{"id":540567,"date":"2026-07-09T07:02:11","date_gmt":"2026-07-09T07:02:11","guid":{"rendered":"https:\/\/www.newsbeep.com\/ie\/540567\/"},"modified":"2026-07-09T07:02:11","modified_gmt":"2026-07-09T07:02:11","slug":"earths-longest-volcanic-ridge-may-be-an-underwater-moving-hotspot","status":"publish","type":"post","link":"https:\/\/www.newsbeep.com\/ie\/540567\/","title":{"rendered":"Earth\u2019s Longest Volcanic Ridge May Be an Underwater Moving Hotspot"},"content":{"rendered":"<p><a href=\"https:\/\/www.newsbeep.com\/ie\/wp-content\/uploads\/2026\/07\/NinetyEastRidge.jpg\"><img fetchpriority=\"high\" decoding=\"async\" width=\"676\" height=\"506\" src=\"https:\/\/www.newsbeep.com\/ie\/wp-content\/uploads\/2026\/07\/NinetyEastRidge.jpg\" alt=\"\" class=\"wp-image-274681\"\/><\/a>Ninetyeast Ridge, the long, pale-blue line slicing through the Indian Ocean near 90 degrees east, is the largest underwater mountain ridge in the world. Image via Wiki Commons.<\/p>\n<p class=\"wp-block-paragraph\">The deep oceans are far from flat. They feature ridges, trenches, seamounts, and valleys, creating a diverse and dramatic underwater landscape shaped by tectonic activity and volcanic processes. Among this landscape, the Ninetyeast Ridge is one of the most impressive features.<\/p>\n<p class=\"wp-block-paragraph\">It\u2019s not the largest underwater ridge in the strictest sense \u2014 the global mid-ocean ridge system is far longer. But the Ninetyeast Ridge is often described more precisely as the world\u2019s longest straight underwater mountain chain, or Earth\u2019s longest preserved linear volcanic ridge.<\/p>\n<p class=\"wp-block-paragraph\">It stretches over 5,000 kilometers beneath the Indian Ocean, making it the Earth\u2019s longest <a data-wpil-monitor-id=\"1194\" href=\"https:\/\/www.zmescience.com\/science\/ocean-life-carbon-emissions-825132\/\" rel=\"nofollow noopener\" target=\"_blank\">linear volcanic<\/a> ridge. It also has an <a href=\"https:\/\/academic.oup.com\/petrology\/article-abstract\/54\/6\/1177\/1409380?redirectedFrom=fulltext#:~:text=The%20Ninetyeast%20Ridge%20rises%20to,et%20al.%2C%201991).\" rel=\"nofollow noopener\" target=\"_blank\">average width of around<\/a> 200 km and a top height of 3.5 km. This is a mountain range on the scale of the Rockies, but hidden under thousands of meters of water. It\u2019s also quite mysterious, it turns out.<\/p>\n<p class=\"wp-block-paragraph\">A new research employing advanced geophysical techniques concludes that the ridge was formed by a geological \u201chotspot\u201d, challenging assumptions about how plumes of molten material from the mantle move and interact with tectonic plates.<\/p>\n<p>What\u2019s a hotspot?<\/p>\n<p class=\"wp-block-paragraph\">We tend to think of the <a data-wpil-monitor-id=\"1197\" href=\"https:\/\/www.zmescience.com\/science\/news-science\/model-earth-surface-evolution\/\" rel=\"nofollow noopener\" target=\"_blank\">Earth\u2019s surface<\/a> as stationary but in reality, it moves around quite a bit \u2014 just very slowly. The Earth\u2019s outer shell (<a href=\"https:\/\/www.zmescience.com\/feature-post\/natural-sciences\/geology-and-paleontology\/planet-earth\/thinnest-layer-earth\/\" rel=\"nofollow noopener\" target=\"_blank\">called the crust<\/a>) is divided into large, rigid plates. These plates move on the <a data-wpil-monitor-id=\"1200\" href=\"https:\/\/www.zmescience.com\/science\/news-science\/scientists-find-ancient-250-million-year-old-seafloor-from-the-time-of-dinosaurs-hidden-in-earths-mantle\/\" rel=\"nofollow noopener\" target=\"_blank\">semi-fluid mantle<\/a> beneath. Convection currents in the mantle (with the hot mantle floating to the surface and the cooler, denser mantle going downwards) are what push these tectonic plates. This interaction shapes the entire planet\u2019s surface, <a data-wpil-monitor-id=\"1192\" href=\"https:\/\/www.zmescience.com\/feature-post\/natural-sciences\/geography\/mountain-files-the-5-tallest-mountains-on-earth\/\" rel=\"nofollow noopener\" target=\"_blank\">creating mountains<\/a>, earthquakes, and volcanoes.<\/p>\n<p><a href=\"https:\/\/cdn.zmescience.com\/wp-content\/uploads\/2024\/12\/Models_of_mantle_dynamics-1.jpg\" rel=\"nofollow noopener\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"508\" alt=\"\" class=\"wp-image-274683 perfmatters-lazy\" src=\"https:\/\/www.newsbeep.com\/ie\/wp-content\/uploads\/2026\/07\/Models_of_mantle_dynamics-1-1024x508.jpg\"  data-\/><\/a>The movement we see on the Earth\u2019s surface is largely guided by convection currents in the mantle. This is what pushes tectonic plates apart in some areas and pushes them against each other in other areas. Image in public domain.<\/p>\n<p class=\"wp-block-paragraph\">In some areas, the plates move away from each other, forming new bits of crust, as seen at mid-ocean ridges. In other areas, called convergent boundaries, one plate dives beneath another, causing mountain ranges or <a data-wpil-monitor-id=\"1193\" href=\"https:\/\/www.zmescience.com\/science\/physics\/mariana-trench-james-cameron-13122012\/\" rel=\"nofollow noopener\" target=\"_blank\">deep ocean trenches<\/a>. Hotspots are special areas.<\/p>\n<p class=\"wp-block-paragraph\">Unlike most volcanic activity, which occurs at <a data-wpil-monitor-id=\"1196\" href=\"https:\/\/www.zmescience.com\/feature-post\/natural-sciences\/geology-and-paleontology\/earth-dynamics\/plate-tectonics-we-figured-out-how-to-build-an-atomic-bomb-before-we-realized-how-mountains-form\/\" rel=\"nofollow noopener\" target=\"_blank\">tectonic plate boundaries<\/a>, hotspots can form in the middle of tectonic plates. They are powered by mantle plumes\u2014columns of hot, <a data-wpil-monitor-id=\"1198\" href=\"https:\/\/www.zmescience.com\/feature-post\/natural-sciences\/geology-and-paleontology\/rocks-and-minerals\/most-common-types-of-rocks\/\" rel=\"nofollow noopener\" target=\"_blank\">buoyant rock<\/a> rising from deep within the Earth. These hotspot plumes are stationary; as tectonic plates move over these stationary plumes, they create features like island chains or ridges, such as the Hawaiian Islands or the Ninetyeast Ridge. The movement of plates over hotspots leaves a trail of volcanoes that can help scientists track the plates\u2019 past movements and understand mantle dynamics.<\/p>\n<p class=\"wp-block-paragraph\">At least, that was the theory until now.<\/p>\n<p>\u00d7<\/p>\n<p>                        Thank you! One more thing&#8230;<\/p>\n<p>Please check your inbox and confirm your subscription.<\/p>\n<p class=\"wp-block-paragraph\">The new data suggests the Ninetyeast Ridge, and the underlying Kerguelen hotspot, suggests that hotspots are not as static as we thought.<\/p>\n<p class=\"wp-block-paragraph\">Using precise Argon dating methods (40Ar\/39Ar) and a technique called seismic tomography, researchers have mapped the volcanic progression along the ridge with unprecedented accuracy. This work reveals that the Kerguelen hotspot exhibited variable motion, influenced by interactions with the Indian\u2013Antarctic spreading ridge. These findings mark a significant departure from earlier models that assumed a constant volcanic progression rate.<\/p>\n<p><a href=\"https:\/\/www.newsbeep.com\/ie\/wp-content\/uploads\/2026\/07\/hot-spot-track-3-10x.webp\"><img loading=\"lazy\" decoding=\"async\" width=\"650\" height=\"443\" alt=\"Active volcano diagram showing magma movement and tectonic plates at ZME Science.\" class=\"wp-image-274685 perfmatters-lazy\" src=\"https:\/\/www.newsbeep.com\/ie\/wp-content\/uploads\/2026\/07\/hot-spot-track-3-10x.webp\"\/><\/a>Depiction of a hotspot rising towards the surface. The hotspot is stationary while the tectonic plates move over it. Image via Wiki Commons.<\/p>\n<p>Seeing into the bowels of an underwater mountain<\/p>\n<p class=\"wp-block-paragraph\">Seismic tomography is a technique that uses <a data-wpil-monitor-id=\"1195\" href=\"https:\/\/www.zmescience.com\/science\/geology\/the-types-of-seismic-waves\/\" rel=\"nofollow noopener\" target=\"_blank\">seismic waves<\/a> generated by earthquakes or artificial sources to create three-dimensional images of Earth\u2019s interior. These waves travel at different speeds depending on the density, temperature, and composition of the material they pass through. By analyzing the travel times and paths of seismic waves, scientists can map structures in the mantle, such as mantle plumes and ponding zones \u2014 all key to understanding hotspot dynamics.<\/p>\n<p class=\"wp-block-paragraph\">Geochronology methods, particularly 40Ar\/39Ar dating, were used to determine the ages of volcanic rocks along the Ninetyeast Ridge. This technique measures the decay of radioactive isotopes in minerals, specifically the ratio of argon isotopes, to calculate the time since the rock solidified.<\/p>\n<p class=\"wp-block-paragraph\">Combining these ages with the plate movement history and seismic imaging, the study reconstructed the volcanic progression of the ridge and the motion of the Kerguelen hotspot over millions of years, providing a comprehensive picture of how <a href=\"https:\/\/www.zmescience.com\/science\/geology\/seismic-wave-hot-blog-16062020\/\" rel=\"nofollow noopener\" target=\"_blank\">the mantle plumes interact<\/a> with the crust.<\/p>\n<p><a href=\"https:\/\/cdn.zmescience.com\/wp-content\/uploads\/2024\/12\/ninetyeast-ridge.png\" rel=\"nofollow noopener\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"737\" alt=\"Earth's underwater ridge map showcasing tectonic activity and oceanic features.\" class=\"wp-image-274686 perfmatters-lazy\" src=\"https:\/\/www.newsbeep.com\/ie\/wp-content\/uploads\/2026\/07\/ninetyeast-ridge-1024x737.png\"  data-\/><\/a>A gravity map of the Ninetyeast Ridge and nearby geological features. Variations in density change the local gravitational field, and these differences can be imaged on such a gravity map. Image via Wiki Commons.<\/p>\n<p class=\"wp-block-paragraph\">The study\u2019s main conclusion is that the Kerguelen hotspot, responsible for creating the Ninetyeast Ridge, exhibited significant motion over time. The hotspot moved due to influence by interactions with the Indian\u2013Antarctic spreading ridge.<\/p>\n<p class=\"wp-block-paragraph\">The idea that hotspots can also move around is not new, but it\u2019s very difficult to prove, says <a href=\"https:\/\/staffportal.curtin.edu.au\/staff\/profile\/view\/hugo-olierook-53cb80e8\/\" rel=\"nofollow noopener\" target=\"_blank\">Dr. Hugo Olierook<\/a>\u00a0from Curtin\u2019s School of Earth and Planetary Sciences, one of the study\u2019s authors.<\/p>\n<p class=\"wp-block-paragraph\">\u201cUnlike most volcanic\u00a0hotspots\u00a0that remain stationary in the mantle and create volcanic trails as tectonic plates drift over them, this study found that the hotspot responsible for the Ninetyeast Ridge moved by several hundred kilometres within the mantle over time,\u201d Olierook said.<\/p>\n<p class=\"wp-block-paragraph\">\u201cThis kind of hotspot movement is thought to be common but is hard to prove and has only previously been demonstrated for a few hotspots in the <a href=\"https:\/\/www.zmescience.com\/science\/oceanography\/a-600-year-old-coral-shows-us-how-the-pacific-ocean-has-changed-since-1370\/\" data-wpil-monitor-id=\"1199\" rel=\"nofollow noopener\" target=\"_blank\">Pacific Ocean<\/a>, making this the first documented case in the Indian Ocean.\u201d<\/p>\n<p>What this means for geology<\/p>\n<p class=\"wp-block-paragraph\">The dynamic behavior of the Kerguelen hotspot carries significant implications for reconstructing Earth\u2019s tectonic history. If hotspots are mobile, they cannot serve as fixed reference points for tracking plate movements. This necessitates a reevaluation of global plate motion models, particularly those relying on hotspot tracks.<\/p>\n<p class=\"wp-block-paragraph\">Moreover, the study highlights the influence of regional mantle convection over large-scale mantle processes. Similar mobility patterns observed in Pacific hotspots, like those forming the Hawaiian Islands, reinforce the idea that hotspot motion is shaped by localized mantle dynamics rather than global mantle flow.<\/p>\n<p class=\"wp-block-paragraph\">This doesn\u2019t mean anything major.  It\u2019s not like we need to rewrite the geology books, but it\u2019s a potential improvement to our existing models.<\/p>\n<p class=\"wp-block-paragraph\">\u201cFor years, rough age estimates of the Ninetyeast Ridge have been used to construct models of how Earth\u2019s tectonic plates moved and reconfigured\u201d, says co-author\u00a0<a href=\"https:\/\/staffportal.curtin.edu.au\/staff\/profile\/view\/fred-jourdan-5dcc8042\/\" rel=\"nofollow noopener\" target=\"_blank\">Professor Fred Jourdan<\/a>, from Curtin\u2019s School of Earth and Planetary Sciences and the John de Laeter Centre. \u201cBy using high-precision dating we can refine these models significantly, leading to better insights into ancient continental movements.\u201d<\/p>\n<p class=\"wp-block-paragraph\">Other hotspots may reveal similar features.<\/p>\n<p class=\"wp-block-paragraph\">There is another reason the ridge matters today: it is also a climate archive. Sediments drilled from the crest of the ridge, including at IODP Site U1443, preserve clues about the Indian monsoon, ocean circulation, salinity, sea level, and the delivery of material from surrounding landmasses into the Bay of Bengal. Because the site has stayed near the equator for tens of millions of years and is perched on the ridge rather than buried deep under Bengal Fan sediments, it offers scientists a relatively clean window into past ocean and climate change.<\/p>\n<p class=\"wp-block-paragraph\">The study <a href=\"https:\/\/www.nature.com\/articles\/s41467-024-54092-6\" rel=\"nofollow noopener\" target=\"_blank\">was published<\/a> in Nature Communications.<\/p>\n<p class=\"wp-block-paragraph\">The article was originally published in March 25, 2025, and has been edited to include additional information. <\/p>\n","protected":false},"excerpt":{"rendered":"Ninetyeast Ridge, the long, pale-blue line slicing through the Indian Ocean near 90 degrees east, is the largest&hellip;\n","protected":false},"author":2,"featured_media":540568,"comment_status":"","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[7],"tags":[229704,229705,61,229706,60,229707,229708,229709,229710,127207,82,229711,229712],"class_list":["post-540567","post","type-post","status-publish","format-standard","has-post-thumbnail","category-science","tag-geochronology","tag-hotspots","tag-ie","tag-indian-ocean-geology","tag-ireland","tag-kerguelen-hotspot","tag-mantle-dynamics","tag-mantle-plumes","tag-ninetyeast-ridge","tag-plate-tectonics","tag-science","tag-seismic-tomography","tag-volcanic-ridges"],"_links":{"self":[{"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/posts\/540567","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/comments?post=540567"}],"version-history":[{"count":0,"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/posts\/540567\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/media\/540568"}],"wp:attachment":[{"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/media?parent=540567"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/categories?post=540567"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/tags?post=540567"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}