原版英语RAZ 教案(T) Earthquakes, Volcanoes, and Tsunamis.pdf
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1、www.readinga-LEVELED READER ALEVELED BOOK TWritten by Elizabeth AustinEarthquakes,Volcanoes,and TsunamisQTWVisit www.readinga- for thousands of books and materials.Earthquakes,Volcanoes,and TsunamisA Reading AZ Level T Leveled BookWord Count:1,449Earthquakes,Volcanoes,and TsunamisLevel T Leveled Boo
2、k Learning AZWritten by Elizabeth AustinAll rights reserved.www.readinga-Photo Credits:Front cover,page 4:Photodisc/Getty Images;back cover,title page,pages 7,13(all),14,17,21:ArtToday;page 8:courtesy of Library of Congress,Prints&Photographs Division LC-USZ62-55720;page 9:Boris Grdanoski/AP Images;
3、page 11:StockTrek/Photodisc/GettyImages;page 15:Roger Ressmeyer/Corbis/VCG/Corbis Documentary/Getty Images;page 16:Marshall Myrman/Corbis;page 19:Harry Yeh,University of Washington;page 20:Eric Skitzi/AP ImagesCorrelationLEVEL TP3838Fountas&PinnellReading RecoveryDRAwww.readinga-Earthquakes,Volcanoe
4、s,and TsunamisWritten by Elizabeth AustinEarthquakes,Volcanoes,and Tsunamis Level T 34Table of ContentsIntroduction.4Deep Within the Earth .5Earthquakes:Terrible Trembling.7The Richter Scale.10Volcanoes:Enormous Explosions.11Tsunamis:Wild Waves .16Conclusion .21Glossary .22IntroductionWe usually thi
5、nk of the ground and the ocean as peaceful things.The ground lies quietly beneath our feet,and the ocean laps gently against the shore.But forces deep within the Earth can suddenly destroy that peacefulness.These forces cause violent shakings called earthquakes;explosions of ash,gases,and hot rocks
6、called volcanoes;and huge waves called tsunamis(tsoo-NOM-ees).In this book,you will read about these amazing events and the forces that cause them to happen.Smoke rises from what seems to be a peaceful volcano.Earthquakes,Volcanoes,and Tsunamis Level T 56PacificPlateUnderneath the plates,the Earth i
7、s very hot.It is so hot that rock melts into a liquid called magma.The plates float on top of this liquid magma.The magma is always moving,dragging the plates around with it.At the edges of the moving plates,three different things can happen.If the plates are moving against each other,one plate slid
8、es over or under the other plate(Fig.1).If the plates are moving past each other,the edges of the plates grind together(Fig.2).And if the plates are moving apart,they make a gap where magma seeps out(Fig.3).MountainsMagmaMagmaMagmaFig.1Fig.2Fig.3MountainsDeep Within the EarthBeneath the soil,rock,an
9、d water on the surface of our planet,the Earth is constantly changing.The top layer of Earth is made of giant pieces of rock,like the pieces of a puzzle.The pieces of rock,called plates,make up continents and ocean floors.Where the edges of the plates come together,there are often cracks and gaps,ca
10、lled faults.The dotted lines show the edges of the plates.Tectonic PlatesPacificPlateAustralianPlateIndianPlateEurasianPlateNazcaPlateSouth AmericanPlateNorth AmericanPlateAfricanPlateAntarcticPlateScotia PlateEQUATOREarthquakes,Volcanoes,and Tsunamis Level T 78Earthquakes:Terrible TremblingThe plat
11、es usually move very slowly.But sometimes large pieces of the plates get caught.The plates keep trying to move,but these large blocks of rock hold them back.The pressure and energy build up.Then,suddenly,the rocks give way,releasing all that pressure and energy.The plates jerk forward,and the ground
12、 shakes.Far above,on the surface,people feel an earthquake.Earthquakes can damage or even destroy buildings.In a small earthquake,the ground shakes a little,causing some hanging objects to swing.Tree branches sway,as if there were a gentle breeze.Some earthquakes are so small that we do not notice t
13、hem.But sometimes the shaking is so strong that buildings crumble,bridges collapse,and large cracks open in the ground over large areas.The ground here was ripped open by an earthquake.Earthquakes,Volcanoes,and Tsunamis Level T 910The Richter Scale1 People cannot feel the earthquakeonly sensitive in
14、struments can detect it.2 People usually do not feel it;some people in tall buildings may sense a slight swaying.3 Many people near the origin of the earthquake notice the shaking.No damage occurs.4 People at the origin of the quake definitely feel it.Hanging objects sway.Water sloshes in swimming p
15、ools.Some weak buildings may be damaged.5 Felt over a wider area.Usually lots of damage to weak buildings at and around center.Some damage to strong buildings.6 Lots of damage to weak buildings;some damage to strong buildings.Damage can spread over 160 kilometers(100 mi).7 A very major earthquake.Mo
16、st buildings at the center are destroyed.Cracks form in the Earth.Underground pipes break.Large landslides can occur.8 Buildings and bridges destroyed.Large cracks appear in the ground.Large landslides.9 The ground appears to move in“waves.”Entire rivers may move.Objects can be thrown into the air.T
17、otal destruction of buildings and other structures.There is no top to the Richter scale,but the strongest earthquake ever recorded was a 9.5.We measure the strength of earthquakes on an instrument called a seismograph(SIZE-moh-graf).Each earthquake is given a number from the Richter(RICK-ter)scale d
18、epending on its strength.You can look at the chart on the next page to learn what the different strengths of earthquakes feel like.For each number on the Richter scale,an earthquake is ten times as strong as the previous number.A 6.0 earthquake is ten times as strong as a 5.0 earthquake.It is one hu
19、ndred times as strong as a 4.0 earthquake!The largest earthquake ever recorded measured 9.5 on the Richter scale.It occurred on the coast of the South American country of Chile.Scientists are still learning about these dangerous events.One day,they may be able to warn people before earthquakes occur
20、.A seismographEarthquakes,Volcanoes,and Tsunamis Level T 1112Volcanoes:Enormous ExplosionsA volcano occurs wherever magma from deep inside the Earth comes out through a crack in the surface.Volcanoes usually happen near the edges of the plates,where there are many cracks and thin spots where the mag
21、ma can leak out.When the magma pours onto the surface,it hardens,often piling up into a mountain.Sometimes,the liquid rock flows peacefully out across the land.This is how many of the active volcanoes on the Hawaiian Islands behave.Runny liquid rock on this Hawaiian volcano flows smoothly,like a pea
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