Use Dynamic Media To Bring Earth Science To Life - Pearson

3y ago
15 Views
2 Downloads
6.79 MB
35 Pages
Last View : 15d ago
Last Download : 2m ago
Upload by : Kairi Hasson
Transcription

Use Dynamic Media to BringEarth Science to LifeA01 TARB3536 15 SE FM.indd 14/28/17 2:33 PM

Bring Field Experience toStudents’ Fingertips.How to download a QR Code Reader1700 ftUsing a smartphone, students are encouraged to downloada QR Code reader app from Google Play or the Apple AppStore. Many are available for free. Once downloaded, students open the app and point the camera to a QRCode. Once scanned, they’re prompted to open the url to immediately be connected to the digital world and deepentheir learning experience with the printed text.Shiprock, New Mexico, is a volcanic neck composedof igneous rock that solidified in the conduit of a volcano.SmartFigure 6.26 Volcanic neckShiprock, New Mexico, is a volcanic neck thatstands about 520 meters (1700 feet) high. Itconsists of igneous rock that crystallized inthe vent of a volcano that has long since beeneroded. (Photo by Dennis Tasa)TUTORIALhttps://goo.gl/TjW5uhNEW! QR Codes link to SmartFiguresQuick Response (QR) codes link to over 238 videos and animations, giving readers immediate access to five typesof dynamic media: Project Condor Quadcopter Videos,Mobile Field Trips, Tutorials, Animations, and Videos tohelp visualize physical processes and concepts. S martFiguresextend the print book to bring Earth Science to life.NEW! SmartFigures: Project Condor Quadcopter VideosBringing Earth Science to life for students, three geologists, using a quadcopter-mounted GoPro camera,have ventured into the field to film 10 key geologiclocations and processes. These process-oriented videos,accessed through QR codes, are designed to bringthe field to the classroom and improve the learning experience within the text.A01 TARB3536 15 SE FM.indd 24/28/17 2:33 PM

.with SmartFiguresNEW! SmartFigures: Mobile Field TripsOn each trip, students will accompany geologist pilot-photographer Michael Collier in the airand on the ground to visit and learn about iconic landscapes that relate to discussions in the chapter.These extraordinary field trips are accessed by usingQR codes throughout the text. New Mobile FieldTrips for the 15th edition include Formation of aWater Gap, Ice Sculpts Yosemite, Fire and Ice Land,Dendrochronology, and Desert Geomorphology.NEW! SmartFigures: AnimationsBrief animations created by text illustrator DennisTasa animate a process or concept depicted in the textbook’s figures. With QR codes, students are given aview of moving figures rather than static art to depicthow geologic processes move throughout time.HALLMARK! SmartFigures: TutorialsThese brief tutorial videos present the student with a 3- to 4-minute feature (minilesson), most narrated and annotated by Professor Callan Bentley. Each lesson examines and explains the concepts illustrated bythe figure. With over 150 SmartFigureTutorials inside the text, students have amultitude of ways to enjoy art that teaches.A01 TARB3536 15 SE FM.indd 34/28/17 2:33 PM

180Earth ScienceThis photo shows the February 3, 2015, eruption of Mount Sinabung in NorthSumatra, Indonesia. Before awaking in 2010, Mount Sinabung had beendormant since 1600. In recent years it has erupted several times, resulting inthe evacuation of more than 30,000 people and at least 23 deaths.Each chapter in this 15th edition begins with FocusConcepts:ofpumice-ladenlearningthat correspond to theQUESTIONon1Whatname is given toathesetash- andcloudobjectivesthatis racing down this volcano?chapter’s major sections. By identifying key knowledge and skills, these objectives help students prioritize the material.QUESTION 2What type of volcano is associated with these destructiveEach major section concludes with Concept Checksso that students can check their learning. Three end-of-chaptereruptions?features continue the learning path. Concepts in Review are coordinated with the Focus on Concepts at the beginningof the chapter and with the numbered sections within the chapter, providing a readable and concise overview of keyFortunately, the pilots were able to dive to a lower altiEffects of Volcanic Ash and Gases on Weather andideas, with photos, diagrams, and questions. The questionsand problems in Give It SomeThought and Examining thetude and restart the engines, which allowed them toClimate Volcanic eruptions can eject dust-sized parland thinkingthe aircraft in Anchorage.ticles of volcanicandash andapplysulfur dioxidehigh into theEarth System challenge learners by requiring higher safelyorderskills to analyze, synthesize,thegasmaterial.(Photo by Ulet Ifansasti/Getty Images)Clear Learning Pathin EachChaptereYe ON earth6.1More recently, the 2010 eruption of Iceland’s Eyjafjallajökull Volcano sent ash high into the atmosphere. Thisthick plume of ash drifted over Europe, causing airlines allacross Europe to cancel thousands of flights and leavinghundreds of thousands of travelers stranded. Several weekspassed before air travel resumed its normal schedule.Volcanoesandis not the only problem. Ash canEngine cloggingdamageaircraft’s fuselage and pit the windshields ofOther anIgneousthepilot’s cabin. In addition, ash has been known to coatActivitya plane to the point that it becomes tail-heavy.atmosphere. The ash particles reflect sunlight back tospace, producing temporary atmospheric cooling. The1783 Laki eruptions in Iceland appear to have affectedatmospheric circulation around the globe. Drought conditions prevailed in the Nile River valley and in India,and the winter of 1784 saw the longest period of below2) Each chapter sectionzero temperatures in New England’s history.Othereruptions thatwithhave producedsignificantconcludesConcepteffects on climate worldwide include the eruption ofChecks, a set of questionsIndonesia’s Mount Tambora in 1815, which producedFocus on conceptsthatis atiedto(1816),the andsection’sthe “yearwithoutsummer”the eruptionVolcanicGases and Respiratory Health One of theof El Chichón in Mexico in 1982. El Chichón’s erup6.1learningobjectivesandmost destructive volcanic events, called the Laki eruption, although small, emitted an unusually large quantityChapter6 tortions,began along a large fissure in southern Iceland inof sulfurallowsdioxide thatreactedwatervaporthe Activity6.31783. pheretoproduceadensecloudoftinysulfuricvolcanoes, calderas form slowly as lava drains from the magma salticwere Onreleased,alongwith 130millionbeneath lavasthe volcano.a compositevolcano,calderacollapse oftenacid droplets.particles,aerosols,take several6.11 PartialMeltingandthe Originof Magma6.5explosiveeruptioncan resultgases.in significantand tofactsandideas.tons oss of lifeyearssettle outof theatmosphere.Likefine ash,theseSummarizethemajorprocesses thatgeneratemagmafrom solid rock.6.6destruction of property.sulfur Fissuredioxideeruptionsis ng,geothermalgradient,decompression meltingoccasionally produce massive floods of fluid basaltic6.7 lungstoproducesulfuricacid, to space.rock maymelt undergeologic circumstances: when heat Solidsolarlavafrom largecracks, calledthe crust.Layerupon layerby reflecting6.8is added to the rock, raising its temperature; when already hot rockthese floodbasalts mayaccumulatesignificantthicknesses andhalfofofIceland’slivestockdied,and thetoensuingfamine6.9experiences lower pressures (decompression, as seen at orthwesternUnitedkilled25 percent of the island’s human population.concept6.8is added (as occurs at subduction zones).6.10ridges);checksand when waterStates is an example.huge Neweruptionalsopeopleneckandwhere the lava in6.11Shiprock,Mexico,is anendangeredexample of a volcanic This1.Describepyroclasticflowsand explain why theypropertyacrossEurope.Crop failureoccurredthe all“throat”of anancient volcanocongealedto form a inplug of solid rock6.12are6.12capableof travelinggreat distances.PlateTectonicsand Volcanismthatweatheredmore slowlythe surroundingvolcanicperrocks. Theparts ofWesternEurope,andthanthousandsof residentssurrounding pyroclastic debris eroded, and the resistant neck remains2.as WhatExplainthe global distribution of volcanic activity is related to plateis a howlahar?ished fromlung-related diseases. One report estimatedtectonics.a distinctive landform.that a similar eruption today would cause more than3. ListKEYat TERMS:least threevolcanic hazards besides195Ring of Fire, volcanic island arc (island arc), continental volcanic140,000 cardiopulmonary fatalities in Europe alone.pyroclasticflowsand lahars.arc, intraplatevolcanism,mantle plume, hot spot, superplume1616.10 Intrusive IgneousActivity Volcanoes occur at both convergent and divergent plate boundaries, as61) The chapter-openingFocus on Concepts liststhe learning objectivesfor the chapter. Eachsection of the chapter istied to a specific learningobjective, providingstudents with a clearlearning path to thechapter content.Each statement represents the primary learning objective for thecorresponding major heading within the chapter. After you completethe chapter, you should be able to:Compare and contrast the 1980 eruption of Mount St.Helens with the most recent eruption of Kilauea, whichbegan in 1983.Explain why some volcanic eruptions are explosive andothers are quiescent.List and describe the three categories of materialsextruded during volcanic eruptions.Draw and label a diagram that illustrates the basicfeatures of a typical volcanic cone.Summarize the characteristics of shield volcanoes andprovide one example of this type of volcano.Describe the formation, size, and composition of cindercones.List the characteristics of composite volcanoes anddescribe how they form.Describe the major geologic hazards associated withvolcanoes.List volcanic landforms other than shield, cinder, andcomposite volcanoes and describe their formation.Compare and contrast these intrusive igneous structures:dikes, sills, batholiths, stocks, and laccoliths.Summarize the major processes that generate magmafrom solid rock.Explain how the global distribution of volcanic activity isrelated to plate tectonics.Chapter 6A rising mantle plume with alarge bulbous head is thought togenerate Earth’s large basaltplateaus.3) Concepts in Review provides students withOceaniclithosphereB.Volcanic trailOceaniclithosphereCompare and contrast these intrusive igneous structures: dikes, sills,batholiths, stocks, and laccoliths.Partialmeltingant, concordant,sill, columnar jointing,batholith, stock, laccolith6.9Otherdike,VolcanicLandformsrock rises, it can begin to melt without the addition of heat.plate boundaries that involve the subduction of oceanic crust Convergentvolcanoesmagmaintrudeslandformsother rocks, itothermay coolandshield,crystallizebefore and composite WhenListvolcanicthancinder,and describeEXAMININGTHEearthsYsteMare the most common site for explosive volcanoes—most prominently in thereaching the surface to produce intrusions called plutons. Plutons cometheir formation.Risingplumetail Volcanic eruptions cover a broad spectrum from explosive eruptions, like that of Mount St. Helens in 1980, to the quiescent eruptions of Kilauea.6.2 The Nature of Volcanic EruptionsExplain why some volcanic eruptions are explosive and others are quiescent.KEY TERMS: magma, lava, effusive eruption, viscosity, eruption column The two primary factors determining the nature of a volcanic eruption are theviscosity (resistance to flow) of the magma and its gas content. In general, magmasthat contain more silica are more viscous, while those with lower silica content aremore fluid. Temperature also influences viscosity. Hot lavas are more fluid, whilecool lavas are more viscous.Basaltic magmas, which are fluid and have low gas content, tend to generate effusive(nonexplosive) eruptions. In contrast, silica-rich magmas (andesitic and rhyolitic),which are the most viscous and contain the greatest quantity of gases, are the mostexplosive.? Although Kilauea mostly erupts in a gentle manner, what risks might youencounter if you chose to live nearby?KEY TERMS: aa flow, pahoehoe flow, lava tube, pillow lava, volatile, pyroclas-tic material, tephra, scoria, pumice Volcanoes erupt molten lava, gases, and solid pyroclastic materials. Low-viscosity basaltic lava flows can extend great distances from a volcano.GIVEIT ionGlobal photoVolcanismUSGS7 Do some investigating online and in your textbook. What are the key1 SmithsonianExamine theaccompanyingand Programcompleteandthethefollowing:work a.togethercompilea list ofisnewand changingvolcanicactivityyouworldcharacteristics for this type of volcano?Whattotypeof volcanoshown?What featureshelpedclassifywide. NOAA also uses this information to issue Volcanic Ash Advisories to8 Briefly describe the most recent activity. How was this activityit as such?alert aircraft of volcanic ash in the air.a.observed?b. What is the eruptive style of such volcanoes? Describe the likelycompositionACTIVITIESand viscosity of its magma.c. Which type of plate boundary is the likely setting for thisGo to thevolcano?Weekly Volcanic Activity Report page at http://volcano.si.edu.1 Whatinformationis displayedon thistopage?d. Namea city thatis vulnerablethe effects of a volcanothistype. and Disclaimers. Which volcanoes are not displayed2 ClickofonCriteriaon this map?3 In what areas is most of the volcanic activity concentrated?4 Click on Weekly Report. List the new volcanic activity locations. List4/10/17 3:04 PMthree ongoing volcanic activity locations.Click on the name of a volcano under New Activity/Unrest.5 Where197is thisM06 TARB3536 15 SE C06.inddvolcano located? Be sure to include the city, country,volcanic region name, latitude, and longitude.A01 TARB3536 15 SE FM.indd 4Subducting ocean4/10/17 3:04 PMDATA analYsisof the flow congeals, and lava continues to flow below in tunnels called lavatubes. When lava erupts underwater, the outer surface is chilled instantlyto obsidian, while the inside continues to flow, producing pillow lavas.The gases most commonly emitted by volcanoes are water vapor andcarbon dioxide. Upon reaching the surface, these gases rapidly expand,leading to explosive eruptions that can generate a mass of lava fragmentscalled pyroclastic materials.Pyroclastic materials come in several sizes. From smallest to largest,they are ash, lapilli, and blocks or bombs. Blocks exit the volcano as solidfragments, whereas bombs exit as liquid blobs.by requiring higher-order thinking skills toanalyze, synthesize, and apply chapter material.On the surface, they travel as pahoehoe or aa flows. Sometimes the surface TrenchUSGS4) Give It Some Thought and Examiningthe Earth System activities challenge learnersList and describe the three categories of materials extruded during volcanic eruptions.Continentalvolcanic arcJon A Helgason/Yay Micro/AGE FotostockM06 TARB3536 15 SE C06.indd 1806.3 Materials Extruded During an Eruptionand briefly explain how magma is generated in this setting.? Label the intrusive igneous structures in the accompanying diagram,using the following terms: volcanic neck, sill, batholith, laccolith.Compare and contrast the 1980 eruption of Mount St. Helens with the most recent eruption of Kilauea, which began in 1983.M06 TARB3536 15 SE C06.indd 195decompression melting is the dominant generator of magma. As warmCalderasconcepts IN reVieWVolcanoes and Other Igneous Activity6.1 Mount St. Helens Versus Kilauea well as in intraplate settings.plate boundaries, where lithosphere is being rifted apart, At divergentChapter 6 Volcanoes and Other Igneous Activity1994/10/17 3:04 PMKEY TERMS: host (country) rock, intrusion (pluton), tabular, massive, discord-Pacific Ring of Fire. The release of water from the subducting plate triggersin many shapes. They may cut across the host rocks without regard for1preexistingSpeculate structures,about some orof thethatweaka greatandinprolongedincreasein explosivevolcanicmantle.activityThemighthave on eachof Earth’smeltingin the overlyingascendingmagmainteracts with thethe possiblemagma consequencesmay flow alongzonesthefourspheres.lower crust of the overlying plate and can form a volcanic arc at the surface.host widelyrock, suchas between thehorizontallayers of sedimentaryThe mostrecognizedvolcanicstructuresare the ntleplume—a column t(dikes). C.cone-shaped edifices of composite volcanoes that dotof mantlerockarethatlargeis warmerand more buoyantthan the surroundingMassive plutons may be small (stocks) or very large (batholiths). A blisterRecall thatcalderassteep-sideddepressionsHot-spot volcanism is thought to explain the formation of large basalt plateaus and the chains ducesmantle.intrusion that lifts the overlying rock layers is a laccolith. As solidthat have diameters exceeding 1 kilometer (0.6 miles)other distinctiveand importantlandforms.igneous rock cools,its volume decreases.Contraction can produce aThe accompanying diagram shows one of the tectonic settingsand have? wherea somewhatcircular form. Those less than 1distinctive fracture pattern called columnar jointing.volcanism is a dominant process. Name the tectonic settingRisingplumetailTailFigure 6.40 Mantle plumes and large basalt plateausvolcanic islands associated with these features.6Large basalticplateauFlood basaltsHeadA.Plate motiona structured review of the chapter. Consistentwith the Focus on Concepts and Concept Checks,Concepts in Review is structured around thelearning objective for each 06 TARB3536 15 SE C06.indd 161Plate motionPlate motionEruption of ash from Mount Bromo Volcano, 2011, in Java,Indonesia.(Photo provided by Richard Roscoe/Stocktrek Images,Inc./Alamy Stock Photo)Volcanoes and Other Igneous ActivityBecause of plate movement, volcanicactivity from the rising tail of the plumegenerates a linear chain of smallervolcanic structures.Rapid decompression melting ofthe plume head produces extensive outpourings of flood basaltsover a relatively short time span.6 What is the primary volcanic type?9 What are the dates for the most recent activity?10 Click on Eruptive History. What is the earliest date listed for this volcano?11 Find this volcano on the map on the previous page. Is this volcanonear a plate boundary? If so, between which plates? (Use yourtextbook to determine the location of plate boundaries.)USGSGo to the VolcanicAsh Advisory Center (VAAC) page atwww.ssd.noaa.gov/VAAC/washington.html.12 List the VAAC locations.13 Click on Current Volcanic Ash Advisories. When was the most recentVolcanic Ash Advisory issued? What is the location of this advisory?14 Which of the new volcanic activity locations from question 4 currentlyhave Volcanic Ash Advisories? For each, what is the date of the mostrecent advisory?4/10/17 3:04 PM4/28/17 2:33 PM

EXAMINING THE earth sYsteM1 Speculate about some of the possible consequences that a great and prolonged increase in explosive volcanic activity might have on each of Earth’sfour spheres.Jon A Helgason/Yay Micro/AGE FotostockExposing Students to Source Dataand the Tools of ScienceNEW! Each chapter of the 15th edition now concludes with new Data Analysis ctivities. These brief capstone activities send students outside of the book to online scienceatools and data sets from organizations such as NASA, NOAA, and USGS, empowering studentsto apply and extend chapter concepts and develop their data analysis and critical thinking skillsDATA analYsisRecent Volcanic ActivityThe Smithsonian Institution Global Volcanism Program and the USGSwor

Bringing Earth Science to life for students, three geologists, using a quadcopter-mounted GoPro camera, have ventured into the field to film 10 key geologic locations and processes. These process-oriented videos, accessed through QR codes, are designed to bring the field to the classroom and improve the learning experience within the text.

Related Documents:

Dec 06, 2018 · Dynamic Strategy, Dynamic Structure A Systematic Approach to Business Architecture “Dynamic Strategy, . Michael Porter dynamic capabilities vs. static capabilities David Teece “Dynamic Strategy, Dynamic Structure .

iii 1 Mass Media Literacy 1 2 Media Technology 16 3 Media Economics 39 4 Cybermedia 59 5 Legacy Media 75 6 News 98 7 Entertainment 119 8 Public Relations 136 9 Advertising 152 10 Mass Audiences 172 11 Mass Media Effects 190 12 Governance and Mass Media 209 13 Global Mass Media 227 14 Mass Media Law 245 15 Mass Media Ethi

Digital Media Middle East & Middle Eastern Digital Media Awards 29-30 Nov 2022 Riyadh Digital Media Africa & African Digital Media Awards 12-13 July 2022 Virtual Digital Media LATAM & LATAM Digital Media Awards 16-18 Nov 2022 Mexico City Digital Media India & Indian Digital Media Awards 08-10 Mar 2022 Virtual Digital Media Asia &

There are many dynamic probe devices in the world, such as Dynamic Cone Penetrometer (DCP), Mackin-tosh probe, Dynamic Probing Light (DPL), Dynamic Probing Medium (DPM), Dynamic Probing High (DPH), Dynamic Probing Super High (DPSH), Perth Sand Penetrometer (PSP), etc. Table 1 shows some of the dynamic probing devices and their specifications.

work/products (Beading, Candles, Carving, Food Products, Soap, Weaving, etc.) ⃝I understand that if my work contains Indigenous visual representation that it is a reflection of the Indigenous culture of my native region. ⃝To the best of my knowledge, my work/products fall within Craft Council standards and expectations with respect to

Media Terminology Media Planning - A series of decisions involving the delivery of messages to audiences. Media Objectives - Goals to be attained by the media strategy and program. Media Strategy - Decisions on how the media objectives can be attained. Media - The various categories of delivery systems, including broadcast and print media.

Index Terms—social media; social media marketing; strat-egy; sufficient, e-word-of-mouth; Starbucks I. INTRODUCTION N MODERN society, social media is one of the essential factors in a media sector and marketing. It is said that so-cial media is a new measure for media over the world, which has a vast difference with public media. I

Hands-on Introduction to Dynamic Blocks 2 What is a Dynamic Block? A dynamic block has flexibility and intelligence. A dynamic block reference can easily be changed in a drawing while you work. You can manipulate the geometry in a dynamic b