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What is a Stratovolcano (Composite Cone)? - Earth How

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aria-current="page">What is a Stratovolcano (Composite Cone)?</span></span></div><h1 class="entry-title">What is a Stratovolcano (Composite Cone)?</h1><div class="entry-meta entry-meta-divider-customicon"> <div class="meta-comments"><span class="kadence-svg-iconset"><svg class="kadence-svg-icon kadence-comments-alt-svg" fill="currentColor" version="1.1" xmlns="http://www.w3.org/2000/svg" width="28" height="28" viewBox="0 0 28 28"><title>Comments</title><path d="M10 14c0 1.109-0.891 2-2 2s-2-0.891-2-2 0.891-2 2-2 2 0.891 2 2zM16 14c0 1.109-0.891 2-2 2s-2-0.891-2-2 0.891-2 2-2 2 0.891 2 2zM22 14c0 1.109-0.891 2-2 2s-2-0.891-2-2 0.891-2 2-2 2 0.891 2 2zM14 6c-6.5 0-12 3.656-12 8 0 2.328 1.563 4.547 4.266 6.078l1.359 0.781-0.422 1.5c-0.297 1.109-0.688 1.969-1.094 2.688 1.578-0.656 3.016-1.547 4.297-2.672l0.672-0.594 0.891 0.094c0.672 0.078 1.359 0.125 2.031 0.125 6.5 0 12-3.656 12-8s-5.5-8-12-8zM28 14c0 5.531-6.266 10-14 10-0.766 0-1.531-0.047-2.266-0.125-2.047 1.813-4.484 3.094-7.187 3.781-0.562 0.156-1.172 0.266-1.781 0.344h-0.078c-0.313 0-0.594-0.25-0.672-0.594v-0.016c-0.078-0.391 0.187-0.625 0.422-0.906 0.984-1.109 2.109-2.047 2.844-4.656-3.219-1.828-5.281-4.656-5.281-7.828 0-5.516 6.266-10 14-10v0c7.734 0 14 4.484 14 10z"></path> </svg></span><a class="meta-comments-link anchor-scroll" href="#comments">2 Comments</a></div></div></header> <div class="entry-content single-content"> <figure class="wp-block-image is-style-default"><img fetchpriority="high" decoding="async" width="900" height="657" src="https://earthhow.com/wp-content/uploads/2019/07/Stratovolcano-900x657.png" alt="Stratovolcano" class="wp-image-9181" srcset="https://earthhow.com/wp-content/uploads/2019/07/Stratovolcano-900x657.png 900w, https://earthhow.com/wp-content/uploads/2019/07/Stratovolcano-300x219.png 300w, https://earthhow.com/wp-content/uploads/2019/07/Stratovolcano-675x493.png 675w, https://earthhow.com/wp-content/uploads/2019/07/Stratovolcano-425x310.png 425w, https://earthhow.com/wp-content/uploads/2019/07/Stratovolcano-550x401.png 550w, https://earthhow.com/wp-content/uploads/2019/07/Stratovolcano-850x620.png 850w, https://earthhow.com/wp-content/uploads/2019/07/Stratovolcano.png 1036w" sizes="(max-width: 900px) 100vw, 900px"/></figure> <div class="wp-block-group" style="padding-top:var(--wp--preset--spacing--30);padding-bottom:var(--wp--preset--spacing--30)"><div class="wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained"> <h3 class="wp-block-heading">What are the characteristics of a stratovolcano?</h3> <p>The stratovolcano is a tall, steep, and cone-shaped type of volcano. Unlike flat shield volcanoes like in Hawaii, they have higher peaks. At the peak, stratovolcanoes usually have a small crater.</p> <p>Stratovolcanoes build up on height by <a href="https://earthhow.com/lava-magma-difference/">layering lava</a>, ash, and tephra. By definition, they have alternating layers of pyroclastics and lava.</p> <p>When ash falls or lava flows, it solidifies and makes a narrower cone. Lava is high viscosity so it&#8217;s steep-sided. But shield volcanoes have lava that runs all the way down the side of the volcano.</p></div></div><div class="wp-block-group" style="padding-top:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50)"><div class="wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained"> <h3 class="wp-block-heading">How do stratovolcanoes work?</h3> <p>At subduction zones, both land and water dive into continents. Then, water enters into a <a href="https://earthhow.com/parts-of-a-volcano/">magma chamber</a> and becomes superheated.</p> <p>At this point, it helps heat up the magma and make it easier to rise to the surface. Eventually, gases are trapped. Then, pressure builds. It&#8217;s less dense so they erupt violently.</p> <div class="wp-block-image is-style-default"> <figure class="aligncenter"><img decoding="async" width="550" height="408" src="https://earthhow.com/wp-content/uploads/2017/08/Ring-Of-Fire-550x408.png" alt="Ring of Fire" class="wp-image-206" srcset="https://earthhow.com/wp-content/uploads/2017/08/Ring-Of-Fire-550x408.png 550w, https://earthhow.com/wp-content/uploads/2017/08/Ring-Of-Fire-300x223.png 300w, https://earthhow.com/wp-content/uploads/2017/08/Ring-Of-Fire-675x501.png 675w, https://earthhow.com/wp-content/uploads/2017/08/Ring-Of-Fire-425x315.png 425w, https://earthhow.com/wp-content/uploads/2017/08/Ring-Of-Fire-850x631.png 850w, https://earthhow.com/wp-content/uploads/2017/08/Ring-Of-Fire-80x60.png 80w, https://earthhow.com/wp-content/uploads/2017/08/Ring-Of-Fire.png 1046w" sizes="(max-width: 550px) 100vw, 550px"/></figure></div><p><strong>Pyroclastic flow</strong> is deadly because it&#8217;s fast, hot, and poisonous. This type of flow can travel at speeds up to 700 mph. But stratovolcanoes run through cycles with lots of small eruptions.</p> <p>Even though the conduit is the main pipe from the magma chamber to the summit, lava can also go through a dyke or fissure to a side vent.</p></div></div><div class="wp-block-group" style="padding-top:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50)"><div class="wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained"> <h3 class="wp-block-heading">What are examples of stratovolcanoes?</h3> <p>Most stratovolcanoes are at <a href="https://earthhow.com/convergent-plate-boundaries-tectonics/">subduction zones</a>. If you travel along the Ring of Fire, these are mostly this type of volcano. The Ring of Fire is just a string of subduction zone volcanoes surrounding the Pacific Ocean.</p> <p>The Pacific Ocean seafloor is subducting under the continents. It brings water causing eruptions from stratovolcanoes. This includes the deadliest volcanoes in Indonesia, Japan, and the Philippines.</p> <p>Here are some examples of stratovolcanoes in the <a href="https://earthhow.com/pacific-ring-of-fire-volcanoes/">Pacific Ring of Fire</a>:</p> <ul class="wp-block-list"> <li><strong>MOUNT FUJI:</strong> Mount Fuji is a dormant stratovolcano that last erupted in the early 1700s.</li> <li><strong>MOUNT RAINIER:</strong> Mount Rainier is a stratovolcano and is the tallest mountain in the state of Washington.</li> <li><strong>ANDES MOUNTAINS:</strong> The Andes Mountains run along the western side of South America and are dominated by stratovolcano.</li> <li><strong>INDONESIA</strong>: Indonesia is the most volcanically active including Mount Krakatoa which catastrophically erupted in 1883.</li> <li><strong>CASCADES</strong>: The Cascades are a long chain of stratovolcanoes in Washington, Oregon, and Central California.</li> </ul> <div class="wp-block-image size-medium_plus wp-image-9294 is-style-default"> <figure class="aligncenter"><img decoding="async" width="550" height="274" src="https://earthhow.com/wp-content/uploads/2019/07/Mount-Baker-550x274.png" alt="Mount Baker" class="wp-image-9294" srcset="https://earthhow.com/wp-content/uploads/2019/07/Mount-Baker-550x274.png 550w, https://earthhow.com/wp-content/uploads/2019/07/Mount-Baker-300x149.png 300w, https://earthhow.com/wp-content/uploads/2019/07/Mount-Baker-675x336.png 675w, https://earthhow.com/wp-content/uploads/2019/07/Mount-Baker-425x212.png 425w, https://earthhow.com/wp-content/uploads/2019/07/Mount-Baker.png 837w" sizes="(max-width: 550px) 100vw, 550px"/></figure></div></div></div><div class="wp-block-group" style="padding-top:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50)"><div class="wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained"> <h3 class="wp-block-heading">What is the neck of a stratovolcano?</h3> <p>Over time, stratovolcanoes erode away from wind and water. The pyroclastics and ash erode quicker than the solid plug. They&#8217;re loose and get stripped away. What remains is the solid rock conduit sticking out of the ground. This is called a &#8220;neck&#8221;.</p> <ul class="wp-block-list"> <li><strong>SHIPROCK:</strong> Shiprock in New Mexico has a remnant neck and dyke eroded away.</li> <li><strong>DEVILS TOWER:</strong> Devil&#8217;s Tower was considered an ancient volcano. But recently, geologists believe it&#8217;s an igneous intrusion that formed underground from molten rock.</li> </ul> <p>Overall, Devil&#8217;s Tower and Shiprock are both prominent geological features known as volcanic necks, remnants of ancient stratovolcanoes where the softer surrounding rock eroded away, leaving behind these distinctive and resistant volcanic plugs.</p></div></div><div class="wp-block-group" style="padding-top:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50)"><div class="wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained"> <h3 class="wp-block-heading">What is a stratovolcano?</h3> <p>The stratovolcano is a type of volcano that rises above the Earth&#8217;s surface in a conical or cylindrical shape.</p> <p>They are constructed by many layers of hardened lava, volcanic ash, and volcanic bombs called tephra.</p> <p>Please use the comment form below to get in touch with us if you have questions about 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Type" decoding="async" loading="lazy" srcset="https://earthhow.com/wp-content/uploads/2018/09/Convergent-Plate-Tectonics-Type-0-300x225.png 300w, https://earthhow.com/wp-content/uploads/2018/09/Convergent-Plate-Tectonics-Type-0-675x507.png 675w, https://earthhow.com/wp-content/uploads/2018/09/Convergent-Plate-Tectonics-Type-0-425x319.png 425w, https://earthhow.com/wp-content/uploads/2018/09/Convergent-Plate-Tectonics-Type-0-550x413.png 550w, https://earthhow.com/wp-content/uploads/2018/09/Convergent-Plate-Tectonics-Type-0.png 678w, https://earthhow.com/wp-content/uploads/2018/09/Convergent-Plate-Tectonics-Type-0-326x245.png 326w, https://earthhow.com/wp-content/uploads/2018/09/Convergent-Plate-Tectonics-Type-0-80x60.png 80w, https://earthhow.com/wp-content/uploads/2018/09/Convergent-Plate-Tectonics-Type-0-267x200.png 267w" sizes="(max-width: 300px) 100vw, 300px"/></a></div></div></div><div class="kt-blocks-post-grid-item-inner"><header><h6 class="entry-title"><a href="https://earthhow.com/convergent-plate-boundaries-tectonics/">Convergent Plate Boundaries: The Collision of Plate Tectonics</a></h6><div class="kt-blocks-post-top-meta"></div></header><div class="entry-content"></div><footer class="kt-blocks-post-footer"><div class="kt-blocks-post-footer-left"></div><div class="kt-blocks-post-footer-right"></div></footer></div></div></article></div></div></div></div></div></div></div></div></article> <div id="comments" class="comments-area"> <h2 class="comments-title">2 Comments</h2> <ol class="comment-list"> <li id="comment-42013" class="comment even thread-even depth-1"> <article id="div-comment-42013" class="comment-body"> <footer class="comment-meta"> <div class="comment-author vcard"> <b class="fn">Some kid</b> <span class="says">says:</span></div><div class="comment-metadata"> <a href="https://earthhow.com/stratovolcano/#comment-42013"><time datetime="2024-10-02T11:18:45-06:00">October 2, 2024 at 11:18 am</time></a></div></footer> <div class="comment-content"> <p>The Black Tusk Stratovolcano is the oldest maybe not the first</p></div></article> </li> <li id="comment-17404" class="comment odd alt thread-odd thread-alt depth-1"> <article id="div-comment-17404" class="comment-body"> <footer class="comment-meta"> <div class="comment-author vcard"> <b class="fn">Martha Evans</b> <span class="says">says:</span></div><div class="comment-metadata"> <a href="https://earthhow.com/stratovolcano/#comment-17404"><time datetime="2022-10-16T21:21:40-06:00">October 16, 2022 at 9:21 pm</time></a></div></footer> <div class="comment-content"> <p>What was the world&#8217;s first stratovolcano?</p></div></article> </li> </ol> <div id="respond" class="comment-respond"> <h3 id="reply-title" class="comment-reply-title">Leave a Reply</h3><form action="https://earthhow.com/wp-comments-post.php" method="post" id="commentform" class="comment-form" novalidate><p class="comment-notes"><span id="email-notes">Your email address will not be 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