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Magma's Role in the Rock Cycle

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data-test-id="col" class="col-md-2"><h2 class="display-4 mb-1">ARTICLE</h2></div></div></div><div data-test-id="col" class="d-flex my-0 justify-content-end align-items-center col-2"></div></div><div data-test-id="row" class="g-0 row"><div data-test-id="col" class="d-none d-md-flex col-md-8"><h1 class="mt-2 pt-1 pt-lg-0 mt-lg-3 mb-0 ng-asset-page-title">Magma&#x27;s Role in the Rock Cycle</h1></div><div data-test-id="col" class="d-flex d-md-none my-0 col"><h1 class="mt-2 pt-1 mb-0 ng-asset-page-title">Magma&#x27;s Role in the Rock Cycle</h1></div></div><div data-test-id="row" class="g-0 row"><div data-test-id="col" class="d-flex mt-3 pt-1 pt-lg-0 px-0 col-md-8"><p>Magma is a mixture of molten and semi-molten rock found beneath the surface of the Earth.</p></div></div><div data-test-id="row" class="flex-column flex-md-row pt-0 pt-0 pt-lg-2 pb-0 row"><div data-test-id="col" class="pb-3 pb-md-0 col-md-3"><h3 class="display-4 mb-1" data-test-id="grades-text">Grades</h3><p class="m-0 text-small text-color-gray-900" data-test-id="grades-value">9 - 12+</p></div><div data-test-id="col" class="col-md-5"><h3 class="display-4 mb-1" data-test-id="subject-text">Subjects</h3><p class="m-0 text-small text-color-gray-900" data-test-id="subject-value">Earth Science, Geology, Geography, Physical Geography</p></div></div></div><div data-test-id="row" class="g-0 py-3 pt-md-5 pb-md-0 row"><div data-test-id="col" class="col-md-12"><div class="loading-wrapper"><div class="loading-info-panel p-3"><div data-test-id="skeleton"><span aria-live="polite" aria-busy="true"><span class="react-loading-skeleton loading-text" style="--base-color:#f5f5f5;--highlight-color:#fafafa">‌</span><br/></span></div><br/><div data-test-id="skeleton"><span aria-live="polite" aria-busy="true"><span class="react-loading-skeleton loading-text" style="--base-color:#f5f5f5;--highlight-color:#fafafa">‌</span><br/><span class="react-loading-skeleton loading-text" 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class="col-md-12"><div class="mt-3"><p><span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">Magma</span> is a <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">molten</span> and semi-molten <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">rock</span> mixture found under the surface of Earth. This mixture is usually made up of four parts: a hot <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">liquid</span> base, called the <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">melt</span>; <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">minerals</span> <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">crystallized</span> by the melt; solid rocks <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">incorporated</span> into the melt from the surrounding <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">confines</span>; and <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">dissolved</span> <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">gases</span>. </p><p>When magma is <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">ejected</span> by a <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">volcano</span> or other <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">vent</span>, the material is called <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">lava</span>. Magma that has cooled into a solid is called <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">igneous rock</span>. </p><p>Magma is extremely hot—between 700° and 1,300° Celsius (1,292° and 2,372° Fahrenheit). This heat makes magma a very <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">fluid</span> and <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">dynamic</span> substance, able to create new <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">landforms</span> and <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">engage</span> physical and chemical <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">transformations</span> in a variety of different <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">environments</span>. </p><p></p><p><strong>How Magma Forms</strong> </p><p>Earth is divided into three general layers. The <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">core</span> is the superheated center, the <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">mantle</span> is the thick, middle layer, and the <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">crust</span> is the top layer on which we live. </p><p>Magma <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">originates</span> in the lower part of Earth’s crust and in the upper portion of the mantle. Most of the mantle and crust are solid, so the presence of magma is <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">crucial</span> to understanding the <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">geology</span> and <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">morphology</span> of the mantle. </p><p>Differences in <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">temperature</span>, <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">pressure</span>, and structural formations in the mantle and crust cause magma to form in different ways. </p><p></p><p><span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0"><em>Decompression Melting</em></span></p><p>Decompression melting involves the upward movement of Earth&#x27;s mostly solid mantle. This hot material rises to an area of lower pressure through the process of <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">convection</span>. Areas of lower pressure always have a lower <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">melting point</span> than areas of high pressure. This reduction in overlying pressure, or decompression, enables the mantle rock to melt and form magma. </p><p>Decompression melting often occurs at divergent boundaries, where <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">tectonic plates</span> separate. The <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">rifting</span> movement causes the <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">buoyant</span> magma below to rise and fill the space of lower pressure. The rock then cools into new crust. </p><p>Decompression melting also occurs at mantle plumes, columns of hot rock that rise from Earth’s high-pressure core to its lower-pressure crust. When located beneath the ocean, these plumes, also known as <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">hot spots</span>, push magma onto the <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">seafloor</span>. These volcanic mounds can grow into <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">volcanic islands</span> over millions of years of activity. </p><p></p><p><em>Transfer of Heat</em></p><p>Magma can also be created when hot, liquid rock <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">intrudes</span> into Earth’s cold crust. As the liquid rock solidifies, it loses its heat to the surrounding crust. Much like hot fudge being poured over cold ice cream, this transfer of heat is able to melt the surrounding rock (the “ice cream”) into magma. </p><p>Transfer of heat often happens at convergent boundaries, where tectonic plates are crashing together. As the <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">denser</span> tectonic plate <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">subducts</span>, or sinks below, or the less-dense tectonic plate, hot rock from below can intrude into the cooler plate above. This process transfers heat and creates magma. Over millions of years, the magma in this <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">subduction zone</span> can create a series of active volcanoes known as a <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">volcanic arc</span>. </p><p>Flux melting occurs when water or carbon dioxide are added to rock. These compounds cause the rock to melt at lower temperatures. This creates magma in places where it originally maintained a solid structure.</p><p> </p><p><span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0"><em>Flux Melting</em></span></p><p>Much like heat transfer, flux melting also occurs around subduction zones. In this case, water overlying the subducting seafloor would lower the melting temperature of the mantle, generating magma that rises to the surface. </p><p></p><p><strong>Magma Escape Routes</strong> </p><p>Magma leaves the confines of the upper mantle and crust in two major ways: as an intrusion or as an extrusion. An intrusion can form features such as <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">dikes</span> and <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">xenoliths</span>. An extrusion could include lava and volcanic rock. </p><p>Magma can intrude into a low-density area of another geologic formation, such as a <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">sedimentary rock</span> structure. When it cools to solid rock, this intrusion is often called a <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">pluton</span>. A pluton is an intrusion of magma that wells up from below the surface. </p><p>Plutons can include dikes and xenoliths. A magmatic dike is simply a large slab of magmatic material that has intruded into another rock body. A xenolith is a piece of rock trapped in another type of rock. Many xenoliths are crystals torn from inside the Earth and <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">embedded</span> in magma while the magma was cooling. </p><p>The most familiar way for magma to escape, or <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">extrude</span>, to Earth’s surface is through lava. Lava <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">eruptions</span> can be “fire fountains” of liquid rock or thick, slow-moving rivers of molten material. Lava cools to form volcanic rock as well as <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">volcanic glass</span>. </p><p>Magma can also extrude into Earth’s <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">atmosphere</span> as part of a violent volcanic <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">explosion</span>. This magma solidifies in the air to form volcanic rock called <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">tephra</span>. In the atmosphere, tephra is more often called <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">volcanic ash</span>. As it falls to Earth, tephra includes rocks such as <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">pumice</span>. </p><p></p><p><span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0"><strong>Magma Chamber</strong></span> </p><p>In areas where temperature, pressure, and structural formation allow, magma can collect in magma chambers. Most magma chambers sit far beneath the surface of the Earth. </p><p>The pool of magma in a magma chamber is layered. The least-dense magma rises to the top. The densest magma sinks near the bottom of the chamber. Over millions of years, many magma chambers simply cool to form a pluton or large igneous intrusion. </p><p>If a magma chamber <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">encounters</span> an <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">enormous</span> amount of pressure, however, it may <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">fracture</span> the rock around it. The cracks, called <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">fissures</span> or vents, are tell-tale signs of a volcano. Many volcanoes sit over magma chambers. </p><p>As a volcano’s magma chamber experiences greater pressure, often due to more magma seeping into the chamber, the volcano may undergo an eruption. An eruption <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">reduces</span> the pressure inside the magma chamber. As long as more magma pools into a volcano’s magma chamber, there is the possibility of an eruption and the volcano will remain active. </p><p>Large eruptions can nearly empty the magma chamber. The layers of magma may be <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">documented</span> by the type of eruption material the volcano <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">emits</span>. Gases, ash, and light-colored rock are emitted first, from the least-dense, top layer of the magma chamber. Dark, dense volcanic rock from the lower part of the magma chamber may be released later. </p><p>In violent eruptions, the volume of magma shrinks so much that the entire magma chamber collapses and forms a <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">caldera</span>. </p><p></p><p><strong>Types of Magma </strong></p><p>All magma contains gases and a mixture of simple <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">elements</span>. Being that oxygen and silicon are the most <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">abundant</span> elements in magma, geologists define magma types in terms of their <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">silica</span> content, expressed as SiO2. These differences in chemical composition are directly related to differences in gas content, temperature, and <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">viscosity</span>. </p><p></p><p><em><span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">Mafic</span> Magma</em></p><p>Mafic magma has relatively low silica content, roughly 50%, and higher contents in iron and magnesium. This type of magma has a low gas content and low viscosity, or resistance to flow. Mafic magma also has high <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">mean</span> temperatures, between 1000o and 2000o Celsius (1832° and 3632° Fahrenheit), which contributes to its lower viscosity. </p><p>Low viscosity means that mafic magma is the most fluid of magma types. It erupts non-explosively and moves very quickly when it reaches Earth’s surface as lava. This lava cools into <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">basalt</span>, a rock that is heavy and dark in color due to its higher iron and magnesium levels. Basalt is one of the most common rocks in Earth’s crust as well as the volcanic islands created by hot spots. The Hawaiian Islands are a direct result of mafic magma eruptions. Steady and relatively calm “<span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">lava fountains</span>” continue to change and expand the “Big Island” of Hawaii. </p><p></p><p><em>Intermediate Magma</em></p><p>Intermediate magma has higher silica content (roughly 60%) than mafic magma. This results in a higher gas content and viscosity. Its mean temperature ranges from 800° to 1000° Celsius (1472° to 1832° Fahrenheit). </p><p>As a result of its higher viscosity and gas content, intermediate magma builds up pressure below the Earth’s surface before it can be released as lava. This more gaseous and sticky lava tends to explode violently and cools as <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">andesite</span> rock. Intermediate magma most commonly transforms into andesite due to the transfer of heat at convergent plate boundaries. Andesitic rocks are often found at <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">continental</span> volcanic arcs, such as the Andes Mountains in South America, after which they are named. </p><p></p><p><em><span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">Felsic</span> Magma</em></p><p>Felsic magma has the highest silica content of all magma types, between 65-70%. As a result, felsic magma also has the highest gas content and viscosity, and lowest mean temperatures, between 650° and 800° Celsius (1202° and 1472° Fahrenheit). </p><p>Thick, <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">viscous</span> felsic magma can trap gas bubbles in a volcano’s magma chamber. These trapped bubbles can cause explosive and <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">destructive</span> eruptions. These eruptions eject lava violently into the air, which cools into <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">dacite</span> and <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">rhyolite</span> rock. Much like intermediate magma, felsic magma may be most commonly found at convergent plate boundaries where transfer of heat and flux melting create large <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">stratovolcanoes</span>.</p><p>Magma can intrude into a low-density area of another geologic formation, such as a <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">sedimentary rock</span> structure. When it cools to solid rock, this intrusion is often called a <span class="cursor-pointer text-nowrap glossified-term" data-test-id="glossified" tabindex="0">pluton</span>. A pluton is an intrusion of magma that wells up from below the surface. </p></div></div><div data-test-id="col" class="col-md-12"><div data-test-id="container" class="border bg-light mt-4 mb-3 p-4 pb-3 container"><p class="display-4">Fast Fact</p><div data-test-id="container" class="container"><p><strong>Hawaii&#x27;s Molten Magma</strong><br/>Hawaiian magma is different than magma in other parts of the Earth because it has more molten rock and less dissolved gases and rock fragments. The Hawaiian volcano Kilauea, on the &quot;Big Island&quot; of Hawaii, has erupted with enough molten lava to pave a road around the Earth three times.</p></div></div><div data-test-id="container" class="border bg-light mt-4 mb-3 p-4 pb-3 container"><p class="display-4">Fast Fact</p><div data-test-id="container" class="container"><div><p><strong>Mysterious Magma</strong></p><p>Magma is usually studied as lava or igneous rock. But most magma remains molten or partly molten beneath Earth’s surface. In fact, magma has only been discovered three times in its “natural” habitat deep in Earth’s crust. Geothermal drilling projects discovered two magma sites on the “Big Island” of Hawai&#x27;i, and one on Iceland.</p></div></div></div><div data-test-id="container" class="border bg-light mt-4 mb-3 p-4 pb-3 container"><p class="display-4">Fast Fact</p><div data-test-id="container" class="container"><div><p><strong>Tapping into Magma’s Potential</strong></p><p>In 2009, the Icelandic Deep Drilling Project created a well that uses magma to generate geothermal energy. Normally, geothermal energy is created by pumping water into hot volcanic bedrock, creating steam that is then harnessed to generate electricity. While normal geothermal sources average around 60° to 80° Celsius (140° to 176° Fahrenheit), the magma well’s steam reached a record-breaking temperature of 450° Celsius (842° Fahrenheit)! This huge increase in temperature allowed just one magma well to generate roughly 36 megawatts of electricity, powering 36,000 homes. In comparison, one single wind turbine generates between one to three megawatts.</p></div></div></div></div><div data-test-id="col" class="col-md-12"><div><h6 class="mt-4 fw-bold">Articles &amp; Profiles</h6><div data-test-id="list" class="list-group-padding-m list-group-no-borders-no-dividers list-group-block-hover list-group"><a data-test-id="listItem" href="https://www.nationalgeographic.com/science/article/100923-science-early-earth-core-magma-liquid-molten-layer" data-rr-ui-event-key="https://www.nationalgeographic.com/science/article/100923-science-early-earth-core-magma-liquid-molten-layer" class="list-group-item">National Geographic Science: New Magma Layer Found Deep in Earth&#x27;s Mantle?</a><a data-test-id="listItem" href="https://www.nationalgeographic.com/science/article/110119-yellowstone-park-supervolcano-eruption-magma-science" data-rr-ui-event-key="https://www.nationalgeographic.com/science/article/110119-yellowstone-park-supervolcano-eruption-magma-science" class="list-group-item">National Geographic Science: Yellowstone Has Bulged as Magma Pocket Swells</a><a data-test-id="listItem" href="https://www.nsf.gov/news/news_summ.jsp?cntn_id=126475" data-rr-ui-event-key="https://www.nsf.gov/news/news_summ.jsp?cntn_id=126475" class="list-group-item">National Science Foundation: Magma in Earth&#x27;s Mantle Forms Deeper Than Once Thought</a></div></div><div><h6 class="mt-4 fw-bold">Reference</h6><div data-test-id="list" class="list-group-padding-m list-group-no-borders-no-dividers list-group-block-hover list-group"><a data-test-id="listItem" href="https://www2.tulane.edu/~sanelson/Natural_Disasters/volcan&amp;magma.htm" data-rr-ui-event-key="https://www2.tulane.edu/~sanelson/Natural_Disasters/volcan&amp;magma.htm" class="list-group-item">Tulane University: Volcanoes, Magma, and Volcanic Eruptions</a></div></div><div><h6 class="mt-4 fw-bold">Website</h6><div data-test-id="list" class="list-group-padding-m list-group-no-borders-no-dividers list-group-block-hover list-group"><a data-test-id="listItem" href="https://volcanoes.sdsu.edu/" data-rr-ui-event-key="https://volcanoes.sdsu.edu/" class="list-group-item">San Diego State University: How Volcanoes Work</a></div></div></div></div></div></div></div></div></div></div></div><div data-test-id="row" class="g-0 mx-md-3 justify-content-center py-3 pt-md-5 pb-md-0 row"><div data-test-id="col" class="col-lg-8 col-md-10 col-12"><div data-test-id="accordion" class="mb-3 accordion"><div class="accordion-item"><div data-test-id="accordion-0" class="card-light shadow-none card"><div data-test-id="accordion-toggle" aria-controls="credits-accordion-0-content" id="credits-accordion-0-toggle" role="button" tabindex="0" aria-expanded="false" class="accordion-has-icon cursor-pointer accordion-toggle accordion-button collapsed"><div class="card-title"><h5 class="m-0 fw-bold accordion-title">Credits</h5></div></div><div data-test-id="accordion-collapse" aria-labelledby="credits-accordion-0-toggle" id="credits-accordion-0-content" class="accordion-collapse collapse"><div class="card-body"><h6 class="mb-3 mt-4 fw-bold">Media Credits</h6><p>The audio, illustrations, photos, and videos are credited beneath the media asset, except for promotional images, which generally link to another page that contains the media credit. 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The Hawaiian volcano Kilauea, on the \"Big Island\" of Hawaii, has erupted with enough molten lava to pave a road around the Earth three times.","_key":"a8a57d3b65bc1"}],"_type":"block","style":"normal","_key":"a8a57d3b65bc"}],[{"children":[{"_type":"span","marks":["strong"],"text":"Mysterious Magma","_key":"622bc3cce7a40"}],"_type":"block","style":"normal","_key":"622bc3cce7a4","markDefs":[]},{"_type":"block","style":"normal","_key":"0773c5a3dc7c","markDefs":[],"children":[{"_type":"span","marks":[],"text":"Magma is usually studied as lava or igneous rock. But most magma remains molten or partly molten beneath Earth’s surface. In fact, magma has only been discovered three times in its “natural” habitat deep in Earth’s crust. Geothermal drilling projects discovered two magma sites on the “Big Island” of Hawai'i, and one on Iceland.","_key":"5679059ddf6d"}]}],[{"style":"normal","_key":"6e090ba3443a","markDefs":[],"children":[{"_type":"span","marks":["strong"],"text":"Tapping into Magma’s Potential","_key":"6e090ba3443a0"}],"_type":"block"},{"children":[{"_type":"span","marks":[],"text":"In 2009, the Icelandic Deep Drilling Project created a well that uses magma to generate geothermal energy. Normally, geothermal energy is created by pumping water into hot volcanic bedrock, creating steam that is then harnessed to generate electricity. While normal geothermal sources average around 60° to 80° Celsius (140° to 176° Fahrenheit), the magma well’s steam reached a record-breaking temperature of 450° Celsius (842° Fahrenheit)! This huge increase in temperature allowed just one magma well to generate roughly 36 megawatts of electricity, powering 36,000 homes. 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