原版英语RAZ 教案Q10-Earthquakes, Volcanoes, and Tsunamis (3).pdf
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1、www.readinga-Visit www.readinga- for thousands of books and materials.LEVELED BOOK QQTWWritten by Elizabeth AustinEarthquakes,Volcanoes,and TsunamisA Reading AZ Level Q Leveled BookWord Count:749Earthquakes,Volcanoes,and Tsunamiswww.readinga-Written by Elizabeth AustinEarthquakes,Volcanoes,and Tsuna
2、misLevel Q Leveled Book Learning AZWritten by Elizabeth AustinIllustrated by Craig FrederickAll 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 Divis
3、ion LC-USZ62-55720;page 9:Boris Grdanoski/AP Images;page 11:StockTrek/Photodisc/GettyImages;15:Roger Ressmeyer/Corbis;page 16:Marshall Myrman/Corbis;page 19:Harry Yeh,University of Washington;page 20:Eric Skitzi/AP ImagesEarthquakes,Volcanoes,and TsunamisCorrelationLEVEL QN3030Fountas&PinnellReading
4、 RecoveryDRA34Table of ContentsIntroduction.4Deep Within the Earth .5Earthquakes:Terrible Trembling.7The Richter Scale.10Volcanoes:Enormous Explosions.11Tsunamis:Wild Waves .16Conclusion .21Glossary .22IntroductionThe ground and the ocean are usually peaceful.But forces deep within the earth can sud
5、denly cause earthquakes,volcanoes,and tsunamis(tsoo-NOM-ees).In this book,you will read about these events and the forces that cause them.Smoke rises from what seems to be a peaceful volcano.Earthquakes,Volcanoes,and Tsunamis Level Q34Table of ContentsIntroduction.4Deep Within the Earth .5Earthquake
6、s:Terrible Trembling.7The Richter Scale.10Volcanoes:Enormous Explosions.11Tsunamis:Wild Waves .16Conclusion .21Glossary .22IntroductionThe ground and the ocean are usually peaceful.But forces deep within the earth can suddenly cause earthquakes,volcanoes,and tsunamis(tsoo-NOM-ees).In this book,you w
7、ill read about these events and the forces that cause them.Smoke rises from what seems to be a peaceful volcano.Earthquakes,Volcanoes,and Tsunamis Level Q56Deep Within the EarthThe 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
8、 continents and ocean floors.Where the plates come together,there are often cracks and gaps,called faults.Underneath the plates,the Earth is 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 ar
9、ound with it.At the edges of the moving plates,three different things can happen.If the plates are moving against each other,one plate slides 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 apar
10、t,they make a gap where magma comes out(Fig.3).MAGMAThe dotted lines show the edges of the plates.PacificPlateAustralianPlateIndianPlateEurasianPlateNazcaPlateSouth AmericanPlateNorth AmericanPlateAfricanPlateAntarcticPlatePacificPlateScotia PlateEQUATORTectonic PlatesMAGMAMAGMAMountainsFig.1Fig.2Fi
11、g.3Earthquakes,Volcanoes,and Tsunamis Level Q56Deep Within the EarthThe 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 plates come together,there are often cracks and gaps,called faults.Und
12、erneath the plates,the Earth is 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 aga
13、inst each other,one plate slides 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 comes out(Fig.3).MAGMAThe dotted lines show the edges of the plates.PacificPlat
14、eAustralianPlateIndianPlateEurasianPlateNazcaPlateSouth AmericanPlateNorth AmericanPlateAfricanPlateAntarcticPlatePacificPlateScotia PlateEQUATORTectonic PlatesMAGMAMAGMAMountainsFig.1Fig.2Fig.3Earthquakes,Volcanoes,and Tsunamis Level Q78Earthquakes:Terrible TremblingSometimes the plates get caught
15、on each other and cannot move.The pressure and energy build up.Then,suddenly,the rocks give way.The ground shakes.Far above,people feel an earthquake.The ground here was ripped open by an earthquake.Earthquakes can damage or even destroy buildings.Some earthquakes are small and harmless.But sometime
16、s the shaking is so strong that buildings crumble,bridges collapse,and large cracks open in the ground.Earthquakes,Volcanoes,and Tsunamis Level Q78Earthquakes:Terrible TremblingSometimes the plates get caught on each other and cannot move.The pressure and energy build up.Then,suddenly,the rocks give
17、 way.The ground shakes.Far above,people feel an earthquake.The ground here was ripped open by an earthquake.Earthquakes can damage or even destroy buildings.Some earthquakes are small and harmless.But sometimes the shaking is so strong that buildings crumble,bridges collapse,and large cracks open in
18、 the ground.Earthquakes,Volcanoes,and Tsunamis Level Q910We 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,depending on its strength.A seismographThe Richter Scale1 People cannot feel the eart
19、hquakeonly sensitive instruments 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.Wate
20、r sloshes in swimming pools.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 v
21、ery major earthquake.Most 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 b
22、e thrown into the air.Total destruction of buildings and other structures.There is no top to the Richter scale,but the strongest earthquake ever recorded was a 9.5.Earthquakes,Volcanoes,and Tsunamis Level Q910We measure the strength of earthquakes on an instrument called a seismograph(SIZE-moh-graf)
23、.Each earthquake is given a number from the Richter(RICK-ter)scale,depending on its strength.A seismographThe Richter Scale1 People cannot feel the earthquakeonly sensitive instruments can detect it.2 People usually do not feel it;some people in tall buildings may sense a slight swaying.3 Many peopl
24、e 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 pools.Some weak buildings may be damaged.5 Felt over a wider area.Usually lots of damage to weak buildings at and around cente
25、r.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.Most buildings at the center are destroyed.Cracks form in the Earth.Underground pipes break.Large landslides can occur.8 Buildi
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