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A Tale of Two Submerged Continents | Britannica
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Rafferty" data-title="A Tale of Two Submerged Continents" data-published-date="7 Apr. 2017" data-url="https://www.britannica.com/story/a-tale-of-two-submerged-continents" > <div class="citation-text"></div> </div> <button class="js-copy-citation-button mt-20 btn btn-xs btn-outline-blue border shadow-sm pr-10" > <em class="material-icons md-icon ml-n10 my-n5 mr-5" data-icon="file_copy"></em> <span class="js-citation-status-text">Copy Citation</span> </button> </div> </div> </div> <div> <button class="js-share-modal-button js-modal gtm-topic-tool btn btn-xs btn-outline-blue border shadow-sm pr-10" data-modal=".md-share-modal"> <em class="material-icons md-icon ml-n10 my-n5 mr-5" data-icon="share"></em> Share </button> <div class="md-share-modal size-lg d-none qa-share-modal"> <div class="md-modal-body"> <div class="h2 font-serif d-flex align-items-center pb-15 border-bottom"> <em class="material-icons text-blue mr-10" data-icon="share"></em> Share </div> <div class="label my-20">Share to social media</div> <div class="md-social-toolbar-circle d-flex align-items-start inverted" data-value="share" title="A Tale of Two Submerged Continents" data-url="https://www.britannica.com/story/a-tale-of-two-submerged-continents" > <a class="social-icon facebook justify-content-center d-flex align-items-center align-self-center" data-provider="facebook" href="https://www.facebook.com/BRITANNICA/" target="_blank" rel="noopener"><span>Facebook</span></a> <a class="social-icon x justify-content-center d-flex align-items-center align-self-center" data-provider="x" href="https://x.com/britannica" target="_blank" rel="noopener"><span>X</span></a> </div> <div class="label pt-20 mt-20 mb-5 border-top">URL</div> <a class="font-serif text-truncate d-inline-block" href="https://www.britannica.com/story/a-tale-of-two-submerged-continents">https://www.britannica.com/story/a-tale-of-two-submerged-continents</a> </div> </div> </div> </div> <div class="md-byline module-spacing font-12"> <div class="font-serif font-12"> <span class="written-by text-gray-700"> Written by </span> <div class="editor-popover popover p-0"> <a class="d-block p-20 gtm-byline font-12 byline-contributor" href="/editor/John-P-Rafferty/6747" > <div class="editor-title font-16 font-weight-bold">John P. Rafferty</div> <div class="editor-description font-12 font-serif mt-5 clamp-description text-black">John P. Rafferty writes about Earth processes and the environment. He serves currently as the editor of Earth and life sciences, covering climatology, geology, zoology, and other topics that relate to...</div> </a> <div data-popper-arrow></div> </div> <span class="btn btn-link editor-link p-0 qa-byline-link gtm-byline font-12 byline-contributor text-decoration-underline"> John P. Rafferty</span></div> <div class="font-serif font-12 text-gray-700"> <span class="qa-fact-checked-by">Fact-checked by</span> <div class="editor-popover popover p-0"> <a class="d-block p-20 font-12" href="/editor/The-Editors-of-Encyclopaedia-Britannica/4419" > <div class="editor-title font-16 font-weight-bold">The Editors of Encyclopaedia Britannica</div> <div class="editor-description font-12 font-serif mt-5 text-black">Encyclopaedia Britannica's editors oversee subject areas in which they have extensive knowledge, whether from years of experience gained by working on that content or via study for an advanced degree. They write new content and verify and edit content received from contributors.</div> </a> <div data-popper-arrow></div> </div> <span class="btn btn-link editor-link p-0 qa-byline-link font-12 "> The Editors of Encyclopaedia Britannica</span></div></div> </div> <article class="topic-content content mt-20"><figure class="md-assembly md-feature-assembly print-false" data-type="1" data-descid="1"><div class="md-assembly-wrapper card-media " data-type="image"><a href="https://cdn.britannica.com/66/194766-050-5908DD25/canyon-swell-reef-sunlight-water-surface-Pacific.jpg" target="_blank" class="gtm-assembly-link position-relative d-flex align-items-center justify-content-center " data-href="*"><img src="https://cdn.britannica.com/66/194766-050-5908DD25/canyon-swell-reef-sunlight-water-surface-Pacific.jpg?w=600&q=60" alt="Small canyon underwater carved by the swell into the fore reef with sunlight through water surface, Huahine island, Pacific ocean, French Polynesia." data-width="1600" data-height="1067" loading="eager"><button class="magnifying-glass btn btn-circle position-absolute shadow btn-white top-10 right-10" aria-label="Zoom in"><em class="material-icons link-blue" data-icon="zoom_in"></em></button></a></div><figcaption class=""><div class="md-assembly-caption text-muted font-14 font-serif line-clamp"><span><button class="js-more-btn d-none btn btn-unstyled font-12 bg-white js-content" aria-label="Toggle more/less fact data"><span class="link-blue">(more)</span></button></span></div><cite class="credit d-block mt-5">漏 Seaphotoart/Dreamstime.com</cite></figcaption></figure><!--[BP1]--><p class="topic-paragraph">In February 2017 separate studies examining Earth鈥檚 geological and geophysical characteristics revealed evidence of ancient sunken <a href="https://www.britannica.com/science/continent" class="md-crosslink " data-show-preview="true">continents</a> in the Indian and Pacific Oceans.</p><!--[P1]--><!--[MOD1]--><span class="MOD1"></span><!--[BP2]--><p class="topic-paragraph">In the first study, a multinational team made up of South African, German, and Norwegian geologists and geophysicists noticed a large region of gravitational anomalies beneath the <a href="https://www.britannica.com/place/Indian-Ocean" class="md-crosslink " data-show-preview="true">Indian Ocean</a>. This difference in <a href="https://www.britannica.com/science/gravity-physics" class="md-crosslink " data-show-preview="true">gravity</a> suggested the presence of a dense mass of continental crust in the Indian Ocean between <a href="https://www.britannica.com/place/Madagascar" class="md-crosslink " data-show-preview="true">Madagascar</a> and India. The scientists reported that the gravity data was later combined with data showing the discovery of <a href="https://www.britannica.com/science/zircon" class="md-crosslink " data-show-preview="true">zircons</a> (a type of silicate mineral of volcanic origin) dated to between 2.5 billion and 3 billion years ago within far younger volcanic rocks on <a href="https://www.britannica.com/place/Mauritius" class="md-crosslink " data-show-preview="true">Mauritius</a> (an island that is thought to have formed about 8 million years ago). The age differences between rocks on the island and the zircons within the rocks suggested that the zircons formed on a landmass much older than the present-day island. The scientists hypothesized that volcanism stemming from the tectonic <a href="https://www.britannica.com/science/hotspot-geology" class="md-crosslink " data-show-preview="true">hotspot</a> that grew into Mauritius could have transported zircons from submerged continental crust to the island鈥檚 surface. The combination of the gravitational data with that provided by the zircons suggested the presence of a large, arc-shaped, submerged landmass (which the scientists called Mauritia) that extends from Mauritius to India鈥檚 southwestern coast.</p><!--[P2]--><!--[MOD2]--><span class="MOD2"></span><!--[BP3]--><p class="topic-paragraph">Similarly, an analysis of gravitational maps of the southern <a href="https://www.britannica.com/place/Pacific-Ocean" class="md-crosslink " data-show-preview="true">Pacific Ocean</a> near Australia鈥檚 eastern coast showed the presence of a large underwater <a href="https://www.britannica.com/science/plateau-landform" class="md-crosslink " data-show-preview="true">plateau</a> upon which present-day <a href="https://www.britannica.com/place/New-Caledonia-French-unique-collectivity-Pacific-Ocean" class="md-crosslink " data-show-preview="true">New Caledonia</a>, <a href="https://www.britannica.com/place/New-Zealand" class="md-crosslink " data-show-preview="true">New Zealand</a>, and other smaller islands sit. Samples taken from the sea floor reveal that the plateau is also made up of continental crust and not the denser <a href="https://www.britannica.com/science/oceanic-crust" class="md-crosslink " data-show-preview="true">oceanic crust</a> common to other underwater features in the ocean. Scientists claimed that this large underwater plateau (which they called Zealandia) was once an emergent continent that was connected to <a href="https://www.britannica.com/place/Gondwana-supercontinent" class="md-crosslink " data-show-preview="true">Gondwana</a> (a supercontinent which lasted from perhaps 600 million to 140 million years ago). Zealandia, it seems, slipped beneath the waves sometime after it broke away from Australia about 80 million years ago. </p><!--[P3]--><!--[MOD3]--><span class="MOD3"></span><figure class="md-assembly md-feature-assembly print-false" data-type="1" data-descid="2"><div class="md-assembly-wrapper card-media " data-type="image"><a href="https://cdn.britannica.com/04/194204-050-32C2AD57/Infographic-continents-evidence-history-Earth.jpg" target="_blank" class="gtm-assembly-link position-relative d-flex align-items-center justify-content-center " data-href="*"><img src="https://cdn.britannica.com/04/194204-050-32C2AD57/Infographic-continents-evidence-history-Earth.jpg" alt="Paleocontinents infographic. Mauritia, Zealandia, Rodinia, Laurentia, Pangea, Gondwana." data-width="1600" data-height="1067" loading="eager"><button class="magnifying-glass btn btn-circle position-absolute shadow btn-white top-10 right-10" aria-label="Zoom in"><em class="material-icons link-blue" data-icon="zoom_in"></em></button></a></div><figcaption class=""><div class="md-assembly-caption text-muted font-14 font-serif line-clamp"><span><a class="gtm-assembly-link md-assembly-title font-weight-bold d-inline font-sans-serif mr-5 media-overlay-link" target="_blank" href="https://cdn.britannica.com/04/194204-050-32C2AD57/Infographic-continents-evidence-history-Earth.jpg" data-href="*">Submerged continents</a><span>The infographic gives more information about the submerged continents of Mauritia and Zealandia.</span><button class="js-more-btn d-none btn btn-unstyled font-12 bg-white js-content" aria-label="Toggle more/less fact data"><span class="link-blue">(more)</span></button></span></div><cite class="credit d-block mt-5">Encyclop忙dia Britannica, Inc./Kenny Chmielewski</cite></figcaption></figure><span class="AM-END-OF-ARTICLE am-inline"></span></article><div class="related-info grid"><!--[RELATED-TOPICS]--><div class="col"><div class="learn-more"><h3>Learn More About This Topic</h3><ul class="list-unstyled"><li><a href="https://www.britannica.com/science/continent" class="md-crosslink " data-show-preview="true">What is a continent?</a></li><li><a href="https://www.britannica.com/science/zircon" class="md-crosslink " data-show-preview="true">Which chemical elements are used to create zircon?</a></li><li><a href="https://www.britannica.com/place/Gondwana-supercontinent" class="md-crosslink " data-show-preview="true">Which present-day landmasses were once part of Gondwana?</a></li></ul></div></div><div class="col-md-auto col-100"> <div class="related-feature mb-30"> <div class="box"> <a href="/story/is-australia-an-island" > <div class="feature-type">Story</div> <img loading="lazy" src="https://cdn.britannica.com/86/183586-131-98C46E36/World-Data-Locator-Map-Australia.jpg?w=225&h=120" alt="World Data Locator Map: Australia" /> <strong>Is Australia an Island?</strong> <p>What鈥檚 the difference between an island and a continent anyway?</p> </a> </div> </div> </div></div> </div> </div> </div> <aside class="cm-rightrail d-none d-md-block ad-rail"></aside> </div> </div> </div> </div> </main> <div class="grid gx-0"> <div class="col"> <div class="md-loading hidden display-4 font-weight-normal"></div> <div class="text-center my-20 mb-100"> <button class="md-infinite-load-next btn btn-blue" data-value="next-page">Load More</button> </div> </div> <div class="col-md-da-320 hidden-xs"> </div> </div></div> </div> </main> <div id="md-footer"></div> <noscript><iframe src="//www.googletagmanager.com/ns.html?id=GTM-5W6NC8" height="0" width="0" style="display:none;visibility:hidden"></iframe></noscript> <script type="text/javascript" id="_informizely_script_tag"> var IzWidget = IzWidget || {}; 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