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Oceanic crust - Wikipedia

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class="vector-toc-list"> <li id="toc-Geochemistry" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Geochemistry"> <div class="vector-toc-text"> <span class="vector-toc-numb">1.1</span> <span>Geochemistry</span> </div> </a> <ul id="toc-Geochemistry-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Life_cycle" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Life_cycle"> <div class="vector-toc-text"> <span class="vector-toc-numb">1.2</span> <span>Life cycle</span> </div> </a> <ul id="toc-Life_cycle-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-Magnetic_anomalies" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Magnetic_anomalies"> <div class="vector-toc-text"> <span class="vector-toc-numb">2</span> <span>Magnetic anomalies</span> </div> </a> <ul id="toc-Magnetic_anomalies-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-See_also" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#See_also"> <div class="vector-toc-text"> <span class="vector-toc-numb">3</span> <span>See also</span> </div> </a> <ul id="toc-See_also-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Notes" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Notes"> <div class="vector-toc-text"> <span class="vector-toc-numb">4</span> <span>Notes</span> </div> </a> <ul id="toc-Notes-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-References" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#References"> <div class="vector-toc-text"> <span class="vector-toc-numb">5</span> <span>References</span> </div> </a> <ul id="toc-References-sublist" class="vector-toc-list"> </ul> </li> </ul> </div> </div> </nav> </div> </div> <div class="mw-content-container"> <main id="content" class="mw-body"> <header class="mw-body-header vector-page-titlebar"> <nav aria-label="Contents" class="vector-toc-landmark"> <div id="vector-page-titlebar-toc" class="vector-dropdown vector-page-titlebar-toc vector-button-flush-left" > <input type="checkbox" id="vector-page-titlebar-toc-checkbox" role="button" aria-haspopup="true" data-event-name="ui.dropdown-vector-page-titlebar-toc" class="vector-dropdown-checkbox " aria-label="Toggle the table of contents" > <label id="vector-page-titlebar-toc-label" for="vector-page-titlebar-toc-checkbox" class="vector-dropdown-label cdx-button cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--weight-quiet cdx-button--icon-only " aria-hidden="true" ><span class="vector-icon mw-ui-icon-listBullet mw-ui-icon-wikimedia-listBullet"></span> <span class="vector-dropdown-label-text">Toggle the table of contents</span> </label> <div class="vector-dropdown-content"> <div id="vector-page-titlebar-toc-unpinned-container" class="vector-unpinned-container"> </div> </div> </div> </nav> <h1 id="firstHeading" class="firstHeading mw-first-heading"><span class="mw-page-title-main">Oceanic crust</span></h1> <div id="p-lang-btn" class="vector-dropdown mw-portlet mw-portlet-lang" > <input type="checkbox" id="p-lang-btn-checkbox" role="button" aria-haspopup="true" data-event-name="ui.dropdown-p-lang-btn" class="vector-dropdown-checkbox mw-interlanguage-selector" aria-label="Go to an article in another language. Available in 45 languages" > <label id="p-lang-btn-label" for="p-lang-btn-checkbox" class="vector-dropdown-label cdx-button cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--weight-quiet cdx-button--action-progressive mw-portlet-lang-heading-45" aria-hidden="true" ><span class="vector-icon mw-ui-icon-language-progressive mw-ui-icon-wikimedia-language-progressive"></span> <span class="vector-dropdown-label-text">45 languages</span> </label> <div class="vector-dropdown-content"> <div class="vector-menu-content"> <ul class="vector-menu-content-list"> <li class="interlanguage-link interwiki-ar mw-list-item"><a href="https://ar.wikipedia.org/wiki/%D9%82%D8%B4%D8%B1%D8%A9_%D9%85%D8%AD%D9%8A%D8%B7%D9%8A%D8%A9" title="قشرة محيطية – Arabic" lang="ar" hreflang="ar" data-title="قشرة محيطية" data-language-autonym="العربية" data-language-local-name="Arabic" class="interlanguage-link-target"><span>العربية</span></a></li><li class="interlanguage-link interwiki-az mw-list-item"><a href="https://az.wikipedia.org/wiki/Okean_yer_qab%C4%B1%C4%9F%C4%B1" title="Okean yer qabığı – Azerbaijani" lang="az" hreflang="az" data-title="Okean yer qabığı" data-language-autonym="Azərbaycanca" data-language-local-name="Azerbaijani" class="interlanguage-link-target"><span>Azərbaycanca</span></a></li><li class="interlanguage-link interwiki-bh mw-list-item"><a href="https://bh.wikipedia.org/wiki/%E0%A4%B8%E0%A4%AE%E0%A5%81%E0%A4%82%E0%A4%A6%E0%A5%8D%E0%A4%B0%E0%A5%80_%E0%A4%95%E0%A5%8D%E0%A4%B0%E0%A4%B8%E0%A5%8D%E0%A4%9F" title="समुंद्री क्रस्ट – Bhojpuri" lang="bh" hreflang="bh" data-title="समुंद्री क्रस्ट" data-language-autonym="भोजपुरी" data-language-local-name="Bhojpuri" class="interlanguage-link-target"><span>भोजपुरी</span></a></li><li class="interlanguage-link interwiki-bg mw-list-item"><a href="https://bg.wikipedia.org/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0" title="Океанска кора – Bulgarian" lang="bg" hreflang="bg" data-title="Океанска кора" data-language-autonym="Български" data-language-local-name="Bulgarian" class="interlanguage-link-target"><span>Български</span></a></li><li class="interlanguage-link interwiki-ca mw-list-item"><a href="https://ca.wikipedia.org/wiki/Escor%C3%A7a_oce%C3%A0nica" title="Escorça oceànica – Catalan" lang="ca" hreflang="ca" data-title="Escorça oceànica" 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/Oce%C3%A1nsk%C3%A1_k%C5%AFra" title="Oceánská kůra – Czech" lang="cs" hreflang="cs" data-title="Oceánská kůra" 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/Oceanbundsplade" title="Oceanbundsplade – Danish" lang="da" hreflang="da" data-title="Oceanbundsplade" 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/Ozeanische_Erdkruste" title="Ozeanische Erdkruste – German" lang="de" hreflang="de" data-title="Ozeanische Erdkruste" 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/Ookeaniline_maakoor" title="Ookeaniline maakoor – Estonian" lang="et" hreflang="et" data-title="Ookeaniline maakoor" 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/Corteza_oce%C3%A1nica" title="Corteza oceánica – Spanish" lang="es" hreflang="es" data-title="Corteza oceánica" 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/Oceankrusto" title="Oceankrusto – Esperanto" lang="eo" hreflang="eo" data-title="Oceankrusto" 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/Lurrazal_ozeaniko" title="Lurrazal ozeaniko – Basque" lang="eu" hreflang="eu" data-title="Lurrazal ozeaniko" 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/%D9%BE%D9%88%D8%B3%D8%AA%D9%87_%D8%A7%D9%82%DB%8C%D8%A7%D9%86%D9%88%D8%B3%DB%8C" title="پوسته اقیانوسی – Persian" lang="fa" hreflang="fa" data-title="پوسته اقیانوسی" 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/Lithosph%C3%A8re_oc%C3%A9anique" title="Lithosphère océanique – French" lang="fr" hreflang="fr" data-title="Lithosphère océanique" data-language-autonym="Français" data-language-local-name="French" class="interlanguage-link-target"><span>Français</span></a></li><li class="interlanguage-link interwiki-ga mw-list-item"><a href="https://ga.wikipedia.org/wiki/Screamh_aig%C3%A9anach" title="Screamh aigéanach – Irish" lang="ga" hreflang="ga" data-title="Screamh aigéanach" data-language-autonym="Gaeilge" data-language-local-name="Irish" class="interlanguage-link-target"><span>Gaeilge</span></a></li><li class="interlanguage-link interwiki-gl mw-list-item"><a href="https://gl.wikipedia.org/wiki/Codia_oce%C3%A1nica" title="Codia oceánica – Galician" lang="gl" hreflang="gl" data-title="Codia oceánica" 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/%ED%95%B4%EC%96%91_%EC%A7%80%EA%B0%81" title="해양 지각 – Korean" lang="ko" hreflang="ko" data-title="해양 지각" data-language-autonym="한국어" data-language-local-name="Korean" class="interlanguage-link-target"><span>한국어</span></a></li><li class="interlanguage-link interwiki-hi mw-list-item"><a href="https://hi.wikipedia.org/wiki/%E0%A4%AE%E0%A4%B9%E0%A4%BE%E0%A4%B8%E0%A4%BE%E0%A4%97%E0%A4%B0%E0%A5%80%E0%A4%AF_%E0%A4%AD%E0%A5%82%E0%A4%AA%E0%A4%B0%E0%A5%8D%E0%A4%AA%E0%A4%9F%E0%A5%80" title="महासागरीय भूपर्पटी – Hindi" lang="hi" hreflang="hi" data-title="महासागरीय भूपर्पटी" data-language-autonym="हिन्दी" data-language-local-name="Hindi" class="interlanguage-link-target"><span>हिन्दी</span></a></li><li class="interlanguage-link interwiki-hr mw-list-item"><a href="https://hr.wikipedia.org/wiki/Oceanska_kora" title="Oceanska kora – Croatian" lang="hr" hreflang="hr" data-title="Oceanska kora" data-language-autonym="Hrvatski" data-language-local-name="Croatian" class="interlanguage-link-target"><span>Hrvatski</span></a></li><li class="interlanguage-link interwiki-id mw-list-item"><a href="https://id.wikipedia.org/wiki/Kerak_samudra" title="Kerak samudra – Indonesian" lang="id" hreflang="id" data-title="Kerak samudra" 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/Hafsbotnsskorpa" title="Hafsbotnsskorpa – Icelandic" lang="is" hreflang="is" data-title="Hafsbotnsskorpa" 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/Crosta_oceanica" title="Crosta oceanica – Italian" lang="it" hreflang="it" data-title="Crosta oceanica" data-language-autonym="Italiano" data-language-local-name="Italian" class="interlanguage-link-target"><span>Italiano</span></a></li><li class="interlanguage-link interwiki-ky mw-list-item"><a href="https://ky.wikipedia.org/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD_%D1%82%D0%B0%D0%BC%D0%B0%D0%BD%D1%8B" title="Океан таманы – Kyrgyz" lang="ky" hreflang="ky" data-title="Океан таманы" data-language-autonym="Кыргызча" data-language-local-name="Kyrgyz" class="interlanguage-link-target"><span>Кыргызча</span></a></li><li class="interlanguage-link interwiki-lv mw-list-item"><a href="https://lv.wikipedia.org/wiki/Oke%C4%81nisk%C4%81_Zemes_garoza" title="Okeāniskā Zemes garoza – Latvian" lang="lv" hreflang="lv" data-title="Okeāniskā Zemes garoza" data-language-autonym="Latviešu" data-language-local-name="Latvian" class="interlanguage-link-target"><span>Latviešu</span></a></li><li class="interlanguage-link interwiki-mk mw-list-item"><a href="https://mk.wikipedia.org/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0" title="Океанска кора – Macedonian" lang="mk" hreflang="mk" data-title="Океанска кора" 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/Kerak_lautan" title="Kerak lautan – Malay" lang="ms" hreflang="ms" data-title="Kerak lautan" 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/Oceanische_lithosfeer" title="Oceanische lithosfeer – Dutch" lang="nl" hreflang="nl" data-title="Oceanische lithosfeer" data-language-autonym="Nederlands" data-language-local-name="Dutch" class="interlanguage-link-target"><span>Nederlands</span></a></li><li class="interlanguage-link interwiki-ja badge-Q70894304 mw-list-item" title=""><a href="https://ja.wikipedia.org/wiki/%E6%B5%B7%E6%B4%8B%E6%80%A7%E5%9C%B0%E6%AE%BB" title="海洋性地殻 – Japanese" lang="ja" hreflang="ja" data-title="海洋性地殻" 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/Havbunnsskorpe" title="Havbunnsskorpe – Norwegian Bokmål" lang="nb" hreflang="nb" data-title="Havbunnsskorpe" 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/Havbotnskorpe" title="Havbotnskorpe – Norwegian Nynorsk" lang="nn" hreflang="nn" data-title="Havbotnskorpe" 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-pl mw-list-item"><a href="https://pl.wikipedia.org/wiki/Skorupa_ziemska_oceaniczna" title="Skorupa ziemska oceaniczna – Polish" lang="pl" hreflang="pl" data-title="Skorupa ziemska oceaniczna" 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/Crusta_oce%C3%A2nica" title="Crusta oceânica – Portuguese" lang="pt" hreflang="pt" data-title="Crusta oceânica" 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%9E%D0%BA%D0%B5%D0%B0%D0%BD%D0%B8%D1%87%D0%B5%D1%81%D0%BA%D0%B0%D1%8F_%D0%BA%D0%BE%D1%80%D0%B0" title="Океаническая кора – Russian" lang="ru" hreflang="ru" data-title="Океаническая кора" 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/Oceanic_crust" title="Oceanic crust – Simple English" lang="en-simple" hreflang="en-simple" data-title="Oceanic crust" 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/Oce%C3%A1nska_zemsk%C3%A1_k%C3%B4ra" title="Oceánska zemská kôra – Slovak" lang="sk" hreflang="sk" data-title="Oceánska zemská kôra" 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/Oceanska_skorja" title="Oceanska skorja – Slovenian" lang="sl" hreflang="sl" data-title="Oceanska skorja" data-language-autonym="Slovenščina" data-language-local-name="Slovenian" class="interlanguage-link-target"><span>Slovenščina</span></a></li><li class="interlanguage-link interwiki-sr mw-list-item"><a href="https://sr.wikipedia.org/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0" title="Океанска кора – Serbian" lang="sr" hreflang="sr" data-title="Океанска кора" data-language-autonym="Српски / srpski" data-language-local-name="Serbian" class="interlanguage-link-target"><span>Српски / srpski</span></a></li><li class="interlanguage-link interwiki-sh mw-list-item"><a href="https://sh.wikipedia.org/wiki/Okeanska_kora" title="Okeanska kora – Serbo-Croatian" lang="sh" hreflang="sh" data-title="Okeanska kora" data-language-autonym="Srpskohrvatski / српскохрватски" data-language-local-name="Serbo-Croatian" class="interlanguage-link-target"><span>Srpskohrvatski / српскохрватски</span></a></li><li class="interlanguage-link interwiki-th mw-list-item"><a href="https://th.wikipedia.org/wiki/%E0%B9%80%E0%B8%9B%E0%B8%A5%E0%B8%B7%E0%B8%AD%E0%B8%81%E0%B9%82%E0%B8%A5%E0%B8%81%E0%B8%A0%E0%B8%B2%E0%B8%84%E0%B8%9E%E0%B8%B7%E0%B9%89%E0%B8%99%E0%B8%AA%E0%B8%A1%E0%B8%B8%E0%B8%97%E0%B8%A3" title="เปลือกโลกภาคพื้นสมุทร – Thai" lang="th" hreflang="th" data-title="เปลือกโลกภาคพื้นสมุทร" data-language-autonym="ไทย" data-language-local-name="Thai" class="interlanguage-link-target"><span>ไทย</span></a></li><li class="interlanguage-link interwiki-tr mw-list-item"><a href="https://tr.wikipedia.org/wiki/Okyanusal_kabuk" title="Okyanusal kabuk – Turkish" lang="tr" hreflang="tr" data-title="Okyanusal kabuk" 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%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%96%D1%87%D0%BD%D0%B0_%D0%B7%D0%B5%D0%BC%D0%BD%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0" title="Океанічна земна кора – Ukrainian" lang="uk" hreflang="uk" data-title="Океанічна земна кора" data-language-autonym="Українська" data-language-local-name="Ukrainian" class="interlanguage-link-target"><span>Українська</span></a></li><li class="interlanguage-link interwiki-vec mw-list-item"><a href="https://vec.wikipedia.org/wiki/Crosta_ose%C3%A0nega" title="Crosta oseànega – Venetian" lang="vec" hreflang="vec" data-title="Crosta oseànega" data-language-autonym="Vèneto" data-language-local-name="Venetian" class="interlanguage-link-target"><span>Vèneto</span></a></li><li class="interlanguage-link interwiki-vi mw-list-item"><a href="https://vi.wikipedia.org/wiki/V%E1%BB%8F_%C4%91%E1%BA%A1i_d%C6%B0%C6%A1ng" title="Vỏ đại dương – Vietnamese" lang="vi" hreflang="vi" data-title="Vỏ đại dương" 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/%E6%B5%B7%E6%B4%8B%E5%9C%B0%E6%AE%BC" title="海洋地殼 – Chinese" lang="zh" hreflang="zh" data-title="海洋地殼" data-language-autonym="中文" data-language-local-name="Chinese" class="interlanguage-link-target"><span>中文</span></a></li><li class="interlanguage-link interwiki-kge mw-list-item"><a href="https://kge.wikipedia.org/wiki/Korak_Samudra" title="Korak Samudra – 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data-mw-ve-target-container> <div class="vector-body-before-content"> <div class="mw-indicators"> </div> <div id="siteSub" class="noprint">From Wikipedia, the free encyclopedia</div> </div> <div id="contentSub"><div id="mw-content-subtitle"></div></div> <div id="mw-content-text" class="mw-body-content"><div class="mw-content-ltr mw-parser-output" lang="en" dir="ltr"><div class="shortdescription nomobile noexcerpt noprint searchaux" style="display:none">Uppermost layer of the oceanic portion of a tectonic plate</div> <figure typeof="mw:File/Thumb"><a href="/wiki/File:Global_Map_of_Oceanic_Plate_Age_by_Fabio_Crameri.png" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/c/cb/Global_Map_of_Oceanic_Plate_Age_by_Fabio_Crameri.png/350px-Global_Map_of_Oceanic_Plate_Age_by_Fabio_Crameri.png" decoding="async" width="350" height="233" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/c/cb/Global_Map_of_Oceanic_Plate_Age_by_Fabio_Crameri.png/525px-Global_Map_of_Oceanic_Plate_Age_by_Fabio_Crameri.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/c/cb/Global_Map_of_Oceanic_Plate_Age_by_Fabio_Crameri.png/700px-Global_Map_of_Oceanic_Plate_Age_by_Fabio_Crameri.png 2x" data-file-width="2953" data-file-height="1967" /></a><figcaption>The colours indicate the age of oceanic crust, wherein lighter indicates younger age, and darker indicates older age. The lines represent tectonic plate boundaries.</figcaption></figure> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Continental_and_oceanic_crust.png" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/e/e7/Continental_and_oceanic_crust.png/220px-Continental_and_oceanic_crust.png" decoding="async" width="220" height="133" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/e/e7/Continental_and_oceanic_crust.png/330px-Continental_and_oceanic_crust.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/e/e7/Continental_and_oceanic_crust.png/440px-Continental_and_oceanic_crust.png 2x" data-file-width="952" data-file-height="577" /></a><figcaption>Continental and oceanic crust on the Earth's upper mantle</figcaption></figure> <p><b>Oceanic crust</b> is the uppermost layer of the oceanic portion of the <a href="/wiki/Plate_tectonics" title="Plate tectonics">tectonic plates</a>. It is composed of the upper oceanic crust, with <a href="/wiki/Pillow_lava" title="Pillow lava">pillow lavas</a> and a <a href="/wiki/Dike_(geology)" title="Dike (geology)">dike</a> complex, and the <a href="/wiki/Lower_oceanic_crust" title="Lower oceanic crust">lower oceanic crust</a>, composed of <a href="/wiki/Troctolite" title="Troctolite">troctolite</a>, <a href="/wiki/Gabbro" title="Gabbro">gabbro</a> and <a href="/wiki/Ultramafic_rock" title="Ultramafic rock">ultramafic</a> <a href="/wiki/Cumulate_rock" title="Cumulate rock">cumulates</a>.<sup id="cite_ref-1" class="reference"><a href="#cite_note-1"><span class="cite-bracket">&#91;</span>1<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-Pirajno_2013_2-0" class="reference"><a href="#cite_note-Pirajno_2013-2"><span class="cite-bracket">&#91;</span>2<span class="cite-bracket">&#93;</span></a></sup> The crust overlies the rigid uppermost layer of the <a href="/wiki/Mantle_(geology)" title="Mantle (geology)">mantle</a>. The crust and the rigid upper mantle layer together constitute oceanic <a href="/wiki/Lithosphere" title="Lithosphere">lithosphere</a>. </p><p>Oceanic crust is primarily composed of <a href="/wiki/Mafic" title="Mafic">mafic</a> rocks, or <a href="/wiki/Sima_(geology)" title="Sima (geology)">sima</a>, which is rich in iron and magnesium. It is thinner than <a href="/wiki/Continental_crust" title="Continental crust">continental crust</a>, or <a href="/wiki/Sial" title="Sial">sial</a>, generally less than 10 kilometers thick; however, it is denser, having a mean density of about 3.0 <a href="/wiki/Gram" title="Gram">grams</a> per cubic centimeter as opposed to continental crust which has a density of about 2.7 grams per cubic centimeter.<sup id="cite_ref-Rogers_3-0" class="reference"><a href="#cite_note-Rogers-3"><span class="cite-bracket">&#91;</span>3<span class="cite-bracket">&#93;</span></a></sup> </p><p>The crust uppermost is the result of the cooling of magma derived from <a href="/wiki/Earth%27s_mantle" title="Earth&#39;s mantle">mantle</a> material below the plate. The magma is injected into the spreading center, which consists mainly of a partly solidified <a href="/wiki/Crystal_mush" title="Crystal mush">crystal mush</a> derived from earlier injections, forming magma lenses that are the source of the <a href="/wiki/Sheeted_dyke_complex" title="Sheeted dyke complex">sheeted dikes</a> that feed the overlying pillow lavas.<sup id="cite_ref-Sinton_&amp;_Detrick_4-0" class="reference"><a href="#cite_note-Sinton_&amp;_Detrick-4"><span class="cite-bracket">&#91;</span>4<span class="cite-bracket">&#93;</span></a></sup> As the lavas cool they are, in most instances, modified chemically by seawater.<sup id="cite_ref-5" class="reference"><a href="#cite_note-5"><span class="cite-bracket">&#91;</span>5<span class="cite-bracket">&#93;</span></a></sup> These eruptions occur mostly at mid-ocean ridges, but also at scattered hotspots, and also in rare but powerful occurrences known as <a href="/wiki/Flood_basalt" title="Flood basalt">flood basalt</a> eruptions. But most <a href="/wiki/Magma" title="Magma">magma</a> <a href="/wiki/Crystallization" title="Crystallization">crystallises</a> at depth, within the <a href="/wiki/Lower_oceanic_crust" title="Lower oceanic crust">lower oceanic crust</a>. There, newly intruded magma can mix and react with pre-existing crystal mush and rocks.<sup id="cite_ref-6" class="reference"><a href="#cite_note-6"><span class="cite-bracket">&#91;</span>6<span class="cite-bracket">&#93;</span></a></sup> </p> <meta property="mw:PageProp/toc" /> <div class="mw-heading mw-heading2"><h2 id="Composition">Composition</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Oceanic_crust&amp;action=edit&amp;section=1" title="Edit section: Composition"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <style data-mw-deduplicate="TemplateStyles:r1236090951">.mw-parser-output .hatnote{font-style:italic}.mw-parser-output div.hatnote{padding-left:1.6em;margin-bottom:0.5em}.mw-parser-output .hatnote i{font-style:normal}.mw-parser-output .hatnote+link+.hatnote{margin-top:-0.5em}@media print{body.ns-0 .mw-parser-output .hatnote{display:none!important}}</style><div role="note" class="hatnote navigation-not-searchable">See also: <a href="/wiki/Lithosphere#Oceanic_lithosphere" title="Lithosphere">Lithosphere §&#160;Oceanic lithosphere</a></div> <p>Although a complete section of oceanic crust has not yet been drilled, geologists have several pieces of evidence that help them understand the ocean floor. Estimations of composition are based on analyses of <a href="/wiki/Ophiolite" title="Ophiolite">ophiolites</a> (sections of oceanic crust that are thrust onto and preserved on the continents), comparisons of the <a href="/wiki/Seismology" title="Seismology">seismic structure</a> of the oceanic crust with laboratory determinations of seismic velocities in known rock types, and samples recovered from the ocean floor by <a href="/wiki/Submersible" title="Submersible">submersibles</a>, dredging (especially from <a href="/wiki/Mid-ocean_ridge" title="Mid-ocean ridge">ridge</a> crests and <a href="/wiki/Fracture_zone" title="Fracture zone">fracture zones</a>) and drilling.<sup id="cite_ref-7" class="reference"><a href="#cite_note-7"><span class="cite-bracket">&#91;</span>7<span class="cite-bracket">&#93;</span></a></sup> Oceanic crust is significantly simpler than continental crust and generally can be divided in three layers.<sup id="cite_ref-8" class="reference"><a href="#cite_note-8"><span class="cite-bracket">&#91;</span>8<span class="cite-bracket">&#93;</span></a></sup> According to <a href="/wiki/Mineral_physics" title="Mineral physics">mineral physics</a> experiments, at lower mantle pressures, oceanic crust becomes denser than the surrounding mantle.<sup id="cite_ref-9" class="reference"><a href="#cite_note-9"><span class="cite-bracket">&#91;</span>9<span class="cite-bracket">&#93;</span></a></sup> </p> <ul><li><b>Layer 1</b> is on an average 0.4&#160;km thick. It consists of unconsolidated or semiconsolidated <a href="/wiki/Sediment" title="Sediment">sediments</a>, usually thin or even not present near the <a href="/wiki/Mid-ocean_ridge" title="Mid-ocean ridge">mid-ocean ridges</a> but thickens farther away from the ridge.<sup id="cite_ref-10" class="reference"><a href="#cite_note-10"><span class="cite-bracket">&#91;</span>10<span class="cite-bracket">&#93;</span></a></sup> Near the continental margins sediment is <a href="/wiki/Terrigenous_sediment" title="Terrigenous sediment">terrigenous</a>, meaning derived from the land, unlike deep sea sediments which are made of tiny <a href="/wiki/Exoskeleton" title="Exoskeleton">shells</a> of marine organisms, usually calcareous and siliceous, or it can be made of volcanic ash and terrigenous <a href="/wiki/Sediment_transport" title="Sediment transport">sediments transported</a> by <a href="/wiki/Turbidity_current" title="Turbidity current">turbidity currents</a>.<sup id="cite_ref-11" class="reference"><a href="#cite_note-11"><span class="cite-bracket">&#91;</span>11<span class="cite-bracket">&#93;</span></a></sup></li> <li><b>Layer 2</b> could be divided into two parts: layer 2A – 0.5&#160;km thick uppermost volcanic layer of glassy to finely crystalline <a href="/wiki/Basalt" title="Basalt">basalt</a> usually in the form of <a href="/wiki/Pillow_lava" title="Pillow lava">pillow basalt</a>, and layer 2B – 1.5&#160;km thick layer composed of <a href="/wiki/Diabase" title="Diabase">diabase</a> <a href="/wiki/Dike_(geology)" title="Dike (geology)">dikes</a>.<sup id="cite_ref-12" class="reference"><a href="#cite_note-12"><span class="cite-bracket">&#91;</span>12<span class="cite-bracket">&#93;</span></a></sup></li> <li><b>Layer 3</b> is formed by slow cooling of <a href="/wiki/Magma" title="Magma">magma</a> beneath the surface and consists of coarse grained <a href="/wiki/Gabbro" title="Gabbro">gabbro</a> and <a href="/wiki/Cumulate_rock" title="Cumulate rock">cumulate</a> <a href="/wiki/Ultramafic_rock" title="Ultramafic rock">ultramafic rocks</a>.<sup id="cite_ref-13" class="reference"><a href="#cite_note-13"><span class="cite-bracket">&#91;</span>13<span class="cite-bracket">&#93;</span></a></sup> It constitutes over two-thirds of oceanic crust volume with almost 5&#160;km thickness.<sup id="cite_ref-14" class="reference"><a href="#cite_note-14"><span class="cite-bracket">&#91;</span>14<span class="cite-bracket">&#93;</span></a></sup></li></ul> <div class="mw-heading mw-heading3"><h3 id="Geochemistry">Geochemistry<span class="anchor" id="marine_geochemistry"></span></h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Oceanic_crust&amp;action=edit&amp;section=2" title="Edit section: Geochemistry"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>The most voluminous <a href="/wiki/Volcanic_rock" title="Volcanic rock">volcanic rocks</a> of the ocean floor are the mid-oceanic ridge basalts, which are derived from low-<a href="/wiki/Potassium" title="Potassium">potassium</a> <a href="/wiki/Tholeiitic_magma_series" title="Tholeiitic magma series">tholeiitic magmas</a>. These rocks have low concentrations of large ion <a href="/wiki/Lithophile" title="Lithophile">lithophile</a> elements (LILE), light rare earth elements (LREE), volatile elements and other highly <a href="/wiki/Incompatible_element" title="Incompatible element">incompatible elements</a>. There can be found basalts enriched with incompatible elements, but they are rare and associated with mid-ocean ridge <a href="/wiki/Hotspot_(geology)" title="Hotspot (geology)">hot spots</a> such as surroundings of <a href="/wiki/Galapagos_Islands" class="mw-redirect" title="Galapagos Islands">Galapagos Islands</a>, the <a href="/wiki/Azores" title="Azores">Azores</a> and <a href="/wiki/Iceland" title="Iceland">Iceland</a>.<sup id="cite_ref-15" class="reference"><a href="#cite_note-15"><span class="cite-bracket">&#91;</span>15<span class="cite-bracket">&#93;</span></a></sup> </p><p>Prior to the <a href="/wiki/Neoproterozoic" title="Neoproterozoic">Neoproterozoic Era</a> 1000 <a href="/wiki/Million_years_ago" title="Million years ago">Ma</a> ago the world's oceanic crust was more <a href="/wiki/Mafic" title="Mafic">mafic</a> than present-days'. The more mafic nature of the crust meant that higher amounts of water molecules (<a href="/wiki/Hydroxy_group" title="Hydroxy group">OH</a>) could be stored the <a href="/w/index.php?title=Alteration_(geology)&amp;action=edit&amp;redlink=1" class="new" title="Alteration (geology) (page does not exist)">altered</a> parts of the crust. At <a href="/wiki/Subduction" title="Subduction">subduction</a> zones this mafic crust was prone to metamorphose into <a href="/wiki/Greenschist" title="Greenschist">greenschist</a> instead of <a href="/wiki/Blueschist" title="Blueschist">blueschist</a> at ordinary <a href="/wiki/Metamorphic_facies" title="Metamorphic facies">blueschist facies</a>.<sup id="cite_ref-PaWh2016_16-0" class="reference"><a href="#cite_note-PaWh2016-16"><span class="cite-bracket">&#91;</span>16<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Life_cycle">Life cycle</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Oceanic_crust&amp;action=edit&amp;section=3" title="Edit section: Life cycle"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Oceanic crust is continuously being created at mid-ocean ridges. As <a href="/wiki/Plate_tectonics" title="Plate tectonics">continental plates</a> diverge at these ridges, magma rises into the upper mantle and crust. As the continental plates move away from the ridge, the newly formed rocks cool and start to erode with sediment gradually building up on top of them. The youngest oceanic rocks are at the oceanic ridges, and they get progressively older away from the ridges.<sup id="cite_ref-17" class="reference"><a href="#cite_note-17"><span class="cite-bracket">&#91;</span>17<span class="cite-bracket">&#93;</span></a></sup> </p><p>As the mantle rises it cools and melts, as the pressure decreases and it crosses the <a href="/wiki/Solidus_(chemistry)" class="mw-redirect" title="Solidus (chemistry)">solidus</a>. The amount of melt produced depends only on the temperature of the mantle as it rises. Hence most oceanic crust is the same thickness (7±1&#160;km). Very slow spreading ridges (&lt;1&#160;cm·yr<sup>−1</sup> half-rate) produce thinner crust (4–5&#160;km thick) as the mantle has a chance to cool on upwelling and so it crosses the solidus and melts at lesser depth, thereby producing less melt and thinner crust. An example of this is the <a href="/wiki/Gakkel_Ridge" title="Gakkel Ridge">Gakkel Ridge</a> under the <a href="/wiki/Arctic_Ocean" title="Arctic Ocean">Arctic Ocean</a>. Thicker than average crust is found above <a href="/wiki/Mantle_plume" title="Mantle plume">plumes</a> as the mantle is hotter and hence it crosses the solidus and melts at a greater depth, creating more melt and a thicker crust. An example of this is <a href="/wiki/Iceland" title="Iceland">Iceland</a> which has crust of thickness ~20&#160;km.<sup id="cite_ref-18" class="reference"><a href="#cite_note-18"><span class="cite-bracket">&#91;</span>18<span class="cite-bracket">&#93;</span></a></sup> </p><p>The age of the oceanic crust can be used to estimate the (thermal) thickness of the lithosphere, where young oceanic crust has not had enough time to cool the mantle beneath it, while older oceanic crust has thicker mantle lithosphere beneath it.<sup id="cite_ref-19" class="reference"><a href="#cite_note-19"><span class="cite-bracket">&#91;</span>19<span class="cite-bracket">&#93;</span></a></sup> The oceanic lithosphere <a href="/wiki/Subduction" title="Subduction">subducts</a> at what are known as <a href="/wiki/Convergent_boundary" title="Convergent boundary">convergent boundaries</a>. These boundaries can exist between oceanic lithosphere on one plate and oceanic lithosphere on another, or between oceanic lithosphere on one plate and continental lithosphere on another. In the second situation, the oceanic lithosphere always subducts because the continental lithosphere is less dense. The subduction process consumes older oceanic lithosphere, so oceanic crust is seldom more than 200 million years old.<sup id="cite_ref-20" class="reference"><a href="#cite_note-20"><span class="cite-bracket">&#91;</span>20<span class="cite-bracket">&#93;</span></a></sup> The process of super-continent formation and destruction via repeated cycles of creation and destruction of oceanic crust is known as the <a href="/wiki/Wilson_Cycle" title="Wilson Cycle">Wilson Cycle</a>. </p><p>The oldest large-scale oceanic crust is in the west <a href="/wiki/Pacific_Ocean" title="Pacific Ocean">Pacific</a> and north-west <a href="/wiki/Atlantic_Ocean" title="Atlantic Ocean">Atlantic</a>&#160;—&#160;both are about up to 180-200 million years old. However, parts of the eastern <a href="/wiki/Mediterranean_Sea" title="Mediterranean Sea">Mediterranean Sea</a> could be remnants of the much older <a href="/wiki/Tethys_Ocean" title="Tethys Ocean">Tethys Ocean</a>, at about 270 and up to 340 million years old.<sup id="cite_ref-21" class="reference"><a href="#cite_note-21"><span class="cite-bracket">&#91;</span>21<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-22" class="reference"><a href="#cite_note-22"><span class="cite-bracket">&#91;</span>22<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-23" class="reference"><a href="#cite_note-23"><span class="cite-bracket">&#91;</span>23<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Magnetic_anomalies">Magnetic anomalies</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Oceanic_crust&amp;action=edit&amp;section=4" title="Edit section: Magnetic anomalies"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main article: <a href="/wiki/Seafloor_spreading" title="Seafloor spreading">Seafloor spreading</a></div> <p>The oceanic crust displays a pattern of magnetic lines, parallel to the ocean ridges, frozen in the <a href="/wiki/Basalt" title="Basalt">basalt</a>. A symmetrical pattern of positive and negative magnetic lines emanates from the mid-ocean ridge.<sup id="cite_ref-24" class="reference"><a href="#cite_note-24"><span class="cite-bracket">&#91;</span>24<span class="cite-bracket">&#93;</span></a></sup> New rock is formed by magma at the mid-ocean ridges, and the ocean floor spreads out from this point. When the magma cools to form rock, <a href="/wiki/Geomagnetic_reversal" title="Geomagnetic reversal">its magnetic polarity</a> is aligned with the then-current positions of the magnetic poles of the Earth. New magma then forces the older cooled magma away from the ridge. This process results in parallel sections of oceanic crust of alternating magnetic polarity. </p> <div class="mw-heading mw-heading2"><h2 id="See_also">See also</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Oceanic_crust&amp;action=edit&amp;section=5" title="Edit section: See also"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <style data-mw-deduplicate="TemplateStyles:r1239009302">.mw-parser-output .portalbox{padding:0;margin:0.5em 0;display:table;box-sizing:border-box;max-width:175px;list-style:none}.mw-parser-output .portalborder{border:1px solid var(--border-color-base,#a2a9b1);padding:0.1em;background:var(--background-color-neutral-subtle,#f8f9fa)}.mw-parser-output .portalbox-entry{display:table-row;font-size:85%;line-height:110%;height:1.9em;font-style:italic;font-weight:bold}.mw-parser-output .portalbox-image{display:table-cell;padding:0.2em;vertical-align:middle;text-align:center}.mw-parser-output .portalbox-link{display:table-cell;padding:0.2em 0.2em 0.2em 0.3em;vertical-align:middle}@media(min-width:720px){.mw-parser-output .portalleft{clear:left;float:left;margin:0.5em 1em 0.5em 0}.mw-parser-output .portalright{clear:right;float:right;margin:0.5em 0 0.5em 1em}}</style><ul role="navigation" aria-label="Portals" class="noprint portalbox portalborder portalright"> <li class="portalbox-entry"><span class="portalbox-image"><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Waves_in_pacifica_1.jpg" class="mw-file-description"><img alt="icon" src="//upload.wikimedia.org/wikipedia/commons/thumb/4/45/Waves_in_pacifica_1.jpg/32px-Waves_in_pacifica_1.jpg" decoding="async" width="32" height="22" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/4/45/Waves_in_pacifica_1.jpg/48px-Waves_in_pacifica_1.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/4/45/Waves_in_pacifica_1.jpg/64px-Waves_in_pacifica_1.jpg 2x" data-file-width="2000" data-file-height="1358" /></a></span></span><span class="portalbox-link"><a href="/wiki/Portal:Oceans" title="Portal:Oceans">Oceans portal</a></span></li></ul> <ul><li><a href="/wiki/Continental_crust" title="Continental crust">Continental crust</a></li> <li><a href="/wiki/Lithosphere" title="Lithosphere">Lithosphere</a></li> <li><a href="/wiki/Mohorovi%C4%8Di%C4%87_discontinuity" title="Mohorovičić discontinuity">Mohorovičić discontinuity</a></li> <li><a href="/wiki/Plate_tectonics" title="Plate tectonics">Plate tectonics</a></li> <li><a href="/wiki/General_Bathymetric_Chart_of_the_Oceans#Seabed_2030_Project" title="General Bathymetric Chart of the Oceans">Seabed 2030</a></li> <li><a href="/wiki/Seafloor_depth_versus_age" title="Seafloor depth versus age">Seafloor depth versus age</a></li></ul> <div class="mw-heading mw-heading2"><h2 id="Notes">Notes</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Oceanic_crust&amp;action=edit&amp;section=6" title="Edit section: Notes"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <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 .references{font-size:100%;margin-bottom:0;list-style-type:inherit}.mw-parser-output .reflist-columns-2{column-width:30em}.mw-parser-output .reflist-columns-3{column-width:25em}.mw-parser-output .reflist-columns{margin-top:0.3em}.mw-parser-output .reflist-columns ol{margin-top:0}.mw-parser-output .reflist-columns li{page-break-inside:avoid;break-inside:avoid-column}.mw-parser-output .reflist-upper-alpha{list-style-type:upper-alpha}.mw-parser-output .reflist-upper-roman{list-style-type:upper-roman}.mw-parser-output .reflist-lower-alpha{list-style-type:lower-alpha}.mw-parser-output .reflist-lower-greek{list-style-type:lower-greek}.mw-parser-output .reflist-lower-roman{list-style-type:lower-roman}</style><div class="reflist"> <div class="mw-references-wrap mw-references-columns"><ol class="references"> <li id="cite_note-1"><span class="mw-cite-backlink"><b><a href="#cite_ref-1">^</a></b></span> <span class="reference-text">Gillis et al. (2014). Primitive layered gabbros from fast-spreading lower oceanic crust. Nature 505, 204-208</span> </li> <li id="cite_note-Pirajno_2013-2"><span class="mw-cite-backlink"><b><a href="#cite_ref-Pirajno_2013_2-0">^</a></b></span> <span class="reference-text"><style 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="CITEREFPirajno_F.2013" class="citation book cs1">Pirajno F. (2013). <a rel="nofollow" class="external text" href="https://books.google.com/books?id=PrXyCAAAQBAJ&amp;q=ultramafic+cumulates+layer+3&amp;pg=PA11"><i>Ore Deposits and Mantle Plumes</i></a>. Springer. p.&#160;11. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a>&#160;<a href="/wiki/Special:BookSources/9789401725026" title="Special:BookSources/9789401725026"><bdi>9789401725026</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=book&amp;rft.btitle=Ore+Deposits+and+Mantle+Plumes&amp;rft.pages=11&amp;rft.pub=Springer&amp;rft.date=2013&amp;rft.isbn=9789401725026&amp;rft.au=Pirajno+F.&amp;rft_id=https%3A%2F%2Fbooks.google.com%2Fbooks%3Fid%3DPrXyCAAAQBAJ%26q%3Dultramafic%2Bcumulates%2Blayer%2B3%26pg%3DPA11&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3AOceanic+crust" class="Z3988"></span></span> </li> <li id="cite_note-Rogers-3"><span class="mw-cite-backlink"><b><a href="#cite_ref-Rogers_3-0">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFRogers2008" class="citation book cs1">Rogers, N., ed. 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(1992). <a rel="nofollow" class="external text" href="https://www.researchgate.net/publication/248793835">"Mid-ocean ridge magma chambers"</a>. <i>Journal of Geophysical Research</i>. <b>97</b> (B1): 197–216. <a href="/wiki/Bibcode_(identifier)" class="mw-redirect" title="Bibcode (identifier)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/1992JGR....97..197S">1992JGR....97..197S</a>. <a href="/wiki/Doi_(identifier)" class="mw-redirect" title="Doi (identifier)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1029%2F91JB02508">10.1029/91JB02508</a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=article&amp;rft.jtitle=Journal+of+Geophysical+Research&amp;rft.atitle=Mid-ocean+ridge+magma+chambers&amp;rft.volume=97&amp;rft.issue=B1&amp;rft.pages=197-216&amp;rft.date=1992&amp;rft_id=info%3Adoi%2F10.1029%2F91JB02508&amp;rft_id=info%3Abibcode%2F1992JGR....97..197S&amp;rft.au=Sinton+J.M.&amp;rft.au=Detrick+R.S.&amp;rft_id=https%3A%2F%2Fwww.researchgate.net%2Fpublication%2F248793835&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3AOceanic+crust" class="Z3988"></span></span> </li> <li id="cite_note-5"><span class="mw-cite-backlink"><b><a href="#cite_ref-5">^</a></b></span> <span class="reference-text">H. 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Ross. <a rel="nofollow" class="external text" href="http://www2.ocean.washington.edu/oc540/lec01-1/">"Ocean 540: Oceanic Lithosphere; Plate Tectonics; Seafloor Topography"</a>. School of Oceanography, University of Washington<span class="reference-accessdate">. Retrieved <span class="nowrap">9 August</span> 2009</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=unknown&amp;rft.btitle=Ocean+540%3A+Oceanic+Lithosphere%3B+Plate+Tectonics%3B+Seafloor+Topography&amp;rft.pub=School+of+Oceanography%2C+University+of+Washington&amp;rft.aulast=McDuff&amp;rft.aufirst=Russell+E.&amp;rft.au=Heath%2C+G.+Ross&amp;rft_id=http%3A%2F%2Fwww2.ocean.washington.edu%2Foc540%2Flec01-1%2F&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3AOceanic+crust" class="Z3988"></span></li></ul> <div class="navbox-styles"><style data-mw-deduplicate="TemplateStyles:r1129693374">.mw-parser-output .hlist dl,.mw-parser-output .hlist ol,.mw-parser-output .hlist ul{margin:0;padding:0}.mw-parser-output .hlist dd,.mw-parser-output .hlist dt,.mw-parser-output .hlist li{margin:0;display:inline}.mw-parser-output .hlist.inline,.mw-parser-output .hlist.inline dl,.mw-parser-output .hlist.inline ol,.mw-parser-output .hlist.inline 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title="Modulational instability">Benjamin–Feir instability</a></li> <li><a href="/wiki/Boussinesq_approximation_(water_waves)" title="Boussinesq approximation (water waves)">Boussinesq approximation</a></li> <li><a href="/wiki/Breaking_wave" title="Breaking wave">Breaking wave</a></li> <li><a href="/wiki/Clapotis" title="Clapotis">Clapotis</a></li> <li><a href="/wiki/Cnoidal_wave" title="Cnoidal wave">Cnoidal wave</a></li> <li><a href="/wiki/Cross_sea" title="Cross sea">Cross sea</a></li> <li><a href="/wiki/Dispersion_(water_waves)" title="Dispersion (water waves)">Dispersion</a></li> <li><a href="/wiki/Edge_wave" title="Edge wave">Edge wave</a></li> <li><a href="/wiki/Equatorial_wave" title="Equatorial wave">Equatorial waves</a></li> <li><a href="/wiki/Gravity_wave" title="Gravity wave">Gravity wave</a></li> <li><a href="/wiki/Green%27s_law" title="Green&#39;s law">Green's law</a></li> <li><a href="/wiki/Infragravity_wave" title="Infragravity wave">Infragravity wave</a></li> <li><a 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srcset="//upload.wikimedia.org/wikipedia/commons/thumb/e/ee/Upwelling.svg/180px-Upwelling.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/e/ee/Upwelling.svg/240px-Upwelling.svg.png 2x" data-file-width="365" data-file-height="242" /></a></span><br /><br /><br /><br /><br /><br /><span typeof="mw:File"><a href="/wiki/File:Antarctic_bottom_water.svg" class="mw-file-description" title="Antarctic bottom water"><img alt="Antarctic bottom water" src="//upload.wikimedia.org/wikipedia/commons/thumb/e/e7/Antarctic_bottom_water.svg/120px-Antarctic_bottom_water.svg.png" decoding="async" width="120" height="76" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/e/e7/Antarctic_bottom_water.svg/180px-Antarctic_bottom_water.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/e/e7/Antarctic_bottom_water.svg/240px-Antarctic_bottom_water.svg.png 2x" data-file-width="745" data-file-height="470" /></a></span></div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Ocean_current" title="Ocean current">Circulation</a></th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Atmospheric_circulation" title="Atmospheric circulation">Atmospheric circulation</a></li> <li><a href="/wiki/Baroclinity" title="Baroclinity">Baroclinity</a></li> <li><a href="/wiki/Boundary_current" title="Boundary current">Boundary current</a></li> <li><a href="/wiki/Coriolis_force" title="Coriolis force">Coriolis force</a></li> <li><a href="/wiki/Coriolis%E2%80%93Stokes_force" title="Coriolis–Stokes force">Coriolis–Stokes force</a></li> <li><a href="/wiki/Craik%E2%80%93Leibovich_vortex_force" title="Craik–Leibovich vortex force">Craik–Leibovich vortex force</a></li> <li><a href="/wiki/Downwelling" title="Downwelling">Downwelling</a></li> <li><a href="/wiki/Eddy_(fluid_dynamics)" title="Eddy (fluid dynamics)">Eddy</a></li> <li><a href="/wiki/Ekman_layer" title="Ekman layer">Ekman layer</a></li> <li><a href="/wiki/Ekman_spiral" title="Ekman spiral">Ekman spiral</a></li> <li><a href="/wiki/Ekman_transport" title="Ekman transport">Ekman transport</a></li> <li><a href="/wiki/El_Ni%C3%B1o%E2%80%93Southern_Oscillation" title="El Niño–Southern Oscillation">El Niño–Southern Oscillation</a></li> <li><a href="/wiki/General_circulation_model" title="General circulation model">General circulation model</a></li> <li><a href="/wiki/Geochemical_Ocean_Sections_Study" title="Geochemical Ocean Sections Study">Geochemical Ocean Sections Study</a></li> <li><a href="/wiki/Geostrophic_current" title="Geostrophic current">Geostrophic current</a></li> <li><a href="/wiki/Global_Ocean_Data_Analysis_Project" title="Global Ocean Data Analysis Project">Global Ocean Data Analysis Project</a></li> <li><a href="/wiki/Gulf_Stream" title="Gulf Stream">Gulf Stream</a></li> <li><a href="/wiki/Humboldt_Current" title="Humboldt Current">Humboldt Current</a></li> <li><a href="/wiki/Hydrothermal_circulation" title="Hydrothermal circulation">Hydrothermal circulation</a></li> <li><a href="/wiki/Langmuir_circulation" title="Langmuir circulation">Langmuir circulation</a></li> <li><a href="/wiki/Longshore_drift" title="Longshore drift">Longshore drift</a></li> <li><a href="/wiki/Loop_Current" title="Loop Current">Loop Current</a></li> <li><a href="/wiki/Modular_Ocean_Model" title="Modular Ocean Model">Modular Ocean Model</a></li> <li><a href="/wiki/Ocean_current" title="Ocean current">Ocean current</a></li> <li><a href="/wiki/Ocean_dynamical_thermostat" title="Ocean dynamical thermostat">Ocean dynamical thermostat</a></li> <li><a href="/wiki/Ocean_dynamics" title="Ocean dynamics">Ocean dynamics</a></li> <li><a href="/wiki/Ocean_gyre" title="Ocean gyre">Ocean gyre</a></li> <li><a href="/wiki/Overflow_(oceanography)" title="Overflow (oceanography)">Overflow</a></li> <li><a href="/wiki/Princeton_Ocean_Model" title="Princeton Ocean Model">Princeton Ocean Model</a></li> <li><a href="/wiki/Rip_current" title="Rip current">Rip current</a></li> <li><a href="/wiki/Subsurface_ocean_current" title="Subsurface ocean current">Subsurface ocean current</a></li> <li><a href="/wiki/Sverdrup_balance" title="Sverdrup balance">Sverdrup balance</a></li> <li><a href="/wiki/Thermohaline_circulation" title="Thermohaline circulation">Thermohaline circulation</a> <ul><li><a href="/wiki/Shutdown_of_thermohaline_circulation" class="mw-redirect" title="Shutdown of thermohaline circulation">shutdown</a></li></ul></li> <li><a href="/wiki/Upwelling" title="Upwelling">Upwelling</a></li> <li><a href="/wiki/Whirlpool" title="Whirlpool">Whirlpool</a></li> <li><a href="/wiki/Wind_generated_current" title="Wind generated current">Wind generated current</a></li> <li><a href="/wiki/World_Ocean_Circulation_Experiment" title="World Ocean Circulation Experiment">World Ocean Circulation Experiment</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Tide" title="Tide">Tides</a></th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Amphidromic_point" title="Amphidromic point">Amphidromic point</a></li> <li><a href="/wiki/Earth_tide" title="Earth tide">Earth tide</a></li> <li><a href="/wiki/Head_of_tide" title="Head of tide">Head of tide</a></li> <li><a href="/wiki/Internal_tide" title="Internal tide">Internal tide</a></li> <li><a href="/wiki/Lunitidal_interval" title="Lunitidal interval">Lunitidal interval</a></li> <li><a href="/wiki/Perigean_spring_tide" title="Perigean spring tide">Perigean spring tide</a></li> <li><a href="/wiki/Rip_tide" title="Rip tide">Rip tide</a></li> <li><a href="/wiki/Rule_of_twelfths" title="Rule of twelfths">Rule of twelfths</a></li> <li><a href="/wiki/Slack_tide" title="Slack tide">Slack tide</a></li> <li><a href="/wiki/Theory_of_tides" title="Theory of tides">Theory of tides</a></li> <li><a href="/wiki/Tidal_bore" title="Tidal bore">Tidal bore</a></li> <li><a href="/wiki/Tidal_force" title="Tidal force">Tidal force</a></li> <li><a href="/wiki/Tidal_power" title="Tidal power">Tidal power</a></li> <li><a href="/wiki/Tidal_race" title="Tidal race">Tidal race</a></li> <li><a href="/wiki/Tidal_range" title="Tidal range">Tidal range</a></li> <li><a href="/wiki/Tidal_resonance" title="Tidal resonance">Tidal resonance</a></li> <li><a href="/wiki/Tide_gauge" title="Tide gauge">Tide gauge</a></li> <li><a href="/wiki/Tideline" title="Tideline">Tideline</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Landform" title="Landform">Landforms</a></th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Abyssal_fan" title="Abyssal fan">Abyssal fan</a></li> <li><a href="/wiki/Abyssal_plain" title="Abyssal plain">Abyssal plain</a></li> <li><a href="/wiki/Atoll" title="Atoll">Atoll</a></li> <li><a href="/wiki/Bathymetric_chart" title="Bathymetric chart">Bathymetric chart</a></li> <li><a href="/wiki/Carbonate_platform" title="Carbonate platform">Carbonate platform</a></li> <li><a href="/wiki/Coastal_geography" title="Coastal geography">Coastal geography</a></li> <li><a href="/wiki/Cold_seep" title="Cold seep">Cold seep</a></li> <li><a href="/wiki/Continental_margin" title="Continental margin">Continental margin</a></li> <li><a href="/wiki/Continental_rise" title="Continental rise">Continental rise</a></li> <li><a href="/wiki/Continental_shelf" title="Continental shelf">Continental shelf</a></li> <li><a href="/wiki/Contourite" title="Contourite">Contourite</a></li> <li><a href="/wiki/Guyot" title="Guyot">Guyot</a></li> <li><a href="/wiki/Hydrography" title="Hydrography">Hydrography</a></li> <li><a href="/wiki/Knoll_(oceanography)" title="Knoll (oceanography)">Knoll</a></li> <li><a href="/wiki/Ocean_bank" title="Ocean bank">Ocean bank</a></li> <li><a href="/wiki/Oceanic_basin" title="Oceanic basin">Oceanic basin</a></li> <li><a href="/wiki/Oceanic_plateau" title="Oceanic plateau">Oceanic plateau</a></li> <li><a href="/wiki/Oceanic_trench" title="Oceanic trench">Oceanic trench</a></li> <li><a href="/wiki/Passive_margin" title="Passive margin">Passive margin</a></li> <li><a href="/wiki/Seabed" title="Seabed">Seabed</a></li> <li><a href="/wiki/Seamount" title="Seamount">Seamount</a></li> <li><a href="/wiki/Submarine_canyon" title="Submarine canyon">Submarine canyon</a></li> <li><a href="/wiki/Submarine_volcano" title="Submarine volcano">Submarine volcano</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Plate_tectonics" title="Plate tectonics">Plate<br />tectonics</a></th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Convergent_boundary" title="Convergent boundary">Convergent boundary</a></li> <li><a href="/wiki/Divergent_boundary" title="Divergent boundary">Divergent boundary</a></li> <li><a href="/wiki/Fracture_zone" title="Fracture zone">Fracture zone</a></li> <li><a href="/wiki/Hydrothermal_vent" title="Hydrothermal vent">Hydrothermal vent</a></li> <li><a href="/wiki/Marine_geology" title="Marine geology">Marine geology</a></li> <li><a href="/wiki/Mid-ocean_ridge" title="Mid-ocean ridge">Mid-ocean ridge</a></li> <li><a href="/wiki/Mohorovi%C4%8Di%C4%87_discontinuity" title="Mohorovičić discontinuity">Mohorovičić discontinuity</a></li> <li><a class="mw-selflink selflink">Oceanic crust</a></li> <li><a href="/wiki/Outer_trench_swell" title="Outer trench swell">Outer trench swell</a></li> <li><a href="/wiki/Ridge_push" title="Ridge push">Ridge push</a></li> <li><a href="/wiki/Seafloor_spreading" title="Seafloor spreading">Seafloor spreading</a></li> <li><a href="/wiki/Slab_pull" title="Slab pull">Slab pull</a></li> <li><a href="/wiki/Slab_suction" title="Slab suction">Slab suction</a></li> <li><a href="/wiki/Slab_window" title="Slab window">Slab window</a></li> <li><a href="/wiki/Subduction" title="Subduction">Subduction</a></li> <li><a href="/wiki/Transform_fault" title="Transform fault">Transform fault</a></li> <li><a href="/wiki/Vine%E2%80%93Matthews%E2%80%93Morley_hypothesis" title="Vine–Matthews–Morley hypothesis">Vine–Matthews–Morley hypothesis</a></li> <li><a href="/wiki/Volcanic_arc" title="Volcanic arc">Volcanic arc</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Ocean zones</th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Benthic_zone" title="Benthic zone">Benthic</a></li> <li><a href="/wiki/Deep_ocean_water" title="Deep ocean water">Deep ocean water</a></li> <li><a href="/wiki/Deep_sea" title="Deep sea">Deep sea</a></li> <li><a href="/wiki/Littoral_zone" title="Littoral zone">Littoral</a></li> <li><a href="/wiki/Mesopelagic_zone" title="Mesopelagic zone">Mesopelagic</a></li> <li><a href="/wiki/Oceanic_zone" title="Oceanic zone">Oceanic</a></li> <li><a href="/wiki/Pelagic_zone" title="Pelagic zone">Pelagic</a></li> <li><a href="/wiki/Photic_zone" title="Photic zone">Photic</a></li> <li><a href="/wiki/Surf_zone" title="Surf zone">Surf</a></li> <li><a href="/wiki/Swash" title="Swash">Swash</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Sea_level" title="Sea level">Sea level</a></th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Deep-ocean_Assessment_and_Reporting_of_Tsunamis" title="Deep-ocean Assessment and Reporting of Tsunamis">Deep-ocean Assessment and Reporting of Tsunamis</a></li> <li><a href="/wiki/Global_Sea_Level_Observing_System" title="Global Sea Level Observing System">Global Sea Level Observing System</a></li> <li><a href="/wiki/North_West_Shelf_Operational_Oceanographic_System" title="North West Shelf Operational Oceanographic System">North West Shelf Operational Oceanographic System</a></li> <li><a href="/wiki/Sea-level_curve" title="Sea-level curve">Sea-level curve</a></li> <li><a href="/wiki/Sea_level_drop" title="Sea level drop">Sea level drop</a></li> <li><a href="/wiki/Sea_level_rise" title="Sea level rise">Sea level rise</a></li> <li><a href="/wiki/World_Geodetic_System" title="World Geodetic System">World Geodetic System</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Acoustical_oceanography" class="mw-redirect" title="Acoustical oceanography">Acoustics</a></th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Deep_scattering_layer" title="Deep scattering layer">Deep scattering layer</a></li> <li><a href="/wiki/Ocean_acoustic_tomography" title="Ocean acoustic tomography">Ocean acoustic tomography</a></li> <li><a href="/wiki/Sofar_bomb" title="Sofar bomb">Sofar bomb</a></li> <li><a href="/wiki/SOFAR_channel" title="SOFAR channel">SOFAR channel</a></li> <li><a href="/wiki/Underwater_acoustics" title="Underwater acoustics">Underwater acoustics</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Satellites</th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Jason-1" title="Jason-1">Jason-1</a></li> <li><a href="/wiki/OSTM/Jason-2" title="OSTM/Jason-2">OSTM/Jason-2</a></li> <li><a href="/wiki/Jason-3" title="Jason-3">Jason-3</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Related</th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Ocean_acidification" title="Ocean acidification">Acidification</a></li> <li><a href="/wiki/Argo_(oceanography)" title="Argo (oceanography)">Argo</a></li> <li><a href="/wiki/Benthic_lander" title="Benthic lander">Benthic lander</a></li> <li><a href="/wiki/Color_of_water" title="Color of water">Color of water</a></li> <li><a href="/wiki/DSV_Alvin" title="DSV Alvin">DSV <i>Alvin</i></a></li> <li><a href="/wiki/Marginal_sea" class="mw-redirect" title="Marginal sea">Marginal sea</a></li> <li><a href="/wiki/Marine_energy" title="Marine energy">Marine energy</a></li> <li><a href="/wiki/Marine_pollution" title="Marine pollution">Marine pollution</a></li> <li><a href="/wiki/Mooring_(oceanography)" title="Mooring (oceanography)">Mooring</a></li> <li><a href="/wiki/National_Oceanographic_Data_Center" title="National Oceanographic Data Center">National Oceanographic Data Center</a></li> <li><a href="/wiki/Ocean" title="Ocean">Ocean</a></li> <li><a href="/wiki/Ocean_exploration" title="Ocean exploration">Explorations</a></li> <li><a href="/wiki/Ocean_observations" title="Ocean observations">Observations</a></li> <li><a href="/wiki/Ocean_reanalysis" title="Ocean reanalysis">Reanalysis</a></li> <li><a href="/wiki/Ocean_surface_topography" title="Ocean surface topography">Ocean surface topography</a></li> <li><a href="/wiki/Ocean_temperature" title="Ocean temperature">Ocean temperature</a></li> <li><a href="/wiki/Ocean_thermal_energy_conversion" title="Ocean thermal energy conversion">Ocean thermal energy conversion</a></li> <li><a href="/wiki/Oceanography" title="Oceanography">Oceanography</a> <ul><li><a href="/wiki/Outline_of_oceanography" title="Outline of oceanography">Outline of oceanography</a></li></ul></li> <li><a href="/wiki/Pelagic_sediment" title="Pelagic sediment">Pelagic sediment</a></li> <li><a href="/wiki/Sea_surface_microlayer" title="Sea surface microlayer">Sea surface microlayer</a></li> <li><a href="/wiki/Sea_surface_temperature" title="Sea surface temperature">Sea surface temperature</a></li> <li><a href="/wiki/Seawater" title="Seawater">Seawater</a></li> <li><a href="/wiki/Science_On_a_Sphere" title="Science On a Sphere">Science On a Sphere</a></li> <li><a href="/wiki/Ocean_stratification" title="Ocean stratification">Stratification</a></li> <li><a href="/wiki/Thermocline" title="Thermocline">Thermocline</a></li> <li><a href="/wiki/Underwater_glider" title="Underwater glider">Underwater glider</a></li> <li><a href="/wiki/Water_column" title="Water column">Water column</a></li> <li><a href="/wiki/World_Ocean_Atlas" title="World Ocean Atlas">World Ocean Atlas</a></li></ul> </div></td></tr><tr><td class="navbox-abovebelow" colspan="3"><div> <ul><li><span class="noviewer" typeof="mw:File"><span title="Category"><img alt="" src="//upload.wikimedia.org/wikipedia/en/thumb/9/96/Symbol_category_class.svg/16px-Symbol_category_class.svg.png" decoding="async" width="16" height="16" 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