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Environmental Problems, Their Causes, and Sustainability 1

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cant (less than 4.0 on the Richter scale), minor (4.0–4.9),damaging (5.0–5.9), destructive (6.0–6.9), major (7.0–7.9),<strong>and</strong> great (over 8.0).Earthquakes often have aftershocks that graduallydecrease in frequency over a period of up to severalmonths, <strong>and</strong> some have foreshocks from seconds toweeks before the main shock.The primary effects of earthquakes include shaking<strong>and</strong> sometimes a permanent vertical or horizontal displacementof the ground. These effects may have seriousconsequences for people <strong>and</strong> for buildings,bridges, freeway overpasses, dams, <strong>and</strong> pipelines. Anearthquake is a very large rock-<strong>and</strong>-roll event.Secondary effects of earthquakes include rockslides,urban fires, <strong>and</strong> flooding caused by subsidence(sinking) of l<strong>and</strong>. Coastal areas can be severely damagedby earthquakes at sea that can generate hugewater waves, called tsunamis (also called tidal waves,although they have nothing to do with tides) thattravel as fast as 950 kilometers (590 miles) per hour.You cannot outrun one of these waves.One way to reduce loss of life <strong>and</strong> property fromearthquakes is to examine historical records <strong>and</strong> makegeologic measurements to locate active fault zones. Wecan also map high-risk areas (Figure 16-7), establishbuilding codes that regulate the placement <strong>and</strong> designof buildings in areas of high risk, <strong>and</strong> increase researchon projecting when <strong>and</strong> where earthquakes will occur.Then people can decide how high the risk might be<strong>and</strong> whether they want to accept the risk <strong>and</strong> live inareas subject to earthquakes.Engineers know how to make homes, large buildings,bridges, <strong>and</strong> freeways more earthquake resistant.But this can be expensive, especially the reinforcementof existing structures.Liquefaction ofrecent sedimentscauses buildingsto sinkL<strong>and</strong>slides mayoccur onhilly groundShockwavesEpicenterFocusTwo adjoining platesmove laterally alongthe fault lineEarth movementscause flooding inlow-lying areasFigure 16-6 Major features <strong>and</strong> effects of an earthquake.CanadaUnited StatesNo damage expectedMinimal damageModerate damageSevere damageFigure 16-7 Expected damage from earthquakes in Canada<strong>and</strong> the contiguous United States. This map is based on earthquakerecords. (U.S. Geological Survey)What Are Volcanoes? Popping an EarthCorkSome volcanoes erupt quietly <strong>and</strong> release flowsof molten rock but others erupt explosively <strong>and</strong>spew large chunks of lava rock, ash, <strong>and</strong> harmfulgases into the atmosphere.An active volcano occurs where magma (molten rock)reaches the earth’s surface through a central vent or along crack (fissure; Figure 16-8, p. 338). Volcanic activitycan release ejecta (debris ranging from large chunksof lava rock to ash that may be glowing hot), liquidlava, <strong>and</strong> gases (such as water vapor, carbon dioxide,<strong>and</strong> sulfur dioxide) into the environment.Volcanic activity is concentrated for the most partin the same areas as seismic activity. Some volcanoeserupt explosively <strong>and</strong> eject large quantities of gases <strong>and</strong>particulate matter (soot <strong>and</strong> mineral ash) high into thetroposphere. Most of the particles of soot <strong>and</strong> ash soonfall back to the earth’s surface. But gases such as sulfurdioxide remain in the atmosphere <strong>and</strong> are converted totiny droplets of sulfuric acid, many of which stay abovethe clouds <strong>and</strong> may not be washed out by rain for up to3 years. These tiny droplets reflect some of the sun’s energy<strong>and</strong> can cool the atmosphere for 1–4 years.http://biology.brookscole.com/miller14337

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