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Magma chamber - Wikipedia
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id="siteNotice"></div> </div> <div class="pre-content heading-holder"> <div class="page-heading"> <h1 id="firstHeading" class="firstHeading mw-first-heading"><span class="mw-page-title-main">Magma chamber</span></h1> <div class="tagline"></div> </div> <ul id="p-associated-pages" class="minerva__tab-container"> <li class="minerva__tab selected"> <a class="minerva__tab-text" href="/wiki/Magma_chamber" rel="" data-event-name="tabs.subject">Article</a> </li> <li class="minerva__tab "> <a class="minerva__tab-text" href="/wiki/Talk:Magma_chamber" rel="discussion" data-event-name="tabs.talk">Talk</a> </li> </ul> <nav class="page-actions-menu"> <ul id="p-views" class="page-actions-menu__list"> <li id="language-selector" class="page-actions-menu__list-item"> <a role="button" href="#p-lang" data-mw="interface" data-event-name="menu.languages" title="Language" class="cdx-button cdx-button--size-large cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--icon-only 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minerva-icon--edit"></span> <span>Edit</span> </a> </li> </ul> </nav> <!-- version 1.0.2 (change every time you update a partial) --> <div id="mw-content-subtitle"></div> </div> <div id="bodyContent" class="content"> <div id="mw-content-text" class="mw-body-content"><script>function mfTempOpenSection(id){var block=document.getElementById("mf-section-"+id);block.className+=" open-block";block.previousSibling.className+=" open-block";}</script><div class="mw-content-ltr mw-parser-output" lang="en" dir="ltr"><section class="mf-section-0" id="mf-section-0"> <p class="mw-empty-elt"> </p> <p>A <b>magma chamber</b> is a large pool of liquid <a href="/wiki/Rock_(geology)" title="Rock (geology)">rock</a> beneath the surface of the Earth. The molten rock, or <a href="/wiki/Magma" title="Magma">magma</a>, in such a chamber is less dense than the surrounding <a href="/wiki/Country_rock_(geology)" title="Country rock (geology)">country rock</a>, which produces <a href="/wiki/Buoyancy" title="Buoyancy">buoyant forces</a> on the magma that tend to drive it upwards.<sup id="cite_ref-1" class="reference"><a href="#cite_note-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> If the magma finds a path to the surface, then the result will be a <a href="/wiki/Volcanic_eruption" class="mw-redirect" title="Volcanic eruption">volcanic eruption</a>; consequently, many <a href="/wiki/Volcano" title="Volcano">volcanoes</a> are situated over magma chambers.<sup id="cite_ref-2" class="reference"><a href="#cite_note-2"><span class="cite-bracket">[</span>2<span class="cite-bracket">]</span></a></sup> These chambers are hard to detect deep within the Earth, and therefore most of those known are close to the surface, commonly between 1 km and 10 km down.<sup id="cite_ref-3" class="reference"><a href="#cite_note-3"><span class="cite-bracket">[</span>3<span class="cite-bracket">]</span></a></sup> </p><figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Vulcanian_Eruption-numbers.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/d/dc/Vulcanian_Eruption-numbers.svg/220px-Vulcanian_Eruption-numbers.svg.png" decoding="async" width="220" height="220" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/d/dc/Vulcanian_Eruption-numbers.svg/330px-Vulcanian_Eruption-numbers.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/d/dc/Vulcanian_Eruption-numbers.svg/440px-Vulcanian_Eruption-numbers.svg.png 2x" data-file-width="1100" data-file-height="1100"></a><figcaption>11 – magma chamber</figcaption></figure> <div id="toc" class="toc" role="navigation" aria-labelledby="mw-toc-heading"><input type="checkbox" role="button" id="toctogglecheckbox" class="toctogglecheckbox" style="display:none"><div class="toctitle" lang="en" dir="ltr"><h2 id="mw-toc-heading">Contents</h2><span class="toctogglespan"><label class="toctogglelabel" for="toctogglecheckbox"></label></span></div> <ul> <li class="toclevel-1 tocsection-1"><a href="#Dynamics_of_magma_chambers"><span class="tocnumber">1</span> <span class="toctext">Dynamics of magma chambers</span></a></li> <li class="toclevel-1 tocsection-2"><a href="#Examples"><span class="tocnumber">2</span> <span class="toctext">Examples</span></a></li> <li class="toclevel-1 tocsection-3"><a href="#See_also"><span class="tocnumber">3</span> <span class="toctext">See also</span></a></li> <li class="toclevel-1 tocsection-4"><a href="#References"><span class="tocnumber">4</span> <span class="toctext">References</span></a></li> </ul> </div> </section><div class="mw-heading mw-heading2 section-heading" onclick="mfTempOpenSection(1)"><span class="indicator mf-icon mf-icon-expand mf-icon--small"></span><h2 id="Dynamics_of_magma_chambers">Dynamics of magma chambers</h2><span class="mw-editsection"> <a role="button" href="/w/index.php?title=Magma_chamber&action=edit&section=1" title="Edit section: Dynamics of magma chambers" class="cdx-button cdx-button--size-large cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--icon-only cdx-button--weight-quiet "> <span class="minerva-icon minerva-icon--edit"></span> <span>edit</span> </a> </span> </div><section class="mf-section-1 collapsible-block" id="mf-section-1"> <figure class="mw-default-size mw-halign-left" typeof="mw:File/Thumb"><a href="/wiki/File:Subduction-en.svg" class="mw-file-description"><noscript><img src="//upload.wikimedia.org/wikipedia/commons/thumb/c/ce/Subduction-en.svg/400px-Subduction-en.svg.png" decoding="async" width="400" height="230" class="mw-file-element" data-file-width="1482" data-file-height="854"></noscript><span class="lazy-image-placeholder" style="width: 400px;height: 230px;" data-src="//upload.wikimedia.org/wikipedia/commons/thumb/c/ce/Subduction-en.svg/400px-Subduction-en.svg.png" data-width="400" data-height="230" data-srcset="//upload.wikimedia.org/wikipedia/commons/thumb/c/ce/Subduction-en.svg/600px-Subduction-en.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/c/ce/Subduction-en.svg/800px-Subduction-en.svg.png 2x" data-class="mw-file-element"> </span></a><figcaption>Magma chambers above a subducting plate</figcaption></figure> <p>Magma rises through cracks from beneath and across the crust because it is less dense than the surrounding rock. When the magma cannot find a path upwards it pools into a magma chamber. These chambers are commonly built up over time,<sup id="cite_ref-4" class="reference"><a href="#cite_note-4"><span class="cite-bracket">[</span>4<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-5" class="reference"><a href="#cite_note-5"><span class="cite-bracket">[</span>5<span class="cite-bracket">]</span></a></sup> by successive horizontal<sup id="cite_ref-6" class="reference"><a href="#cite_note-6"><span class="cite-bracket">[</span>6<span class="cite-bracket">]</span></a></sup> or vertical<sup id="cite_ref-7" class="reference"><a href="#cite_note-7"><span class="cite-bracket">[</span>7<span class="cite-bracket">]</span></a></sup> magma injections. The influx of new magma causes reaction of pre-existing crystals<sup id="cite_ref-8" class="reference"><a href="#cite_note-8"><span class="cite-bracket">[</span>8<span class="cite-bracket">]</span></a></sup> and the pressure in the chamber to increase. </p><p>The residing magma starts to cool, with the higher melting point components such as <a href="/wiki/Olivine" title="Olivine">olivine</a> crystallizing out of the solution, particularly near to the cooler walls of the chamber, and forming a denser conglomerate of minerals which sinks (cumulative rock).<sup id="cite_ref-9" class="reference"><a href="#cite_note-9"><span class="cite-bracket">[</span>9<span class="cite-bracket">]</span></a></sup> Upon cooling, new mineral phases saturate and the rock type changes (e.g. <a href="/wiki/Fractional_crystallization_(geology)" title="Fractional crystallization (geology)">fractional crystallization</a>), typically forming (1) <a href="/wiki/Gabbro" title="Gabbro">gabbro</a>, <a href="/wiki/Diorite" title="Diorite">diorite</a>, <a href="/wiki/Tonalite" title="Tonalite">tonalite</a> and <a href="/wiki/Granite" title="Granite">granite</a> or (2) <a href="/wiki/Gabbro" title="Gabbro">gabbro</a>, <a href="/wiki/Diorite" title="Diorite">diorite</a>, <a href="/wiki/Syenite" title="Syenite">syenite</a> and <a href="/wiki/Granite" title="Granite">granite</a>. If magma resides in a chamber for a long period, then it can become stratified with lower <a href="/wiki/Density" title="Density">density</a> components rising to the top and denser materials sinking. Rocks accumulate in layers, forming a <a href="/wiki/Layered_intrusion" title="Layered intrusion">layered intrusion</a>.<sup id="cite_ref-10" class="reference"><a href="#cite_note-10"><span class="cite-bracket">[</span>10<span class="cite-bracket">]</span></a></sup> Any subsequent eruption may produce distinctly layered deposits; for example, the deposits from the <a href="/wiki/Eruption_of_Mount_Vesuvius_in_79" class="mw-redirect" title="Eruption of Mount Vesuvius in 79">79 AD eruption of Mount Vesuvius</a> include a thick layer of white <a href="/wiki/Pumice" title="Pumice">pumice</a> from the upper portion of the magma chamber overlaid with a similar layer of grey pumice produced from material erupted later from lower in the chamber. </p><p>Another effect of the cooling of the chamber is that the solidifying <a href="/wiki/Crystal" title="Crystal">crystals</a> will release the gas (primarily <a href="/wiki/Steam" title="Steam">steam</a>) previously dissolved when they were liquid, causing the pressure in the chamber to rise, possibly sufficiently to produce an eruption. Additionally, the removal of the lower melting point components will tend to make the magma more <a href="/wiki/Viscosity" title="Viscosity">viscous</a> (by increasing the concentration of <a href="/wiki/Silicate" title="Silicate">silicates</a>). Thus, stratification of a magma chamber may result in an increase in the amount of gas within the magma near the top of the chamber,<sup id="cite_ref-11" class="reference"><a href="#cite_note-11"><span class="cite-bracket">[</span>11<span class="cite-bracket">]</span></a></sup> and also make this magma more viscous, potentially leading to a more explosive eruption than would be the case had the chamber not become stratified. </p><p><a href="/wiki/Supervolcano" title="Supervolcano">Supervolcano</a> eruptions are possible only when an extraordinarily large magma chamber forms at a relatively shallow level in the crust. However, the rate of magma production in tectonic settings that produce supervolcanoes is quite low, around 0.002 km<sup>3</sup> year<sup>−1</sup>, so that accumulation of sufficient magma for a supereruption takes 10<sup>5</sup> to 10<sup>6</sup> years. This raises the question of why the buoyant silicic magma does not break through to the surface more frequently in relatively small eruptions. The combination of regional extension, which lowers the maximum attainable overpressure on the chamber roof, and a large magma chamber with warm walls, which has a high effective <a href="/wiki/Viscoelasticity" title="Viscoelasticity">viscoelasticity</a>, may suppress rhyolite dike formation and allow such large chambers to fill with magma.<sup id="cite_ref-jellinke-depaolo-2003_12-0" class="reference"><a href="#cite_note-jellinke-depaolo-2003-12"><span class="cite-bracket">[</span>12<span class="cite-bracket">]</span></a></sup> </p><p>If the magma is not vented to the surface in a volcanic eruption, it will slowly cool and crystallize at depth to form an <a href="/wiki/Intrusive_rock" title="Intrusive rock">intrusive</a> <a href="/wiki/Igneous" class="mw-redirect" title="Igneous">igneous</a> body, one, for example, composed of <a href="/wiki/Granite" title="Granite">granite</a> or <a href="/wiki/Gabbro" title="Gabbro">gabbro</a> (see also <a href="/wiki/Pluton" class="mw-redirect" title="Pluton">pluton</a>). </p><p>Often, a volcano may have a deep magma chamber many kilometers down, which supplies a shallower chamber near the summit. The location of magma chambers can be mapped using <a href="/wiki/Seismology" title="Seismology">seismology</a>: seismic waves from <a href="/wiki/Earthquakes" class="mw-redirect" title="Earthquakes">earthquakes</a> move more slowly through liquid rock than solid, allowing measurements to pinpoint the regions of slow movement which identify magma chambers.<sup id="cite_ref-13" class="reference"><a href="#cite_note-13"><span class="cite-bracket">[</span>13<span class="cite-bracket">]</span></a></sup> </p><p>As a volcano erupts, surrounding rock will collapse into the emptying chamber. If the chamber's size is reduced considerably, the resulting depression at the surface can form a <a href="/wiki/Caldera" title="Caldera">caldera</a>.<sup id="cite_ref-14" class="reference"><a href="#cite_note-14"><span class="cite-bracket">[</span>14<span class="cite-bracket">]</span></a></sup> </p> </section><div class="mw-heading mw-heading2 section-heading" onclick="mfTempOpenSection(2)"><span class="indicator mf-icon mf-icon-expand mf-icon--small"></span><h2 id="Examples">Examples</h2><span class="mw-editsection"> <a role="button" href="/w/index.php?title=Magma_chamber&action=edit&section=2" title="Edit section: Examples" class="cdx-button cdx-button--size-large cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--icon-only cdx-button--weight-quiet "> <span class="minerva-icon minerva-icon--edit"></span> <span>edit</span> </a> </span> </div><section class="mf-section-2 collapsible-block" id="mf-section-2"> <p>In Iceland, <a href="/wiki/Thrihnukagigur" title="Thrihnukagigur">Thrihnukagigur</a>, discovered in 1974 by <a href="/wiki/Caving" title="Caving">cave explorer</a> Árni B. Stefánsson and opened for tourism in 2012, is the only volcano in the world where visitors can take an elevator and safely descend into the magma chamber.<sup id="cite_ref-15" class="reference"><a href="#cite_note-15"><span class="cite-bracket">[</span>15<span class="cite-bracket">]</span></a></sup> </p> </section><div class="mw-heading mw-heading2 section-heading" onclick="mfTempOpenSection(3)"><span class="indicator mf-icon mf-icon-expand mf-icon--small"></span><h2 id="See_also">See also</h2><span class="mw-editsection"> <a role="button" href="/w/index.php?title=Magma_chamber&action=edit&section=3" title="Edit section: See also" class="cdx-button cdx-button--size-large cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--icon-only cdx-button--weight-quiet "> <span class="minerva-icon minerva-icon--edit"></span> <span>edit</span> </a> </span> </div><section class="mf-section-3 collapsible-block" id="mf-section-3"> <ul><li><a href="/wiki/Aquifer" title="Aquifer">Aquifer</a></li> <li><a href="/wiki/Kiyoo_Mogi#Mogi_model" title="Kiyoo Mogi">Mogi model</a></li></ul> </section><div class="mw-heading mw-heading2 section-heading" onclick="mfTempOpenSection(4)"><span class="indicator mf-icon mf-icon-expand mf-icon--small"></span><h2 id="References">References</h2><span class="mw-editsection"> <a role="button" href="/w/index.php?title=Magma_chamber&action=edit&section=4" title="Edit section: References" class="cdx-button cdx-button--size-large cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--icon-only cdx-button--weight-quiet "> <span class="minerva-icon minerva-icon--edit"></span> <span>edit</span> </a> </span> </div><section class="mf-section-4 collapsible-block" id="mf-section-4"> <style data-mw-deduplicate="TemplateStyles:r1239543626">.mw-parser-output .reflist{margin-bottom:0.5em;list-style-type:decimal}@media screen{.mw-parser-output .reflist{font-size:90%}}.mw-parser-output .reflist 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data-mw-deduplicate="TemplateStyles:r1238218222">.mw-parser-output cite.citation{font-style:inherit;word-wrap:break-word}.mw-parser-output .citation q{quotes:"\"""\"""'""'"}.mw-parser-output .citation:target{background-color:rgba(0,127,255,0.133)}.mw-parser-output .id-lock-free.id-lock-free a{background:url("//upload.wikimedia.org/wikipedia/commons/6/65/Lock-green.svg")right 0.1em center/9px no-repeat}.mw-parser-output .id-lock-limited.id-lock-limited a,.mw-parser-output .id-lock-registration.id-lock-registration a{background:url("//upload.wikimedia.org/wikipedia/commons/d/d6/Lock-gray-alt-2.svg")right 0.1em center/9px no-repeat}.mw-parser-output .id-lock-subscription.id-lock-subscription a{background:url("//upload.wikimedia.org/wikipedia/commons/a/aa/Lock-red-alt-2.svg")right 0.1em center/9px no-repeat}.mw-parser-output .cs1-ws-icon a{background:url("//upload.wikimedia.org/wikipedia/commons/4/4c/Wikisource-logo.svg")right 0.1em center/12px no-repeat}body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-free a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-limited a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-registration a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-subscription a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .cs1-ws-icon a{background-size:contain;padding:0 1em 0 0}.mw-parser-output .cs1-code{color:inherit;background:inherit;border:none;padding:inherit}.mw-parser-output .cs1-hidden-error{display:none;color:var(--color-error,#d33)}.mw-parser-output .cs1-visible-error{color:var(--color-error,#d33)}.mw-parser-output .cs1-maint{display:none;color:#085;margin-left:0.3em}.mw-parser-output .cs1-kern-left{padding-left:0.2em}.mw-parser-output .cs1-kern-right{padding-right:0.2em}.mw-parser-output .citation .mw-selflink{font-weight:inherit}@media screen{.mw-parser-output .cs1-format{font-size:95%}html.skin-theme-clientpref-night .mw-parser-output .cs1-maint{color:#18911f}}@media screen and (prefers-color-scheme:dark){html.skin-theme-clientpref-os .mw-parser-output .cs1-maint{color:#18911f}}</style><cite id="CITEREFPhilpottsAgue2009" class="citation book cs1">Philpotts, Anthony R.; Ague, Jay J. 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class="last-modified-bar__text modified-enhancement" data-user-name="Citation bot" data-user-gender="unknown" data-timestamp="1727499361"> <span>Last edited on 28 September 2024, at 04:56</span> </span> <span class="minerva-icon minerva-icon-size-small minerva-icon--expand"></span> </div> </a> <div class="post-content footer-content"> <div id='mw-data-after-content'> <div class="read-more-container"></div> </div> <div id="p-lang"> <h4>Languages</h4> <section> <ul id="p-variants" class="minerva-languages"></ul> <ul class="minerva-languages"><li class="interlanguage-link interwiki-ar mw-list-item"><a href="https://ar.wikipedia.org/wiki/%D8%AD%D8%AC%D8%B1%D8%A9_%D8%B5%D9%87%D8%A7%D8%B1%D9%8A%D8%A9" title="حجرة صهارية – Arabic" lang="ar" hreflang="ar" data-title="حجرة صهارية" data-language-autonym="العربية" data-language-local-name="Arabic" class="interlanguage-link-target"><span>العربية</span></a></li><li class="interlanguage-link interwiki-gn mw-list-item"><a href="https://gn.wikipedia.org/wiki/Tata_hu%27%C5%A9_%C3%B1emono%27%C3%B5" title="Tata hu'ũ ñemono'õ – Guarani" lang="gn" hreflang="gn" data-title="Tata hu'ũ ñemono'õ" data-language-autonym="Avañe'ẽ" data-language-local-name="Guarani" class="interlanguage-link-target"><span>Avañe'ẽ</span></a></li><li class="interlanguage-link interwiki-az mw-list-item"><a href="https://az.wikipedia.org/wiki/Vulkan_oca%C4%9F%C4%B1" title="Vulkan ocağı – Azerbaijani" lang="az" hreflang="az" data-title="Vulkan ocağı" data-language-autonym="Azərbaycanca" data-language-local-name="Azerbaijani" class="interlanguage-link-target"><span>Azərbaycanca</span></a></li><li class="interlanguage-link interwiki-ca mw-list-item"><a href="https://ca.wikipedia.org/wiki/Cambra_magm%C3%A0tica" title="Cambra magmàtica – Catalan" lang="ca" hreflang="ca" data-title="Cambra magmàtica" data-language-autonym="Català" data-language-local-name="Catalan" class="interlanguage-link-target"><span>Català</span></a></li><li class="interlanguage-link interwiki-cs mw-list-item"><a href="https://cs.wikipedia.org/wiki/Magmatick%C3%BD_krb" title="Magmatický krb – Czech" lang="cs" hreflang="cs" data-title="Magmatický krb" data-language-autonym="Čeština" data-language-local-name="Czech" class="interlanguage-link-target"><span>Čeština</span></a></li><li class="interlanguage-link interwiki-da mw-list-item"><a href="https://da.wikipedia.org/wiki/Magmakammer" title="Magmakammer – Danish" lang="da" hreflang="da" data-title="Magmakammer" data-language-autonym="Dansk" data-language-local-name="Danish" class="interlanguage-link-target"><span>Dansk</span></a></li><li class="interlanguage-link interwiki-de mw-list-item"><a href="https://de.wikipedia.org/wiki/Magmakammer" title="Magmakammer – German" lang="de" hreflang="de" data-title="Magmakammer" data-language-autonym="Deutsch" data-language-local-name="German" class="interlanguage-link-target"><span>Deutsch</span></a></li><li class="interlanguage-link interwiki-et mw-list-item"><a href="https://et.wikipedia.org/wiki/Magmakamber" title="Magmakamber – Estonian" lang="et" hreflang="et" data-title="Magmakamber" data-language-autonym="Eesti" data-language-local-name="Estonian" class="interlanguage-link-target"><span>Eesti</span></a></li><li class="interlanguage-link interwiki-es mw-list-item"><a href="https://es.wikipedia.org/wiki/C%C3%A1mara_magm%C3%A1tica" title="Cámara magmática – Spanish" lang="es" hreflang="es" data-title="Cámara magmática" data-language-autonym="Español" data-language-local-name="Spanish" class="interlanguage-link-target"><span>Español</span></a></li><li class="interlanguage-link interwiki-eo mw-list-item"><a href="https://eo.wikipedia.org/wiki/Magma_kameno" title="Magma kameno – Esperanto" lang="eo" hreflang="eo" data-title="Magma kameno" data-language-autonym="Esperanto" data-language-local-name="Esperanto" class="interlanguage-link-target"><span>Esperanto</span></a></li><li class="interlanguage-link interwiki-eu mw-list-item"><a href="https://eu.wikipedia.org/wiki/Ganbera_magmatiko" title="Ganbera magmatiko – Basque" lang="eu" hreflang="eu" data-title="Ganbera magmatiko" data-language-autonym="Euskara" data-language-local-name="Basque" class="interlanguage-link-target"><span>Euskara</span></a></li><li class="interlanguage-link interwiki-fa mw-list-item"><a href="https://fa.wikipedia.org/wiki/%D8%A7%D8%AA%D8%A7%D9%82%DA%A9_%D9%85%D8%A7%DA%AF%D9%85%D8%A7" title="اتاقک ماگما – Persian" lang="fa" hreflang="fa" data-title="اتاقک ماگما" data-language-autonym="فارسی" data-language-local-name="Persian" class="interlanguage-link-target"><span>فارسی</span></a></li><li class="interlanguage-link interwiki-fr mw-list-item"><a href="https://fr.wikipedia.org/wiki/Chambre_magmatique" title="Chambre magmatique – French" lang="fr" hreflang="fr" data-title="Chambre magmatique" data-language-autonym="Français" data-language-local-name="French" class="interlanguage-link-target"><span>Français</span></a></li><li class="interlanguage-link interwiki-gl mw-list-item"><a href="https://gl.wikipedia.org/wiki/C%C3%A1mara_magm%C3%A1tica" title="Cámara magmática – Galician" lang="gl" hreflang="gl" data-title="Cámara magmática" data-language-autonym="Galego" data-language-local-name="Galician" class="interlanguage-link-target"><span>Galego</span></a></li><li class="interlanguage-link interwiki-ko mw-list-item"><a href="https://ko.wikipedia.org/wiki/%EB%A7%88%EA%B7%B8%EB%A7%88%EA%B5%84" title="마그마굄 – Korean" lang="ko" hreflang="ko" data-title="마그마굄" data-language-autonym="한국어" data-language-local-name="Korean" class="interlanguage-link-target"><span>한국어</span></a></li><li class="interlanguage-link interwiki-id mw-list-item"><a href="https://id.wikipedia.org/wiki/Dapur_magma" title="Dapur magma – Indonesian" lang="id" hreflang="id" data-title="Dapur magma" data-language-autonym="Bahasa Indonesia" data-language-local-name="Indonesian" class="interlanguage-link-target"><span>Bahasa Indonesia</span></a></li><li class="interlanguage-link interwiki-is mw-list-item"><a href="https://is.wikipedia.org/wiki/Kviku%C3%BEr%C3%B3" title="Kvikuþró – Icelandic" lang="is" hreflang="is" data-title="Kvikuþró" data-language-autonym="Íslenska" data-language-local-name="Icelandic" class="interlanguage-link-target"><span>Íslenska</span></a></li><li class="interlanguage-link interwiki-it mw-list-item"><a href="https://it.wikipedia.org/wiki/Camera_magmatica" title="Camera magmatica – Italian" lang="it" hreflang="it" data-title="Camera magmatica" data-language-autonym="Italiano" data-language-local-name="Italian" class="interlanguage-link-target"><span>Italiano</span></a></li><li class="interlanguage-link interwiki-he mw-list-item"><a href="https://he.wikipedia.org/wiki/%D7%AA%D7%90_%D7%9E%D7%90%D7%92%D7%9E%D7%94" title="תא מאגמה – Hebrew" lang="he" hreflang="he" data-title="תא מאגמה" data-language-autonym="עברית" data-language-local-name="Hebrew" class="interlanguage-link-target"><span>עברית</span></a></li><li class="interlanguage-link interwiki-lt mw-list-item"><a href="https://lt.wikipedia.org/wiki/Magmos_%C5%BEidinys" title="Magmos židinys – Lithuanian" lang="lt" hreflang="lt" data-title="Magmos židinys" data-language-autonym="Lietuvių" data-language-local-name="Lithuanian" class="interlanguage-link-target"><span>Lietuvių</span></a></li><li class="interlanguage-link interwiki-mk mw-list-item"><a href="https://mk.wikipedia.org/wiki/%D0%9C%D0%B0%D0%B3%D0%BC%D0%B0%D1%82%D1%81%D0%BA%D0%BE_%D0%BE%D0%B3%D0%BD%D0%B8%D1%88%D1%82%D0%B5" title="Магматско огниште – Macedonian" lang="mk" hreflang="mk" data-title="Магматско огниште" data-language-autonym="Македонски" data-language-local-name="Macedonian" class="interlanguage-link-target"><span>Македонски</span></a></li><li class="interlanguage-link interwiki-ms mw-list-item"><a href="https://ms.wikipedia.org/wiki/Kebuk_magma" title="Kebuk magma – Malay" lang="ms" hreflang="ms" data-title="Kebuk magma" data-language-autonym="Bahasa Melayu" data-language-local-name="Malay" class="interlanguage-link-target"><span>Bahasa Melayu</span></a></li><li class="interlanguage-link interwiki-nl mw-list-item"><a href="https://nl.wikipedia.org/wiki/Magmakamer" title="Magmakamer – Dutch" lang="nl" hreflang="nl" data-title="Magmakamer" data-language-autonym="Nederlands" data-language-local-name="Dutch" class="interlanguage-link-target"><span>Nederlands</span></a></li><li class="interlanguage-link interwiki-ja mw-list-item"><a href="https://ja.wikipedia.org/wiki/%E3%83%9E%E3%82%B0%E3%83%9E%E6%BA%9C%E3%82%8A" title="マグマ溜り – Japanese" lang="ja" hreflang="ja" data-title="マグマ溜り" data-language-autonym="日本語" data-language-local-name="Japanese" class="interlanguage-link-target"><span>日本語</span></a></li><li class="interlanguage-link interwiki-no mw-list-item"><a href="https://no.wikipedia.org/wiki/Magmakammer" title="Magmakammer – Norwegian Bokmål" lang="nb" hreflang="nb" data-title="Magmakammer" data-language-autonym="Norsk bokmål" data-language-local-name="Norwegian Bokmål" class="interlanguage-link-target"><span>Norsk bokmål</span></a></li><li class="interlanguage-link interwiki-nn mw-list-item"><a href="https://nn.wikipedia.org/wiki/Magmakammer" title="Magmakammer – Norwegian Nynorsk" lang="nn" hreflang="nn" data-title="Magmakammer" data-language-autonym="Norsk nynorsk" data-language-local-name="Norwegian Nynorsk" class="interlanguage-link-target"><span>Norsk nynorsk</span></a></li><li class="interlanguage-link interwiki-nds mw-list-item"><a href="https://nds.wikipedia.org/wiki/Magmakamer" title="Magmakamer – Low German" lang="nds" hreflang="nds" data-title="Magmakamer" data-language-autonym="Plattdüütsch" data-language-local-name="Low German" class="interlanguage-link-target"><span>Plattdüütsch</span></a></li><li class="interlanguage-link interwiki-pl mw-list-item"><a href="https://pl.wikipedia.org/wiki/Komora_wulkaniczna" title="Komora wulkaniczna – Polish" lang="pl" hreflang="pl" data-title="Komora wulkaniczna" data-language-autonym="Polski" data-language-local-name="Polish" class="interlanguage-link-target"><span>Polski</span></a></li><li class="interlanguage-link interwiki-pt mw-list-item"><a href="https://pt.wikipedia.org/wiki/C%C3%A2mara_magm%C3%A1tica" title="Câmara magmática – Portuguese" lang="pt" hreflang="pt" data-title="Câmara magmática" data-language-autonym="Português" data-language-local-name="Portuguese" class="interlanguage-link-target"><span>Português</span></a></li><li class="interlanguage-link interwiki-ru mw-list-item"><a href="https://ru.wikipedia.org/wiki/%D0%9C%D0%B0%D0%B3%D0%BC%D0%B0%D1%82%D0%B8%D1%87%D0%B5%D1%81%D0%BA%D0%B0%D1%8F_%D0%BA%D0%B0%D0%BC%D0%B5%D1%80%D0%B0" title="Магматическая камера – Russian" lang="ru" hreflang="ru" data-title="Магматическая камера" data-language-autonym="Русский" data-language-local-name="Russian" class="interlanguage-link-target"><span>Русский</span></a></li><li class="interlanguage-link interwiki-simple mw-list-item"><a href="https://simple.wikipedia.org/wiki/Magma_chamber" title="Magma chamber – Simple English" lang="en-simple" hreflang="en-simple" data-title="Magma chamber" data-language-autonym="Simple English" data-language-local-name="Simple English" class="interlanguage-link-target"><span>Simple English</span></a></li><li class="interlanguage-link interwiki-sk mw-list-item"><a href="https://sk.wikipedia.org/wiki/Magmatick%C3%BD_kozub" title="Magmatický kozub – Slovak" lang="sk" hreflang="sk" data-title="Magmatický kozub" data-language-autonym="Slovenčina" data-language-local-name="Slovak" class="interlanguage-link-target"><span>Slovenčina</span></a></li><li class="interlanguage-link interwiki-sl mw-list-item"><a href="https://sl.wikipedia.org/wiki/Magmatsko_ognji%C5%A1%C4%8De" title="Magmatsko ognjišče – Slovenian" lang="sl" hreflang="sl" data-title="Magmatsko ognjišče" data-language-autonym="Slovenščina" data-language-local-name="Slovenian" class="interlanguage-link-target"><span>Slovenščina</span></a></li><li class="interlanguage-link interwiki-fi mw-list-item"><a href="https://fi.wikipedia.org/wiki/Magmas%C3%A4ili%C3%B6" title="Magmasäiliö – Finnish" lang="fi" hreflang="fi" data-title="Magmasäiliö" data-language-autonym="Suomi" data-language-local-name="Finnish" class="interlanguage-link-target"><span>Suomi</span></a></li><li class="interlanguage-link interwiki-tr mw-list-item"><a href="https://tr.wikipedia.org/wiki/Magma_odas%C4%B1" title="Magma odası – Turkish" lang="tr" hreflang="tr" data-title="Magma odası" data-language-autonym="Türkçe" data-language-local-name="Turkish" class="interlanguage-link-target"><span>Türkçe</span></a></li><li class="interlanguage-link interwiki-uk mw-list-item"><a href="https://uk.wikipedia.org/wiki/%D0%9C%D0%B0%D0%B3%D0%BC%D0%B0%D1%82%D0%B8%D1%87%D0%BD%D0%B0_%D0%BA%D0%BE%D0%BC%D0%BE%D1%80%D0%B0" title="Магматична комора – Ukrainian" lang="uk" hreflang="uk" data-title="Магматична комора" data-language-autonym="Українська" data-language-local-name="Ukrainian" class="interlanguage-link-target"><span>Українська</span></a></li><li class="interlanguage-link interwiki-vi mw-list-item"><a href="https://vi.wikipedia.org/wiki/L%C3%B2_magma" title="Lò magma – Vietnamese" lang="vi" hreflang="vi" data-title="Lò magma" data-language-autonym="Tiếng Việt" data-language-local-name="Vietnamese" class="interlanguage-link-target"><span>Tiếng Việt</span></a></li><li class="interlanguage-link interwiki-zh mw-list-item"><a href="https://zh.wikipedia.org/wiki/%E5%B2%A9%E6%B5%86%E6%88%BF" title="岩浆房 – Chinese" lang="zh" hreflang="zh" data-title="岩浆房" data-language-autonym="中文" data-language-local-name="Chinese" class="interlanguage-link-target"><span>中文</span></a></li></ul> </section> </div> <div class="minerva-footer-logo"><img src="/static/images/mobile/copyright/wikipedia-wordmark-en.svg" alt="Wikipedia" width="120" height="18" style="width: 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