[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"detail-sidebar-cat-0-en-105":3,"doc-seo-657778-105":59,"doc-detail-657778-en":130},{"code":4,"msg":5,"data":6},0,"success",[7,13,18,23,28,33,38,43,48,51,55],{"id":8,"doc_module":4,"doc_module_name":9,"category_name":10,"show_sort_weight":11,"slug":12},1,"Document","Story & Novel",90,"story-novel",{"id":14,"doc_module":4,"doc_module_name":9,"category_name":15,"show_sort_weight":16,"slug":17},2,"Literature",80,"literature",{"id":19,"doc_module":4,"doc_module_name":9,"category_name":20,"show_sort_weight":21,"slug":22},4,"Exam",70,"exam",{"id":24,"doc_module":4,"doc_module_name":9,"category_name":25,"show_sort_weight":26,"slug":27},5,"Comic",60,"comic",{"id":29,"doc_module":4,"doc_module_name":9,"category_name":30,"show_sort_weight":31,"slug":32},6,"Technology",50,"technology",{"id":34,"doc_module":4,"doc_module_name":9,"category_name":35,"show_sort_weight":36,"slug":37},7,"Healthcare",40,"healthcare",{"id":39,"doc_module":4,"doc_module_name":9,"category_name":40,"show_sort_weight":41,"slug":42},8,"Research & Report",30,"research-report",{"id":44,"doc_module":4,"doc_module_name":9,"category_name":45,"show_sort_weight":46,"slug":47},9,"Religion & Spirituality",20,"religion-spirituality",{"id":46,"doc_module":4,"doc_module_name":9,"category_name":49,"show_sort_weight":46,"slug":50},"World Cup","world-cup",{"id":52,"doc_module":4,"doc_module_name":9,"category_name":53,"show_sort_weight":52,"slug":54},10,"Lifestyle","lifestyle",{"id":56,"doc_module":4,"doc_module_name":9,"category_name":57,"show_sort_weight":24,"slug":58},19,"General","general",{"code":4,"msg":60,"data":61},"ok",{"site_id":62,"language":63,"slug":64,"title":65,"keywords":66,"description":67,"schema_data":68,"social_meta":123,"head_meta":125,"extra_data":127,"updated_unix":129},105,"en","lesson-6-volcano-and-eq-differences-margin-types-and-hazards","Lesson 6 - Volcano and EQ Differences - Margin Types and Hazards","","Lesson 6 explains how different plate margin types control both volcanic hazards and earthquake characteristics. The content links constructive, collision, destructive oceanic/oceanic, transform/conservative, and destructive oceanic/continental settings to distinct hazard profiles, emphasizing that volcanic areas can differ greatly even when they are circled together. It also connects lava type to volcano shape, contrasting shield volcanoes with ash/cinder cones, and highlights how natural local variations can raise or reduce risk. Earthquakes are described as occurring across plate margins and within plates, with magnitude tied to frequency and depth, influenced by subduction, folding, faulting, and rifting.",{"@graph":69,"@context":122},[70,84,105],{"@type":71,"itemListElement":72},"BreadcrumbList",[73,77,79,82],{"item":74,"name":75,"@type":76,"position":8},"https://docshare.wps.com","Home","ListItem",{"item":78,"name":9,"@type":76,"position":14},"https://docshare.wps.com/document/",{"item":80,"name":20,"@type":76,"position":81},"https://docshare.wps.com/document/exam/",3,{"item":83,"name":65,"@type":76,"position":19},"https://docshare.wps.com/document/lesson-6-volcano-and-eq-differences-margin-types-and-hazards/657778/",{"url":83,"name":65,"@type":85,"image":86,"author":91,"headline":65,"publisher":94,"fileFormat":97,"inLanguage":63,"description":67,"dateModified":98,"datePublished":99,"encodingFormat":97,"isAccessibleForFree":100,"interactionStatistic":101},"DigitalDocument",{"url":87,"@type":88,"width":89,"height":90},"https://docshare.wps.com/thumbnails/lesson-6-volcano-and-eq-differences-margin-types-and-hazards/657778.png","ImageObject",300,407,{"name":92,"@type":93},"Alexandar","Person",{"url":74,"name":95,"@type":96},"DocShare","Organization","application/pdf","2026-10-30","2026-10-26",true,{"@type":102,"interactionType":103,"userInteractionCount":81},"InteractionCounter",{"@type":104},"ViewAction",{"@type":106,"mainEntity":107},"FAQPage",[108,114,118],{"name":109,"@type":110,"acceptedAnswer":111},"How do different plate margin types change the magnitude and impact of volcanic hazards?","Question",{"text":112,"@type":113},"Different margin types have distinct characteristics that produce different volcanic hazards. The lesson emphasizes that volcanic areas can look similar on a map but still be very different because the margin type alters the processes involved.","Answer",{"name":115,"@type":110,"acceptedAnswer":116},"How does lava type link to volcano shape, and what examples are given?",{"text":117,"@type":113},"Lava type is linked to volcano shape by contrasting shield volcanoes with ash/cinder cones. The lesson asks learners to explain how magma behavior relates to these two main forms.",{"name":119,"@type":110,"acceptedAnswer":120},"What controls earthquake magnitude and how do earthquakes relate to plate boundaries?",{"text":121,"@type":113},"Earthquakes occur along all plate margins and also within intra-plate locations. Magnitude is often associated with frequency and depth, which are dictated by processes such as subduction, collision (rock folding and faulting), or rifting.","https://schema.org",{"og:url":83,"og:type":124,"og:title":65,"og:site_name":95,"og:description":67},"article",{"robots":126,"canonical":83},"index,follow",{"doc_id":128,"site_id":62},657778,1792988843,{"code":4,"msg":5,"data":131},{"doc_id":128,"user_id":132,"nickname":92,"user_avatar":133,"doc_module":4,"category_id":19,"category_name":20,"doc_title":65,"doc_description":67,"doc_content":134,"file_id":135,"file_url":136,"file_type":137,"file_size":138,"view_count":81,"is_deleted":4,"is_public":8,"is_downloadable":8,"audit_status":8,"page_count":139,"language":140,"language_code":63,"site_id":62,"html_lang":63,"table_of_contents":141,"faqs":142,"seo_title":143,"seo_description":67,"update_tm":129,"read_time":144},962090768658,"https://ap-avatar.wpscdn.com/davatar_6f874abed73319feea01a86fa6f0fab8","QU: How do physical processes alter the magnitude of volcanic and EQ  hazards?  \nAIM: To explain how margin type influences the above.  \nSt: Draw a 10 second block diagram of one of the margins below.  \nOutine what you already know about the nature/magnitude of the EQ or volcano  risk on this type of margin.  \nConstructive margin  \nContinental collision margin  \nDestructive oceanic/oceanic margin  \nTransform/conservative margin  \nDestructive oceanic/continental margin  \nRecap-all covered except highlighted.  \nThe circled areas are all volcanic...yet each is very different. Different margin types due to their characteristics produce different hazards. You must be clear on these.  \nTask:  \n1-Complete the gap fill on lava type and hazards and then offer reasons for the questions about the lava types.  \n2-How does lava type link to volcano shape? Explain shield volcanoes and ash/cinder cones. Pg. 22-23 Waugh will help.  \nExt: Link volcano shape to boundary type.  \nA* material? -What natural local variations could increase/decrease the hazard posed by some of these?  \nSparkling water Lemonade  \nWhich of these most characterises the rising magma you would find at a destructive margin? Both have gas content.  \nSo how should they erupt?   outside we go...  \nThis is what your 'lemonade bottle' volcano can do in real terms!!  \nPyroclastic flow  \n132 ,000 ft  \nThese people are 80 miles from the 1991 Pinatubo eruption. Everest is 28,000 ft high for a sense of scale on this ash cloud.  \nFor 2 days sunlight never reached the Phillipines. The tropical nation had a daytime temperature of 4 degrees. Globally the summer of 1992 was wet and cold, attributed to the ash from this one eruption event the previous year.  \nGlobally, sunsets were spectacular!!  \nVolcanic hazards are NOT the same on every plate margin or intra-plate location. magnitude and impacts are influenced by the processes of subduction, gas entrainment or convection.  \nBut what of earthquakes?  \nEarthquakes occur along all plate margins and in intra-plate locations. However their magnitude is often associated with their frequency (small and often versus large and rare) and depth. This is again dictated by processes such as subduction. Or rocks folding and faulting due to collision or rifting.  \nThe map below shows every earthquake recorded between 2002 and 2011  \nRed is recent, and goes to yellow after 15 days, then drops off.  \nStaImartege on Augustadded abo5tee, 20ry072d. ays.   Due to the fact the animation is  \nspeeded up you cannot notice this.  \nCan you identify the most active areas?  \nPlate boundary relationship?  \nRed = Shallow focus EQ Blue/green = deep focus EQ","cbCaiaxJh0aWXYao","https://ap.wps.com/l/cbCaiaxJh0aWXYao","pdf",9088946,21,"English","# Volcano and earthquake hazards by margin type\n## Margin types and hazard differences\n## Lava type and volcano shape\n## Linking boundary type to hazards\n# Earthquakes and boundary relationships\n## Depth, frequency, and magnitude","[{\"question\":\"How do different plate margin types change the magnitude and impact of volcanic hazards?\",\"answer\":\"Different margin types have distinct characteristics that produce different volcanic hazards. The lesson emphasizes that volcanic areas can look similar on a map but still be very different because the margin type alters the processes involved.\"},{\"question\":\"How does lava type link to volcano shape, and what examples are given?\",\"answer\":\"Lava type is linked to volcano shape by contrasting shield volcanoes with ash/cinder cones. The lesson asks learners to explain how magma behavior relates to these two main forms.\"},{\"question\":\"What controls earthquake magnitude and how do earthquakes relate to plate boundaries?\",\"answer\":\"Earthquakes occur along all plate margins and also within intra-plate locations. Magnitude is often associated with frequency and depth, which are dictated by processes such as subduction, collision (rock folding and faulting), or rifting.\"}]","Lesson 6 - Volcano and EQ Differences - Margin Types and Hazards | PDF",53]