Passage 3

　　Natural Disasters

　　Earthquakes

　　When the Earth Moves

　　Earthquakes are caused by the motion of tectonic plates—individual sections that make up the Earth’s surface like panels on a football. Immense strain accumulates along fault lines where adjacent plates meet. When the rock separating the plates gives way, sudden seismic ground-shaking movement occurs.

　　Of course, if we want to know why earthquakes happen, we need to dig a little deeper.

　　Centre of the Earth

　　The Earth is made up of three main layers:

　　The core is at the centre of the Earth.

　　The mantle is a mobile semi-molten layer around the core.

　　The outer-shell of the Earth is called the crust. Scientists call this the lithosphere—it’s the part we’re on now.

　　The crust is made up of 12 individual tectonic plates. Below the sea, they can measure three to six miles (4km-9.6km) thick and under land this increases to 20-44 miles (32km-70.8km). Below the crust, radiation from the Earth’s core heats the semi-molten mantle to temperatures of over 5000°C.

　　All fluids when heated—even molten rock—are affected by a process called convection. That makes hot liquid rise to displace cooler liquid, creating a current. Tectonic plates effectively float on the mantle, like croutons in a bowl of super-heated soup. But these plates and constantly move due to the convection current.

　　Of course, they creep along very slowly—roughly the same speed your fingernails grow. Even at this sub snail-pace, the effects can be devastating. The combined annual force of earthquakes is equal to 100,000 times the power of the atomic bombs that flattened Hiroshima.

　　The point where the seismic activity occurs is the epicentre, where the earthquake is strongest. But it doesn’t always end there; seismic waves travel out from the epicentre, sometimes creating widespread destruction as they pass.

　　Volcanoes

　　Without doubt, erupting volcanoes are the most awesome and terrifying sights in nature. In fact, their untamed destructive firepower has shaped and influenced many ancient cultures from Pompeii, to Japan.

　　It’s estimated that one in ten of the World’s population live within “danger range” of volcanoes. According to the Smithsonian Institute, there are 1511 “active” volcanoes across the globe, and many more dormant ones that could recharge at any moment.

　　When tectonic plates collide，like earthquakes, volcanoes form at weak-points in the Earth’s crust, known as “fault-lines”.

　　When two tectonic plates collide, the event can provide the catalyst for volcanic activity. As one section slides on top of the other, the one beneath is pushed down into the mantle. Water trapped in the crust can cause reactions within the mantle. Why? Well, it’s thought that when the water mixes with the mantle, it lowers the mantle’s melting point, and the solid mantle melts to form a liquid, known as ‘magma’.

　　Under Increasing Pressure

　　Since liquid rock is less dense than solid rock, magma begins to rise through the Earth’s crust. It forces its way up, melting surrounding rock and increasing the amount of magma.

　　Magma only stops rising when the pressure from the rock layer above it becomes too great. It gathers below the Earth’s surface in a “magma chamber”.

　　When the pressure increases in the chamber, the crust finally gives way and magma spews out onto the Earth’s surface forming a volcano. When it reaches the surface, magma becomes known as “lava”.

　　Volcanic eruptions vary in intensity and appearance depending on two factors:

　　the amount of gas contained in the magma

　　its viscosity—how runny it is

　　In general, the explosive eruptions come from high gas levels and high viscosity in the magma. Whilst lava floes result from magmas with low gas levels and low viscosity.

　　Mount Etna

　　Over millions of years, lava and ash from eruptions might build up to form a mountainous volcano like Mt Etna in Italy.

　　Hurricanes

　　By definition, a hurricane is fierce rotating storm with an intense centre of low pressure that only happens in the tropics. In south-east Asia they’re known as typhoons and in the Indian Ocean, cyclones.

　　They cause high winds, huge waves, and heavy flooding. In 1998, Hurricane Gilbert produced 160mph winds, killing 318 people, and devastating Jamaica. A tropical storm can only be classified as a hurricane if it sustains wind speeds above 73mph or force 12 on the Beaufort Scale. Each year about 50 tropical storms reach hurricane status.

　　One of the most powerful of all weather systems, hurricanes are powered by the heat energy released by the condensation of water vapour. However, the conditions have to be exact for a hurricane to form, with the sea’s surface temperature being above 26.5°C.

　　How Hurricanes Happen

　　Air above warm tropical water rises quickly as it is heated by the sea. As the air rises it rotates or spins creating an area of low pressure, known as the eye of the storm. The eye can be clearly seen on satellite pictures, and is usually eerily calm.

　　The hurricane only moves slowly at speeds of 20-25mph bringing torrential rain and thunderstorms and very strong winds. However, they also cause flooding on low lying coastlines with a phenomenon known as a “storm surge”.

　　Storm Surge

　　This is caused by the intense low pressure at the eye of a hurricane, combining with the effect of strong winds. The sea rises 1cm for every millibar of pressure - if the pressure is 930 millibar, the sea surge will be about 80 cm. Hurricanes can raise the seas surface by as much as 4m.

　　The hurricane winds push the surge along in front of its path. When this surge hits low-lying coasts, the effects can be devastating. In addition to the sea surge, flooding can also result from torrential rain falling from the storm clouds.

　　Once it reaches the mainland, a hurricane may cause widespread damage for a few days, but with no warm water to supply heat, they quickly die out.

　　1. Earthquakes are caused by the motion of tectonic plates that make up the Earth’s surface.

　　2. The Earth is made up of four main layers: the core, the mantle, the crust and the magma.

　　3. It is the convection that make hot liquid rise to displace cooler liquid, creating a current.

　　4. The earthquake at the epicenter is weakest.

　　5. Both of volcanoes and earthquakes form at weak-points in the Earth’s crust when tectonic plates collide,.

　　6. Magma will fall through the Earth’s crust if the liquid rock is less dense than solid rock.

　　7. Mt Etna in Italy produced 160mph winds and killed 296 people in 2000.

　　8. A hurricane is defined as a fierce rotating storm with an intense centre of low pressure that_______.

　　9. Torrential rain, __________ are always brought by the hurricane.

　　10. If there is no warm water to supply heat, the hurricane will______.

　答案解析

　　1. Y. 根据题干中的信息词motion of tectonic plates定位到第一个小标题下的第一句话可知题干表述与原文相符。

　　2. N. 根据题干中的信息词made up和layers定位到第二个小标题下的第一段可知题干表述错误。地球从内到外由三层组成：地核、地幔、地壳。

　　3. Y. 根据题干中的信息词convection定位到第二个小标题下的第三段前两句话可知题干表述与原文相符。

　　4. N. 根据题干中的信息词epicenter定位到第二个小标题下第五段的第一句话，可知题干表述与原文相反。

　　5. Y. 根据题干中的信息词volcanoes和tectonic plates collide定位到第三个小标题下的第三段可知题干表述与原文相符。

　　6. N. 根据题干中的信息词Magma和Earth’s crust if the liquid rock定位到第四个小标题下的第一句话可知题干表述与原文相反。

　　7. NG. 根据题干中的信息词Mt Etna和160mph winds定位到第五个小标题和第六个小标题的第二段第二句话，可知原文并没有提到意大利埃特那火山的具体影响。

　　8. only happens in the tropics。 根据题干中的信息词fierce rotating storm及intense centre of low pressure定位到第六个小标题下的第一句话可得答案。

　　9. thunderstorms and strong winds。根据题干中的信息词brought by the hurricane定位到倒数第二个小标题下的最后一段可得答案。

　　10. quickly die out。根据题干中的信息词no warm water定位到原文的最后一句话可得知道答案。