic
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| adj.火山的；象火山的；由火山引起的 | |
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noted
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| adj.著名的，知名的 | |
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remains
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| n.剩余物，残留物；遗体，遗迹 | |
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granite
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| adj.花岗岩，花岗石 | |
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silicon
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| n.硅(旧名矽) | |
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magnesium
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| n.镁 | |
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lighter
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| n.打火机，点火器；驳船；v.用驳船运送；light的比较级 | |
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continental
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| adj.大陆的，大陆性的，欧洲大陆的 | |
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harry
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| vt.掠夺，蹂躏，使苦恼 | |
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tsunami
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| n.海啸 | |
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underneath
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| adj.在...下面，在...底下；adv.在下面 | |
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mantle
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| n.斗篷，覆罩之物，罩子；v.罩住，覆盖，脸红 | |
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hood
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| n.头巾，兜帽，覆盖；v.罩上，以头巾覆盖 | |
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Celsius
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| adj.摄氏温度计的，摄氏的 | |
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