[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"doc-seo-422366-105":3,"detail-sidebar-cat-0-en-105":81,"doc-detail-422366-en":130},{"code":4,"msg":5,"data":6},0,"ok",{"site_id":7,"language":8,"slug":9,"title":10,"keywords":11,"description":12,"schema_data":13,"social_meta":74,"head_meta":76,"extra_data":78,"updated_unix":80},105,"en","volcanoes-a-hands-on-science-kit-violent-volcanoes","VOLCANOES - A hands-on science kit - VIOLENT VOLCANOES!","","A hands-on science kit introduces volcanoes through vivid, age-appropriate storytelling and clear explanations. It recounts a dramatic, time-travel scenario based on the May 18, 1980 eruption of Mount St. Helens, describing ash clouds, scorching winds, and the danger zone. It then explains how Earth’s crust and tectonic plates form volcanic openings along the Ring of Fire, how hot spots create islands like Hawaii, and how volcanoes are classified as active, extinct, or dormant. 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It emphasizes that survival is extremely unlikely at close range.","Answer",{"name":66,"@type":61,"acceptedAnswer":67},"How do the Ring of Fire and tectonic plates relate to volcanoes?",{"text":68,"@type":64},"Volcanoes are linked to where plates separate, collide, or slide, creating breaks in the crust that let magma rise. The Ring of Fire is the boundary where many volcanic openings occur.",{"name":70,"@type":61,"acceptedAnswer":71},"What determines whether a volcano is active, extinct, or dormant?",{"text":72,"@type":64},"The classification depends on its state of activity. Active volcanoes erupt constantly, extinct volcanoes will never erupt again, and dormant volcanoes are inactive but expected to erupt in the future.","https://schema.org",{"og:url":32,"og:type":75,"og:title":10,"og:site_name":45,"og:description":12},"article",{"robots":77,"canonical":32},"index,follow",{"doc_id":79,"site_id":7},422366,1792644147,{"code":4,"msg":82,"data":83},"success",[84,88,92,96,101,105,109,114,119,122,126],{"id":22,"doc_module":4,"doc_module_name":25,"category_name":85,"show_sort_weight":86,"slug":87},"Story & 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UPTroll  \n# A hands-on science kit\n\nBy Ian BoydIllustrated by J.Angel  \nPhoto Credits  \nUnited States Geological Survey  \nMount St.Helens,page 2;Mauna Loa,page 6;Paricutín,page 7(R.E.Wilcox);EI Sangay,page 7(G.E.Lewis);Pahoehoe lava,page 10(T.L.Wright);Aa lava,page 11;Pyroclastic flow,page 11(H.Glicken)  \n◎ The Stock Market/Ralph Perry  \nMount St.Helens,front cover  \nTroll  \nCopyright ◎1997 by Troll Communications L.L.C.  \nAll rights reserved.No part of this book may be reproduced or utilized in any form orby any means,electronic or mechanical,including photocopying,recording,or by anyinformation storage and retrieval system,without written permission from the publisher.  \nPrinted in the United States of America.ISBN 0-8167-4443-2  \n# VIOLENT VOLCANOES!\n\nImagine traveling back in time to the morning of May 18,1980.Your destination is the woodsof Washington state,about 15 miles(24 km)north of Mount St.Helens—a magnificent,snow-capped mountain that happens to be volcanic and is predicted to erupt very soon.But the areaseems to be safe.The sun is shining,birds are chirping,and besides,you're several milesbeyond the evacuation zone.  \nAt 8:30 A.M.,the mountain erupts,belching outa mighty blast of hot gas and ash.But insteadof going straight up,the blast heads north—directly toward you!In the distance,yousee an ominous cloud approaching rapidly.Within minutes,day turns to night as ashenvelops you.Scorching winds rip talltrees out of the ground.Luckily,you seea hole left by an uprooted tree and leapinside to safety.  \nThis is what you might have seen had youbeen near Mount St.Helens on that fatefulmorning.But in reality,it is doubtful thatanyone could survive such a close encounterwith an eruption this powerful.The eruption ofMount St.Helens killed fifty-seven people anddemolished forests as far as 20 miles(32 km)away!And that's minor compared with othermighty eruptions that have occurred withinthe past few centuries.The strength,fury,andunpredictable nature of volcanoes areunequaled in the natural world.  \n2  \nMount FujiJapan  \nRING OF FIRE  \nVolcanoes are really just openings in theearth's upper layer,the crust,through whichMount St.Helensmagma(melted rock)and other materials fromU.S.A.under the ground erupt.There are 600 known volcanicopenings on Earth.More than half occur along the rim ofthe Pacific Ocean,an area often called the “Ring of Fire.”The Ring of Fire is the boundary of one of the earth's tensurface layers,called plates.These enormous plates are constantlyseparating,colliding,or sliding past one another,creating breaks inthe earth's crust and allowing magma to rise to the surface.Mount Pinatubo  \nVolcanoes also occur over areas called“hot spots”—weak spotson the earth's crust where magma forces its way through.These spotsare usually found on the ocean floor.The Hawaiian Islandsformed above a hot spot.  \nAll volcanoes are classified by their state of activity:active,extinct,or dormant.Active volcanoes erupt constantly;extinct volcanoes will never erupt again;and dormant volcanoes are said to beNevado del Ruiz\"sleeping,\"meaning they are inactiveColombiabut are expected to erupt in the future.  \nThe volcanoes shown on this page—Mount Fuji,Mount St.Helens,Nevado del Ruiz,and Mount Pinatubo---are just a few of the activevolcanoes located on the Ring of Fire.  \nHOT TO THE CORE  \nThe earth is made up of four layers:the inner core,the outer core,the mantle,and the crust.These layers constantly interact with one another to bring volcanoes to life.  \nVolcanic activity starts thousands of miles below the earth’s surface.There,temperatures as hotas 13,000°F(7,000°C)radiate through the inner and outer cores and turn areas of the mantleinto molten magma(red-hot,liquid rock).Gas is produced when the rock melts.This gas mixeswith the magma and causes it to rise toward the earth's surface.When the gas-filled magmaencounters the rocky cru","cbCairbluc7dDtBb","https://ap.wps.com/l/cbCairbluc7dDtBb","pdf",1883362,24,"English","# A hands-on science kit\n## VIOLENT VOLCANOES!\n## RING OF FIRE\n## HOT TO THE CORE\n## INSIDE A VOLCANO\n## TYPES OF VOLCANOES","[{\"question\":\"What happens during the eruption of a volcano like Mount St. Helens?\",\"answer\":\"The book describes a blast of hot gas and ash, rapid-moving clouds, and intense winds that can cause severe destruction. It emphasizes that survival is extremely unlikely at close range.\"},{\"question\":\"How do the Ring of Fire and tectonic plates relate to volcanoes?\",\"answer\":\"Volcanoes are linked to where plates separate, collide, or slide, creating breaks in the crust that let magma rise. The Ring of Fire is the boundary where many volcanic openings occur.\"},{\"question\":\"What determines whether a volcano is active, extinct, or dormant?\",\"answer\":\"The classification depends on its state of activity. Active volcanoes erupt constantly, extinct volcanoes will never erupt again, and dormant volcanoes are inactive but expected to erupt in the future.\"}]","VOLCANOES - A hands-on science kit - VIOLENT VOLCANOES! | PDF",1790627046]