Dynamic Earth Interactive Web Quest PDF

Summary

This document is an interactive web quest about plate tectonics and geology. It includes questions and activities to guide students through the material.

Full Transcript

โ€ญName: Neelโ€ฌ โ€ญDynamic Earth Interactive Web Questโ€ฌ โ€ญ irectionsโ€ฌโ€ญ: Go to Google Classroom to access theโ€ฌโ€ญlink or type inโ€ฌ D โ€ญhttps://www.learner.org/wp-content/interactive/dynamicearth/drift.htmlโ€ฌ โ€ญ1.)โ€ฌ R โ€ญ ead theโ€ฌโ€ญIntroductionโ€ฌโ€ญ. Then click on the red arrow...

โ€ญName: Neelโ€ฌ โ€ญDynamic Earth Interactive Web Questโ€ฌ โ€ญ irectionsโ€ฌโ€ญ: Go to Google Classroom to access theโ€ฌโ€ญlink or type inโ€ฌ D โ€ญhttps://www.learner.org/wp-content/interactive/dynamicearth/drift.htmlโ€ฌ โ€ญ1.)โ€ฌ R โ€ญ ead theโ€ฌโ€ญIntroductionโ€ฌโ€ญ. Then click on the red arrowโ€ฌโ€ญwhere it saysโ€ฌโ€ญStart your explorationโ€ฌ โ€ญwithโ€ฌโ€ญPlate Tectonicsโ€ฌโ€ญ(tab located at the top of theโ€ฌโ€ญpage)โ€ฌโ€ญ.โ€ฌ โ€ญ2.)โ€ฌ โ€ญFollow the directions on theโ€ฌโ€ญP late Tectonicsโ€ฌโ€ญpage.โ€ฌ โ€ญRead the information on the page and then click onโ€ฌ โ€ญHow Do We Know Thisโ€ฌโ€ญ?โ€ฌ โ€ญa.โ€ฌ โ€ญWhat evidence did Alfred Wegner discover along the coastlines of continents?โ€ฌ โ€ญi.โ€ฌ โ€ญHe studied the coastlines along Africa and South America looked like they might fitโ€ฌ โ€ญtogetherโ€ฌ โ€ญii.โ€ฌ โ€ญHe also discovered that the same plants and animal fossils can be found on the coastsโ€ฌ โ€ญof both continents, although oceans separated themโ€ฌ โ€ญiii.โ€ฌ โ€ญHe also noticed that the geologic formations of the two continents match upโ€ฌ โ€ญb.โ€ฌ โ€ญWhat isโ€ฌโ€ญPangaeaโ€ฌโ€ญ?โ€ฌ โ€ญi.โ€ฌ โ€ญPangaea is a Greek word that means โ€œall the earthโ€. According to Wegner he believedโ€ฌ โ€ญthat earth was once a large land mass and over time it split apart. The differentโ€ฌ โ€ญlandmasses, or continents, then drifted to their current locations on the globe.โ€ฌ โ€ญc.โ€ฌ โ€ญWhat is theโ€ฌโ€ญtheory ofโ€ฌโ€ญplate tectonicsโ€ฌโ€ญ?โ€ฌ โ€ญi.โ€ฌ โ€ญThe theory of plate tectonics states thatโ€ฌ โ€ญ1.โ€ฌ โ€ญEarth's outer layer, or lithosphere, is broken into several large slabs calledโ€ฌ โ€ญplates.โ€ฌ โ€ญ2.โ€ฌ โ€ญThese plates, which hold the continents and oceans, are slowly but constantlyโ€ฌ โ€ญmoving around the planet.โ€ฌ โ€ญ3.โ€ฌ โ€ญThe movement of the plates not only supports our understanding that continentsโ€ฌ โ€ญare not fixed and moved over time, but also explains how and why earthquakes,โ€ฌ โ€ญvolcanoes, and other geologic events occur.โ€ฌ โ€ญ3.)โ€ฌ Lโ€ญ ocate the red arrow at the bottom of the page and click onโ€ฌโ€ญContinents Over Timeโ€ฌโ€ญ. Follow theโ€ฌ โ€ญdirections on the next page and complete the activity.โ€ฌ โ€ญCOMPLETEDโ€ฌ โ€ญ4.)โ€ฌ โ€ญMove on to the next chapter,โ€ฌโ€ญP late Boundariesโ€ฌโ€ญ, toโ€ฌโ€ญlearn how plates interact. Carefully read the entireโ€ฌ โ€ญpage and answer the following questions as you read:โ€ฌ โ€ญa.โ€ฌ โ€ญAre the earthโ€™s continents constantly moving? Why?โ€ฌ โ€ญi.โ€ฌ โ€ญYes, Tremendous heat and pressure within the earth cause the hot magma to flow inโ€ฌ โ€ญconvection currents. These currents cause the movement of the tectonic plates thatโ€ฌ โ€ญmake up the earth's crust.โ€ฌ โ€ญb.โ€ฌ โ€ญFill in the chart below.โ€ฌ โ€ญType of Plate Boundaryโ€ฌ โ€ญDraw 2 arrows toโ€ฌ โ€ญWhat is it and provide anโ€ฌ โ€ญrepresentโ€ฌ โ€ญexampleโ€ฌ โ€ญConvergent boundaries areโ€ฌ โ€ญwhen two plates comeโ€ฌ โ€ญConvergentโ€ฌ โ€ญtogetherโ€ฌ โ€ญThe boundary between theโ€ฌ โ€ญEurasian Plate and the Indianโ€ฌ โ€ญPlate at the Himalayasโ€ฌ โ€ญA divergent boundary occursโ€ฌ โ€ญwhen two tectonic platesโ€ฌ โ€ญDivergentโ€ฌ โ€ญmove away from each other.โ€ฌ โ€ญThe boundary between theโ€ฌ โ€ญAfrican Plate and the Arabianโ€ฌ โ€ญPlate in the Red Seaโ€ฌ โ€ญTransform boundaries areโ€ฌ โ€ญplaces where plates slideโ€ฌ โ€ญTransformโ€ฌ โ€ญs ideways past each other.โ€ฌ โ€ญThe boundary between theโ€ฌ โ€ญPacific Plate and theโ€ฌ โ€ญAustralian Plate, crossingโ€ฌ โ€ญNew Zealandโ€ฌ โ€ญ5.)โ€ฌ โ€ญUse the map at the bottom of the page to see where the three types of plate boundaries are foundโ€ฌ โ€ญthroughout the world.โ€ฌ โ€ญCOMPLETEDโ€ฌ โ€ญ6.)โ€ฌ โ€ญLocate the red arrow at the bottom of the page and click onโ€ฌโ€ญP lates & Boundaries Challengeโ€ฌโ€ญ. Completeโ€ฌ โ€ญthe challenge.โ€ฌ โ€ญCOMPLETEDโ€ฌ โ€ญ7.)โ€ฌ โ€ญRead theโ€ฌโ€ญSlip, Slide, & Collideโ€ฌโ€ญpage and answer theโ€ฌโ€ญfollowing question:โ€ฌ โ€ญa.โ€ฌ โ€ญGive examples of geological phenomena we experience on Earth that are caused by theโ€ฌ โ€ญs lipping, sliding, and colliding of tectonic plates.โ€ฌ โ€ญi.โ€ฌ โ€ญHimalayan mountains grow taller every year - Plate Collision, Indian and Eurasian plateโ€ฌ โ€ญii.โ€ฌ โ€ญMid Ocean Ridges - At divergent boundaries, plates move apart and magma from theโ€ฌ โ€ญmantle rises to fill up the gapโ€ฌ โ€ญiii.โ€ฌ โ€ญEarthquakes/Volcanoes - Tectonic plates slippingโ€ฌ โ€ญ8.)โ€ฌ โ€ญLocate the red arrow at the bottom of the page and click onโ€ฌโ€ญSee what happens at different plateโ€ฌ โ€ญboundariesโ€ฌโ€ญ. Read and view the diagrams.โ€ฌ โ€ญPlates in Motion Impactsโ€ฌ โ€ญW hat will happen if two continental plates collide?โ€ฌ โ€ญContinent - Continent Collision โ†’ Because the rock making up continental plates is generally lighter and lessโ€ฌ โ€ญ ense than oceanic rock, it is too light to get pulled under the earth and turned into magma. Instead, aโ€ฌ d โ€ญcollision between two continental plates crunches and folds the rock at the boundary, lifting it up and leadingโ€ฌ โ€ญto the formation of mountains and mountain ranges.โ€ฌ โ€ญExample:โ€ฌ Tโ€ญ he Himalayan range in southern Asia - This process began after the breakup of Pangaea, when India becameโ€ฌ โ€ญan island continent and began traveling northward toward Asia. The island of India slammed into Asia about 40โ€ฌ โ€ญto 50 million years ago near modern-day Tibet, crushing and folding the plates to form the Himalayan mountainโ€ฌ โ€ญrange. Indian Plate is continuing its northward movement into Asia, Himalayas continue grow higher each yearโ€ฌ โ€ญby 5 to 20 mm or 1 inch per year.โ€ฌ โ€ญW hat will happen if a continental plate collides with an oceanic plate?โ€ฌ โ€ญContinent - Oceanic Crust Collision โ†’ Oceanic crust tends to be denser and thinner than continental crustโ€ฌ Tโ€ญ his means that the denser oceanic crust gets bent and pulled under, or subducted, beneath the lighter andโ€ฌ โ€ญthicker continental crust.โ€ฌ โ€ญThis forms what is called aโ€ฌโ€ญsubduction zoneโ€ฌโ€ญ.โ€ฌ โ€ญAs the oceanic crust sinks, a deep oceanic trench/valley, is formed at the edge of the continent.โ€ฌ Tโ€ญ he crust continues to be forced deeper into the earth, where high heat and pressure cause trapped water andโ€ฌ โ€ญother gasses to be released from it.โ€ฌ โ€ญThis, in turn, makes the base of the crust melt, forming magmaโ€ฌ โ€ญExample: Band of active volcanoes that encircle the Pacific Ocean, often referred to as the Ring of Fire.โ€ฌ โ€ญW hat will happen if two oceanic plates collide?โ€ฌ โ€ญ ceanic - Oceanic Collision โ†’โ€ฌโ€ญA subduction zone isโ€ฌโ€ญalso generated when two oceanic plates collide โ€”โ€ฌ O โ€ญthe older plate is forced under the younger one โ€” and it leads to the formation of chains of volcanicโ€ฌ โ€ญislands known asโ€ฌโ€ญisland arcsโ€ฌโ€ญ. Since the collisionโ€ฌโ€ญand subduction of plates is not a smooth process,โ€ฌ โ€ญlarge, powerful earthquakes are another phenomenon that result from this type of interaction.โ€ฌ โ€ญEarthquakes generated in a subduction zone can also give rise to tsunamis.โ€ฌ โ€ญExample:โ€ฌ โ€ญโ€ฌ T โ€ญ he Mariana Islands in the western Pacific Oceanโ€ฌ โ€ญโ€ฌ โ€ญThe Aleutian Islands, off the coast of Alaskaโ€ฌ โ€ญWhat is a Subduction Zone? Provide an example and describe what happens here, and provide aโ€ฌ โ€ญdiagram.โ€ฌ โ€ญ subduction zone is generated when two oceanic plates collide โ€” the older plate is forced under theโ€ฌ A โ€ญyounger one โ€” and it leads to the formation of chains of volcanic islands known asโ€ฌโ€ญisland arcsโ€ฌโ€ญ.โ€ฌ โ€ญOceanic crust tends to be denser and thinner than continental crustโ€ฌ โ€ญ his means that the denser oceanic crust gets bent and pulled under, or subducted, beneath theโ€ฌ T โ€ญlighter and thicker continental crust.โ€ฌ โ€ญThis forms what is called aโ€ฌโ€ญsubduction zoneโ€ฌโ€ญ.โ€ฌ

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