Dynamic Earth Interactive Web Quest PDF
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Neel
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This document is an interactive web quest about plate tectonics and geology. It includes questions and activities to guide students through the material.
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โญName: Neelโฌ โญDynamic Earth Interactive Web Questโฌ โญ irectionsโฌโญ: Go to Google Classroom to access theโฌโญlink or type inโฌ D โญhttps://www.learner.org/wp-content/interactive/dynamicearth/drift.htmlโฌ โญ1.)โฌ R โญ ead theโฌโญIntroductionโฌโญ. Then click on the red arrow...
โญName: Neelโฌ โญDynamic Earth Interactive Web Questโฌ โญ irectionsโฌโญ: Go to Google Classroom to access theโฌโญlink or type inโฌ D โญhttps://www.learner.org/wp-content/interactive/dynamicearth/drift.htmlโฌ โญ1.)โฌ R โญ ead theโฌโญIntroductionโฌโญ. Then click on the red arrowโฌโญwhere it saysโฌโญStart your explorationโฌ โญwithโฌโญPlate Tectonicsโฌโญ(tab located at the top of theโฌโญpage)โฌโญ.โฌ โญ2.)โฌ โญFollow the directions on theโฌโญP late Tectonicsโฌโญpage.โฌ โญRead the information on the page and then click onโฌ โญHow Do We Know Thisโฌโญ?โฌ โญa.โฌ โญWhat evidence did Alfred Wegner discover along the coastlines of continents?โฌ โญi.โฌ โญHe studied the coastlines along Africa and South America looked like they might fitโฌ โญtogetherโฌ โญii.โฌ โญHe also discovered that the same plants and animal fossils can be found on the coastsโฌ โญof both continents, although oceans separated themโฌ โญiii.โฌ โญHe also noticed that the geologic formations of the two continents match upโฌ โญb.โฌ โญWhat isโฌโญPangaeaโฌโญ?โฌ โญi.โฌ โญPangaea is a Greek word that means โall the earthโ. According to Wegner he believedโฌ โญthat earth was once a large land mass and over time it split apart. The differentโฌ โญlandmasses, or continents, then drifted to their current locations on the globe.โฌ โญc.โฌ โญWhat is theโฌโญtheory ofโฌโญplate tectonicsโฌโญ?โฌ โญi.โฌ โญThe theory of plate tectonics states thatโฌ โญ1.โฌ โญEarth's outer layer, or lithosphere, is broken into several large slabs calledโฌ โญplates.โฌ โญ2.โฌ โญThese plates, which hold the continents and oceans, are slowly but constantlyโฌ โญmoving around the planet.โฌ โญ3.โฌ โญThe movement of the plates not only supports our understanding that continentsโฌ โญare not fixed and moved over time, but also explains how and why earthquakes,โฌ โญvolcanoes, and other geologic events occur.โฌ โญ3.)โฌ Lโญ ocate the red arrow at the bottom of the page and click onโฌโญContinents Over Timeโฌโญ. Follow theโฌ โญdirections on the next page and complete the activity.โฌ โญCOMPLETEDโฌ โญ4.)โฌ โญMove on to the next chapter,โฌโญP late Boundariesโฌโญ, toโฌโญlearn how plates interact. Carefully read the entireโฌ โญpage and answer the following questions as you read:โฌ โญa.โฌ โญAre the earthโs continents constantly moving? Why?โฌ โญi.โฌ โญYes, Tremendous heat and pressure within the earth cause the hot magma to flow inโฌ โญconvection currents. These currents cause the movement of the tectonic plates thatโฌ โญmake up the earth's crust.โฌ โญb.โฌ โญFill in the chart below.โฌ โญType of Plate Boundaryโฌ โญDraw 2 arrows toโฌ โญWhat is it and provide anโฌ โญrepresentโฌ โญexampleโฌ โญConvergent boundaries areโฌ โญwhen two plates comeโฌ โญConvergentโฌ โญtogetherโฌ โญThe boundary between theโฌ โญEurasian Plate and the Indianโฌ โญPlate at the Himalayasโฌ โญA divergent boundary occursโฌ โญwhen two tectonic platesโฌ โญDivergentโฌ โญmove away from each other.โฌ โญThe boundary between theโฌ โญAfrican Plate and the Arabianโฌ โญPlate in the Red Seaโฌ โญTransform boundaries areโฌ โญplaces where plates slideโฌ โญTransformโฌ โญs ideways past each other.โฌ โญThe boundary between theโฌ โญPacific Plate and theโฌ โญAustralian Plate, crossingโฌ โญNew Zealandโฌ โญ5.)โฌ โญUse the map at the bottom of the page to see where the three types of plate boundaries are foundโฌ โญthroughout the world.โฌ โญCOMPLETEDโฌ โญ6.)โฌ โญLocate the red arrow at the bottom of the page and click onโฌโญP lates & Boundaries Challengeโฌโญ. Completeโฌ โญthe challenge.โฌ โญCOMPLETEDโฌ โญ7.)โฌ โญRead theโฌโญSlip, Slide, & Collideโฌโญpage and answer theโฌโญfollowing question:โฌ โญa.โฌ โญGive examples of geological phenomena we experience on Earth that are caused by theโฌ โญs lipping, sliding, and colliding of tectonic plates.โฌ โญi.โฌ โญHimalayan mountains grow taller every year - Plate Collision, Indian and Eurasian plateโฌ โญii.โฌ โญMid Ocean Ridges - At divergent boundaries, plates move apart and magma from theโฌ โญmantle rises to fill up the gapโฌ โญiii.โฌ โญEarthquakes/Volcanoes - Tectonic plates slippingโฌ โญ8.)โฌ โญLocate the red arrow at the bottom of the page and click onโฌโญSee what happens at different plateโฌ โญboundariesโฌโญ. Read and view the diagrams.โฌ โญPlates in Motion Impactsโฌ โญW hat will happen if two continental plates collide?โฌ โญContinent - Continent Collision โ Because the rock making up continental plates is generally lighter and lessโฌ โญ ense than oceanic rock, it is too light to get pulled under the earth and turned into magma. Instead, aโฌ d โญcollision between two continental plates crunches and folds the rock at the boundary, lifting it up and leadingโฌ โญto the formation of mountains and mountain ranges.โฌ โญExample:โฌ Tโญ he Himalayan range in southern Asia - This process began after the breakup of Pangaea, when India becameโฌ โญan island continent and began traveling northward toward Asia. The island of India slammed into Asia about 40โฌ โญto 50 million years ago near modern-day Tibet, crushing and folding the plates to form the Himalayan mountainโฌ โญrange. Indian Plate is continuing its northward movement into Asia, Himalayas continue grow higher each yearโฌ โญby 5 to 20 mm or 1 inch per year.โฌ โญW hat will happen if a continental plate collides with an oceanic plate?โฌ โญContinent - Oceanic Crust Collision โ Oceanic crust tends to be denser and thinner than continental crustโฌ Tโญ his means that the denser oceanic crust gets bent and pulled under, or subducted, beneath the lighter andโฌ โญthicker continental crust.โฌ โญThis forms what is called aโฌโญsubduction zoneโฌโญ.โฌ โญAs the oceanic crust sinks, a deep oceanic trench/valley, is formed at the edge of the continent.โฌ Tโญ he crust continues to be forced deeper into the earth, where high heat and pressure cause trapped water andโฌ โญother gasses to be released from it.โฌ โญThis, in turn, makes the base of the crust melt, forming magmaโฌ โญExample: Band of active volcanoes that encircle the Pacific Ocean, often referred to as the Ring of Fire.โฌ โญW hat will happen if two oceanic plates collide?โฌ โญ ceanic - Oceanic Collision โโฌโญA subduction zone isโฌโญalso generated when two oceanic plates collide โโฌ O โญthe older plate is forced under the younger one โ and it leads to the formation of chains of volcanicโฌ โญislands known asโฌโญisland arcsโฌโญ. Since the collisionโฌโญand subduction of plates is not a smooth process,โฌ โญlarge, powerful earthquakes are another phenomenon that result from this type of interaction.โฌ โญEarthquakes generated in a subduction zone can also give rise to tsunamis.โฌ โญExample:โฌ โญโฌ T โญ he Mariana Islands in the western Pacific Oceanโฌ โญโฌ โญThe Aleutian Islands, off the coast of Alaskaโฌ โญWhat is a Subduction Zone? Provide an example and describe what happens here, and provide aโฌ โญdiagram.โฌ โญ subduction zone is generated when two oceanic plates collide โ the older plate is forced under theโฌ A โญyounger one โ and it leads to the formation of chains of volcanic islands known asโฌโญisland arcsโฌโญ.โฌ โญOceanic crust tends to be denser and thinner than continental crustโฌ โญ his means that the denser oceanic crust gets bent and pulled under, or subducted, beneath theโฌ T โญlighter and thicker continental crust.โฌ โญThis forms what is called aโฌโญsubduction zoneโฌโญ.โฌ