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Week 1: Topic 2: Plate Tectonics<\/strong><\/p>\n"},"subContentId":"425b37c4-76ea-4872-82f5-2a23858361aa","metadata":{"contentType":"Text","license":"U","title":"Untitled Text"}},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""},{"x":69.6594427244582,"y":42.813455657492355,"width":30.340557275541794,"height":45.87155963302752,"action":{"library":"H5P.AdvancedText 1.1","params":{"text":"

Divergent boundaries: <\/span><\/span><\/span><\/span><\/span><\/span><\/strong>Continental rifts, <\/span><\/span><\/span><\/span><\/span>Midocean ridges (MOR)<\/span><\/span><\/span><\/span><\/span><\/p>\n\n

Convergent boundaries:<\/span><\/span><\/span><\/span><\/span><\/span><\/strong> Ocean\/ocean subduction, <\/span><\/span><\/span><\/span><\/span>Continent\/ocean subduction, <\/span><\/span><\/span><\/span><\/span>Continent\/continent (obduction; mountain building)<\/span><\/span><\/span><\/span><\/span><\/p>\n\n

Transform boundaries<\/span><\/span><\/span><\/span><\/span><\/span><\/strong><\/p>\n"},"metadata":{"contentType":"Text","license":"U","title":"Untitled Text"},"subContentId":"0571ef99-4351-4f4f-b627-64ff5e22575f"},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""}]},{"elements":[{"x":1.5478580990629183,"y":10.515873015873016,"width":58.90227576974565,"height":84.12698412698413,"action":{"library":"H5P.Image 1.1","params":{"contentName":"Image","file":{"path":"images\/file-5f0737c487433.jpg","mime":"image\/jpeg","copyright":{"license":"U"},"width":1449,"height":1050},"alt":"Alfred Wegener's evidence","title":"Alfred Wegener's evidence","decorative":false,"expandImage":"Expand Image","minimizeImage":"Minimize Image"},"subContentId":"08f19b50-4a86-48b4-a296-ed002d9d420e","metadata":{"contentType":"Image","license":"U","title":"Untitled Image"}},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""},{"x":76.30522088353413,"y":2.6455026455026456,"width":20.123839009287927,"height":12.232415902140673,"action":{"library":"H5P.AdvancedText 1.1","params":{"text":"

Alfred WEGENER \"Continental Drift\"<\/p>\n"},"subContentId":"21783939-7d55-49c5-9ea1-1edae201dae9","metadata":{"contentType":"Text","license":"U","title":"Untitled Text"}},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""},{"x":49.01960784313725,"y":79.27075268817204,"width":28.976034858387802,"height":18.279569892473116,"action":{"library":"H5P.Audio 1.5","params":{"fitToWrapper":true,"playerMode":"full","controls":true,"autoplay":true,"playAudio":"Play audio","pauseAudio":"Pause audio","contentName":"Audio","audioNotSupported":"Your browser does not support this audio","files":[{"path":"audios\/files-5f073bb473432.m4a","mime":"audio\/mp4","copyright":{"license":"U"}}]},"subContentId":"679e367c-d060-4e5d-881d-d2df638c2986","metadata":{"contentType":"Audio","license":"U","title":"Wegener"}},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""},{"x":60.24096385542169,"y":16.786534391534392,"width":39.75903614457832,"height":60.31746031746032,"action":{"library":"H5P.Image 1.1","params":{"contentName":"Image","alt":"Permian Terrestrial Fossils","file":{"path":"images\/file-5f07790197cdc.png","mime":"image\/png","copyright":{"license":"U"},"width":577,"height":443},"title":"Permian Terrestrial Fossils","decorative":false,"expandImage":"Expand Image","minimizeImage":"Minimize Image"},"subContentId":"08729707-9372-432a-9509-ae6e8efe32fc","metadata":{"contentType":"Image","license":"U","title":"Untitled Image"}},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""}],"slideBackgroundSelector":{}},{"elements":[{"x":1.5479876160990713,"y":3.058103975535168,"width":74.76780185758514,"height":91.74311926605505,"action":{"library":"H5P.Image 1.1","params":{"contentName":"Image","file":{"path":"images\/file-5f073bcfeb3ba.jpg","mime":"image\/jpeg","copyright":{"license":"U"},"width":1213,"height":751},"alt":"Map of Earth's volcanoes","title":"Map of Earth's volcanoes","decorative":false,"expandImage":"Expand Image","minimizeImage":"Minimize Image"},"subContentId":"c64b898b-449b-4d71-9eb4-7013f210c755","metadata":{"contentType":"Image","license":"U","title":"Untitled Image"}},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""},{"x":74.07407407407408,"y":70.96774193548387,"width":25.163398692810457,"height":21.29032258064516,"action":{"library":"H5P.Audio 1.5","params":{"fitToWrapper":true,"playerMode":"full","controls":true,"autoplay":true,"playAudio":"Play audio","pauseAudio":"Pause audio","contentName":"Audio","audioNotSupported":"Your browser does not support this audio","files":[{"path":"audios\/files-5f073bf386e61.m4a","mime":"audio\/mp4","copyright":{"license":"U"}}]},"subContentId":"f5711451-caac-4a7e-b898-7b2b76a04580","metadata":{"contentType":"Audio","license":"U","title":"Volcanoes"}},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""},{"x":78.94736842105263,"y":9.174311926605505,"width":10.8359133126935,"height":9.174311926605505,"action":{"library":"H5P.AdvancedText 1.1","params":{"text":"

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Earthquakes<\/p>\n\n

Arthur HOLMES<\/p>\n\n

Marie THARP & Lynn SYKES<\/p>\n\n

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Tuzo WILSON<\/p>\n"},"subContentId":"a7986278-2da1-4b37-b1ae-118294e1af00","metadata":{"contentType":"Text","license":"U","title":"Untitled Text"}},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""}],"slideBackgroundSelector":{}},{"elements":[{"x":1.3793103448275863,"y":2.7247956403269753,"width":75.86206896551724,"height":92.64305177111717,"action":{"library":"H5P.Video 1.6","params":{"visuals":{"fit":true,"controls":true},"playback":{"autoplay":false,"loop":false},"l10n":{"name":"Video","loading":"Video player loading...","noPlayers":"Found no video players that supports the given video format.","noSources":"Video is missing sources.","aborted":"Media playback has been aborted.","networkFailure":"Network failure.","cannotDecode":"Unable to decode media.","formatNotSupported":"Video format not supported.","mediaEncrypted":"Media encrypted.","unknownError":"Unknown error.","invalidYtId":"Invalid YouTube ID.","unknownYtId":"Unable to find video with the given YouTube ID.","restrictedYt":"The owner of this video does not allow it to be embedded."},"sources":[{"path":"https:\/\/youtu.be\/AhSaE0omw9o","mime":"video\/YouTube","copyright":{"license":"U"}}]},"subContentId":"7976deb4-e98d-4a2f-8762-1f2da2d9f157","metadata":{"contentType":"Video","license":"U","title":"Hot spot video"}},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""}],"slideBackgroundSelector":{}},{"elements":[{"x":2.7586206896551726,"y":5.449591280653951,"width":78.62068965517241,"height":89.9182561307902,"action":{"library":"H5P.Video 1.6","params":{"visuals":{"fit":true,"controls":true},"playback":{"autoplay":false,"loop":false},"l10n":{"name":"Video","loading":"Video player loading...","noPlayers":"Found no video players that supports the given video format.","noSources":"Video is missing sources.","aborted":"Media playback has been aborted.","networkFailure":"Network failure.","cannotDecode":"Unable to decode media.","formatNotSupported":"Video format not supported.","mediaEncrypted":"Media encrypted.","unknownError":"Unknown error.","invalidYtId":"Invalid YouTube ID.","unknownYtId":"Unable to find video with the given YouTube ID.","restrictedYt":"The owner of this video does not allow it to be embedded."},"sources":[{"path":"https:\/\/youtu.be\/KB7HzF2O3Kg","mime":"video\/YouTube","copyright":{"license":"U"}}]},"subContentId":"a0edee84-c45f-4cd3-a921-092f2007eac2","metadata":{"contentType":"Video","license":"U","title":"Alfred WEGENER"}},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""}],"slideBackgroundSelector":{}},{"elements":[{"x":1.3386880856760375,"y":2.6455026455026456,"width":97.72423025435074,"height":87.3015873015873,"action":{"library":"H5P.MultiChoice 1.16","params":{"media":{"disableImageZooming":false},"answers":[{"correct":true,"tipsAndFeedback":{"tip":"","chosenFeedback":"","notChosenFeedback":""},"text":"

All of these choices are correct<\/div>\n"},{"correct":false,"tipsAndFeedback":{"tip":"","chosenFeedback":"","notChosenFeedback":""},"text":"
Glacial evidence from areas that currently have hot climates<\/div>\n"},{"correct":false,"tipsAndFeedback":{"tip":"","chosenFeedback":"","notChosenFeedback":""},"text":"
Fossil evidence that the four legged creatures who don't fly and don't swim were found on multiple continents. <\/div>\n"},{"correct":false,"tipsAndFeedback":{"tip":"","chosenFeedback":"","notChosenFeedback":""},"text":"
Matching rock strata (layers) and mountain ranges <\/div>\n"},{"correct":false,"tipsAndFeedback":{"tip":"","chosenFeedback":"","notChosenFeedback":""},"text":"
Matching coastlines<\/div>\n"}],"overallFeedback":[{"from":0,"to":100}],"behaviour":{"enableRetry":true,"enableSolutionsButton":true,"enableCheckButton":true,"type":"auto","singlePoint":false,"randomAnswers":true,"showSolutionsRequiresInput":true,"confirmCheckDialog":false,"confirmRetryDialog":false,"autoCheck":false,"passPercentage":100,"showScorePoints":true},"UI":{"checkAnswerButton":"Check","showSolutionButton":"Show solution","tryAgainButton":"Retry","tipsLabel":"Show tip","scoreBarLabel":"You got :num out of :total points","tipAvailable":"Tip available","feedbackAvailable":"Feedback available","readFeedback":"Read feedback","wrongAnswer":"Wrong answer","correctAnswer":"Correct answer","shouldCheck":"Should have been checked","shouldNotCheck":"Should not have been checked","noInput":"Please answer before viewing the solution","a11yCheck":"Check the answers. The responses will be marked as correct, incorrect, or unanswered.","a11yShowSolution":"Show the solution. The task will be marked with its correct solution.","a11yRetry":"Retry the task. Reset all responses and start the task over again.","submitAnswerButton":"Submit"},"confirmCheck":{"header":"Finish ?","body":"Are you sure you wish to finish ?","cancelLabel":"Cancel","confirmLabel":"Finish"},"confirmRetry":{"header":"Retry ?","body":"Are you sure you wish to retry ?","cancelLabel":"Cancel","confirmLabel":"Confirm"},"question":"
Which of the following forms of evidence did Alfred WEGENER use to try to convince geologists that the continents were undergoing \"Continental Drift\"?<\/p>\n"},"subContentId":"1884a6d6-8e81-428e-9e92-9d56517336ac","metadata":{"contentType":"Multiple Choice","license":"U","title":"Wegener"}},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""}],"slideBackgroundSelector":{}},{"elements":[{"x":1.3386880856760375,"y":2.6455026455026456,"width":97.72423025435074,"height":95.23809523809524,"action":{"library":"H5P.MultiChoice 1.16","params":{"media":{"disableImageZooming":false},"answers":[{"correct":true,"tipsAndFeedback":{"tip":"","chosenFeedback":"","notChosenFeedback":""},"text":"
All of these options are correct<\/div>\n"},{"correct":false,"tipsAndFeedback":{"tip":"","chosenFeedback":"","notChosenFeedback":""},"text":"
Magnetic evidence showing \"magnetic stripes\" on the ocean floor, these were eventually interpreted to be evidence of seafloor spreading<\/div>\n"},{"correct":false,"tipsAndFeedback":{"tip":"","chosenFeedback":"","notChosenFeedback":""},"text":"
Radiometric age dating for the rocks of the ocean floor, showing that rocks at the midoceanic ridge were brand new and that those rocks get older the further you get from the ridge <\/div>\n"},{"correct":false,"tipsAndFeedback":{"tip":"","chosenFeedback":"","notChosenFeedback":""},"text":"
Radiometric age dating for the volcanoes of Hawaii, demonstrating that the oceanic floor was indeed moving over time as part of a lithospheric plate.<\/div>\n"},{"correct":false,"tipsAndFeedback":{"tip":"","chosenFeedback":"","notChosenFeedback":""},"text":"
Seismic (earthquake) evidence of the coincidence of earthquake epicentres with midoceanic ridges, with transform boundaries, and with convergent boundaries.<\/div>\n"}],"overallFeedback":[{"from":0,"to":100}],"behaviour":{"enableRetry":true,"enableSolutionsButton":true,"enableCheckButton":true,"type":"auto","singlePoint":false,"randomAnswers":true,"showSolutionsRequiresInput":true,"confirmCheckDialog":false,"confirmRetryDialog":false,"autoCheck":false,"passPercentage":100,"showScorePoints":true},"UI":{"checkAnswerButton":"Check","showSolutionButton":"Show solution","tryAgainButton":"Retry","tipsLabel":"Show tip","scoreBarLabel":"You got :num out of :total points","tipAvailable":"Tip available","feedbackAvailable":"Feedback available","readFeedback":"Read feedback","wrongAnswer":"Wrong answer","correctAnswer":"Correct answer","shouldCheck":"Should have been checked","shouldNotCheck":"Should not have been checked","noInput":"Please answer before viewing the solution","a11yCheck":"Check the answers. The responses will be marked as correct, incorrect, or unanswered.","a11yShowSolution":"Show the solution. The task will be marked with its correct solution.","a11yRetry":"Retry the task. Reset all responses and start the task over again.","submitAnswerButton":"Submit"},"confirmCheck":{"header":"Finish ?","body":"Are you sure you wish to finish ?","cancelLabel":"Cancel","confirmLabel":"Finish"},"confirmRetry":{"header":"Retry ?","body":"Are you sure you wish to retry ?","cancelLabel":"Cancel","confirmLabel":"Confirm"},"question":"
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Break time! Consider these 5 or 10 minute activites from MoveU at UofT:<\/p>\n\n
<\/p>\n\n
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Lithosphere (crust and uppermost mantle)<\/div>\n"},{"correct":false,"tipsAndFeedback":{"tip":"","chosenFeedback":"","notChosenFeedback":""},"text":"
Crust<\/div>\n"},{"correct":false,"tipsAndFeedback":{"tip":"","chosenFeedback":"","notChosenFeedback":""},"text":"
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All of the boundary types working together with the three DRIVING FORCES:<\/p>\n\n
Slab pull<\/strong> (gravity pulling the plate towards the centre of the planet), ridge push<\/strong> (gravity pulling the plates down and away from the \"mountains\" along the midoceanic ridges, in addition to new crust being formed and \"pushing\" the older crust out of the way), and mantle convection<\/strong> (the main driving force - think of it like a lava lamp where heat rises and cold sinks). It turns out that the more of a plate's edge that is hanging down into a subduction zone, the faster that plate moves!<\/p>\n"},"subContentId":"a85ff981-63ec-48e2-a075-163f5c9f1d26","metadata":{"contentType":"Text","license":"U","title":"Untitled Text"}},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""}]},{"elements":[{"x":1.3793103448275863,"y":2.7247956403269753,"width":81.37931034482759,"height":92.64305177111717,"action":{"library":"H5P.Video 1.6","params":{"visuals":{"fit":true,"controls":true},"playback":{"autoplay":false,"loop":false},"l10n":{"name":"Video","loading":"Video player loading...","noPlayers":"Found no video players that supports the given video format.","noSources":"Video is missing sources.","aborted":"Media playback has been aborted.","networkFailure":"Network failure.","cannotDecode":"Unable to decode media.","formatNotSupported":"Video format not supported.","mediaEncrypted":"Media encrypted.","unknownError":"Unknown error.","invalidYtId":"Invalid YouTube ID.","unknownYtId":"Unable to find video with the given YouTube ID.","restrictedYt":"The owner of this video does not allow it to be embedded."},"sources":[{"path":"https:\/\/youtu.be\/KfYn9KVya-Q","mime":"video\/YouTube","copyright":{"license":"U"}}]},"subContentId":"71e60b05-9d6d-4cc3-bb43-49585865285b","metadata":{"contentType":"Video","license":"U","title":"What is the effect of plate tectonics?"}},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""},{"x":82.99866131191433,"y":34.39153439153439,"width":16.465863453815263,"height":39.94708994708995,"action":{"library":"H5P.AdvancedText 1.1","params":{"text":"
What does plate tectonics do...in the long term?<\/p>\n"},"subContentId":"bdb252ed-1c12-4d8a-a3b4-41ead0763df1","metadata":{"contentType":"Text","license":"U","title":"Untitled Text"}},"alwaysDisplayComments":false,"backgroundOpacity":0,"displayAsButton":false,"buttonSize":"big","goToSlideType":"specified","invisible":false,"solution":""}],"slideBackgroundSelector":{}}],"keywordListEnabled":true,"globalBackgroundSelector":{},"keywordListAlwaysShow":false,"keywordListAutoHide":false,"keywordListOpacity":90},"override":{"activeSurface":false,"hideSummarySlide":false,"summarySlideSolutionButton":true,"summarySlideRetryButton":true,"enablePrintButton":true,"social":{"showFacebookShare":false,"facebookShare":{"url":"@currentpageurl","quote":"I scored @score out of @maxScore on a task at @currentpageurl."},"showTwitterShare":false,"twitterShare":{"statement":"I scored @score out of @maxScore on a task at @currentpageurl.","url":"@currentpageurl","hashtags":"h5p, course"},"showGoogleShare":false,"googleShareUrl":"@currentpageurl"}},"l10n":{"slide":"Slide","score":"Score","yourScore":"Your Score","maxScore":"Max Score","total":"Total","totalScore":"Total Score","showSolutions":"Show solutions","retry":"Retry","exportAnswers":"Export text","hideKeywords":"Hide sidebar navigation menu","showKeywords":"Show sidebar navigation menu","fullscreen":"Fullscreen","exitFullscreen":"Exit fullscreen","prevSlide":"Previous slide","nextSlide":"Next slide","currentSlide":"Current slide","lastSlide":"Last slide","solutionModeTitle":"Exit solution mode","solutionModeText":"Solution Mode","summaryMultipleTaskText":"Multiple tasks","scoreMessage":"You achieved:","shareFacebook":"Share on Facebook","shareTwitter":"Share on Twitter","shareGoogle":"Share on Google+","summary":"Summary","solutionsButtonTitle":"Show comments","printTitle":"Print","printIngress":"How would you like to print this presentation?","printAllSlides":"Print all slides","printCurrentSlide":"Print current slide","noTitle":"No title","accessibilitySlideNavigationExplanation":"Use left and right arrow to change slide in that direction whenever canvas is selected.","accessibilityCanvasLabel":"Presentation canvas. Use left and right arrow to move between slides.","containsNotCompleted":"@slideName contains not completed interaction","containsCompleted":"@slideName contains completed interaction","slideCount":"Slide @index of @total","containsOnlyCorrect":"@slideName only has correct answers","containsIncorrectAnswers":"@slideName has incorrect answers","shareResult":"Share Result","accessibilityTotalScore":"You got @score of @maxScore points in total","accessibilityEnteredFullscreen":"Entered fullscreen","accessibilityExitedFullscreen":"Exited fullscreen","confirmDialogHeader":"Submit your answers","confirmDialogText":"This will submit your results, do you want to continue?","confirmDialogConfirmText":"Submit and see results","accessibilityProgressBarLabel":"Choose slide to display","slideshowNavigationLabel":"Slideshow navigation"}}

ESS205 Plate Tectonics

Lisa Tutty