{"id":1118,"date":"2026-07-31T17:14:22","date_gmt":"2026-07-31T17:14:22","guid":{"rendered":"https:\/\/cn-seo.org\/?p=1118"},"modified":"2026-07-31T17:14:22","modified_gmt":"2026-07-31T17:14:22","slug":"the-heezen-tharp-world-ocean-floor-map-state-of-the-planet","status":"publish","type":"post","link":"https:\/\/cn-seo.org\/?p=1118","title":{"rendered":"The Heezen\u2013Tharp World Ocean Floor Map \u2013 State of the Planet"},"content":{"rendered":"<p> <br \/>\n<\/p>\n<p style=\"font-size:clamp(0.901rem, 0.901rem + ((1vw - 0.2rem) * 0.816), 1.35rem);\">Though nearly three-quarters of Earth\u2019s surface lies beneath the oceans, the seafloor remained largely unexamined until the mid-20th century. Published in 1977, the <em>World Ocean Floor<\/em> map presented a sweeping panorama that revealed the underwater landscape in remarkable detail. Today, it is regarded as a landmark in oceanography and scientific cartography.<\/p>\n<p>This interactive explores key regions of the ocean floor and explains how decades of scientific observations were transformed into a vivid portrait of Earth\u2019s hidden landscape. Along the way, you\u2019ll learn how the map was created, meet the people behind it, and discover the marine geology and ocean science that continue to shape our understanding of the planet.<\/p>\n<div id=\"\">\n<summary><strong>View Text<\/strong><\/summary>\n<div class=\"wp-block-group has-global-padding is-layout-constrained wp-block-group-is-layout-constrained\">\n<h2 class=\"wp-block-heading\">The Heezen\u2013Tharp <em>World Ocean Floor<\/em> Map<\/h2>\n<p class=\"wp-block-paragraph\">Before the mid-20th century, much of the ocean floor was still a mystery. Though scientists had measured depths along ship routes and identified some major underwater features, the seafloor was still widely conceived of as a relatively flat, featureless plain.<\/p>\n<p class=\"wp-block-paragraph\"><a href=\"https:\/\/news.climate.columbia.edu\/2020\/07\/27\/marie-tharp-maps-legacy\/\">Marie Tharp<\/a> helped change that. Working with Columbia University geologist Bruce C. Heezen, Tharp transformed decades of ocean-depth measurements into a new visual language for the seafloor. Their maps revealed a vast underwater landscape: rift valleys, volcanic ridges, deep trenches and mountain chains stretching across entire ocean basins.<\/p>\n<p class=\"wp-block-paragraph\">The culmination of their work was the <em>World Ocean Floor<\/em> map, published in 1977. The map combined scientific data, geological interpretation and dramatic artistry to show the ocean floor as a continuous global landscape. Through vertical exaggeration and painterly detail, it made an invisible world understandable to scientists and the public alike.<\/p>\n<p class=\"wp-block-paragraph\">The map became one of the most influential scientific images of the 20th century, and it helped people see the ocean floor not as a static surface, but as part of a dynamic Earth.<\/p>\n<\/div>\n<div class=\"wp-block-group has-global-padding is-layout-constrained wp-block-group-is-layout-constrained\">\n<h2 class=\"wp-block-heading\"><strong>Turning Data Into Landscapes: How Marie Tharp Mapped the Ocean<\/strong><\/h2>\n<p class=\"wp-block-paragraph\">Marie Tharp came to Columbia\u2019s Lamont Geological Observatory (now the <a href=\"https:\/\/lamont.columbia.edu\/\">Lamont-Doherty Earth Observatory<\/a>, part of the Columbia Climate School) in 1948 with training in geology, mathematics and drafting. At Lamont, she began working with Bruce Heezen, forming a scientific partnership that would last for decades. Because women were generally not allowed on oceanographic research cruises at the time, Heezen collected data at sea while Tharp analyzed and mapped it back in the lab.<\/p>\n<figure class=\"wp-block-image size-medium\"><picture class=\"sotp-avif-images\"><source srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Marie-Tharp-at-work-1961-325x258.avif 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Marie-Tharp-at-work-1961-650x516.avif 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Marie-Tharp-at-work-1961.avif 750w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\" type=\"image\/avif\"\/><img decoding=\"async\" width=\"650\" height=\"516\" fetchpriority=\"low\" src=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Marie-Tharp-at-work-1961-650x516.jpg\" alt=\"Marie Tharp at work on a map at Lamont-Doherty with scientific charts and a globe nearby, circa 1961.\" class=\"wp-image-127475 sotp-avif-images\" srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Marie-Tharp-at-work-1961-650x516.jpg 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Marie-Tharp-at-work-1961-325x258.jpg 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Marie-Tharp-at-work-1961.jpg 750w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\"\/><\/picture><\/figure>\n<p class=\"wp-block-paragraph\">The raw material for Tharp\u2019s maps came from echo sounding: instruments that measured ocean depth by sending sound pulses down to the seafloor and recording how long they took to return. These measurements arrived as long rolls of paper showing depth profiles along ship tracks. Tharp plotted the ship tracks, converted the soundings into cross sections, and used them to sketch the shape of the seafloor along each route.<\/p>\n<p class=\"wp-block-paragraph\">But the data were incomplete. Research ships crossed the oceans along widely spaced paths, leaving large gaps between measured areas. Tharp used her geological training to interpret the patterns she saw, extending ridges, valleys, plains and fractures between the sounding lines.<\/p>\n<figure data-wp-context=\"{\" imageid=\"\" data-wp-interactive=\"core\/image\" data-wp-key=\"6a6cd2c1dffa8\" class=\"wp-block-image size-medium wp-lightbox-container\"><picture class=\"sotp-avif-images\"><source srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/figure-1-physiographic-diagram-325x655.avif 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/figure-1-physiographic-diagram-650x1309.avif 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/figure-1-physiographic-diagram-768x1547.avif 768w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/figure-1-physiographic-diagram.avif 902w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\" type=\"image\/avif\"\/><img decoding=\"async\" width=\"650\" height=\"1309\" fetchpriority=\"low\" data-wp-class--hide=\"state.isContentHidden\" data-wp-class--show=\"state.isContentVisible\" data-wp-init=\"callbacks.setButtonStyles\" data-wp-on--click=\"actions.showLightbox\" data-wp-on--load=\"callbacks.setButtonStyles\" data-wp-on--pointerdown=\"actions.preloadImage\" data-wp-on--pointerenter=\"actions.preloadImageWithDelay\" data-wp-on--pointerleave=\"actions.cancelPreload\" data-wp-on-window--resize=\"callbacks.setButtonStyles\" src=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/figure-1-physiographic-diagram-650x1309.png\" alt=\"Scientific line chars showing ship tracks, sounding depths, and interpretive sketches of them as landscapes.\" class=\"wp-image-127476 sotp-avif-images\" srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/figure-1-physiographic-diagram-650x1309.png 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/figure-1-physiographic-diagram-768x1547.png 768w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/figure-1-physiographic-diagram-325x655.png 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/figure-1-physiographic-diagram.png 902w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\"\/><\/picture><button class=\"lightbox-trigger\" type=\"button\" aria-haspopup=\"dialog\" data-wp-bind--aria-label=\"state.thisImage.triggerButtonAriaLabel\" data-wp-init=\"callbacks.initTriggerButton\" data-wp-on--click=\"actions.showLightbox\" data-wp-style--right=\"state.thisImage.buttonRight\" data-wp-style--top=\"state.thisImage.buttonTop\"><br \/>\n\t\t\t<svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" width=\"12\" height=\"12\" fill=\"none\" viewbox=\"0 0 12 12\">\n\t\t\t\t<path fill=\"#fff\" d=\"M2 0a2 2 0 0 0-2 2v2h1.5V2a.5.5 0 0 1 .5-.5h2V0H2Zm2 10.5H2a.5.5 0 0 1-.5-.5V8H0v2a2 2 0 0 0 2 2h2v-1.5ZM8 12v-1.5h2a.5.5 0 0 0 .5-.5V8H12v2a2 2 0 0 1-2 2H8Zm2-12a2 2 0 0 1 2 2v2h-1.5V2a.5.5 0 0 0-.5-.5H8V0h2Z\"\/>\n\t\t\t<\/svg><br \/>\n\t\t<\/button><figcaption class=\"wp-element-caption\">\u201cMethod of preparation of physiographic diagram\u201d: (a) Positions of sounding lines (A, B) are plotted on chart; (b) Soundings are plotted as profiles (A, B) at 40:1 vertical exaggeration; (c) Features shown on profiles (A, B) are sketched on chart along tracks; (d) After all available sounding profiles are sketched the remaining unsounded areas are filled in by extrapolating and interpolating trends observed in a succession of profiles. From \u201c<a href=\"https:\/\/pubs.geoscienceworld.org\/gsa\/books\/book\/701\/chapter\/3808684\/The-Floors-of-the-OceansI-The-North-Atlantic\">The Floors of the Oceans<\/a>\u201c, 1959.<\/figcaption><\/figure>\n<p class=\"wp-block-paragraph\">This map view shows the approximate area detailed in the figure above after interpretation.<\/p>\n<p class=\"wp-block-paragraph\">Tharp chose to present this work as <strong>physiographic diagrams<\/strong>\u2014shaded, landscape-like views of underwater terrain. The style made the seafloor easier to understand than a technical contour map. It also offered a practical advantage during the Cold War: detailed bathymetric contour maps were restricted, while physiographic maps could communicate the shape of the ocean floor without publishing classified measurements.<\/p>\n<p class=\"wp-block-paragraph\">The result was both scientific interpretation and visual storytelling: a way to turn scattered measurements into a coherent image of Earth\u2019s hidden surface.<\/p>\n<p class=\"wp-block-paragraph\">\u201cI worked in the background for most of my career as a scientist, but I have absolutely no resentments,\u201d Tharp said later in life. \u201cI thought I was lucky to have a job that was so interesting.\u201d<\/p>\n<\/div>\n<div class=\"wp-block-group has-global-padding is-layout-constrained wp-block-group-is-layout-constrained\">\n<h2 class=\"wp-block-heading\"><strong>Science Meets Art: Heinrich Berann<\/strong><\/h2>\n<p class=\"wp-block-paragraph\">While Tharp and Heezen supplied the scientific foundation of the <em>World Ocean Floor<\/em> map, Austrian painter and cartographer Heinrich C. Berann was essential in shaping its visual style.<\/p>\n<blockquote class=\"wp-block-quote is-layout-flow wp-block-quote-is-layout-flow\">\n<p class=\"has-medium-font-size wp-block-paragraph\">\u201cNational Geographic had received a letter from a little girl in Austria who wrote, \u2018I\u2019ve been looking at your maps and my father can paint better than you can.\u2019 Intrigued, National Geographic editors sent their chief topographer to Innsbruck, Austria, to meet the girl\u2019s artist father, Heinrich Berann.\u201d \u2014Marie Tharp<\/p>\n<\/blockquote>\n<figure data-wp-context=\"{\" imageid=\"\" data-wp-interactive=\"core\/image\" data-wp-key=\"6a6cd2c1e056f\" class=\"wp-block-image size-medium wp-lightbox-container\"><picture class=\"sotp-avif-images\"><source srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Heinrich-Berann-NPS-Panorama-Yosemite-2400-325x216.avif 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Heinrich-Berann-NPS-Panorama-Yosemite-2400-650x433.avif 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Heinrich-Berann-NPS-Panorama-Yosemite-2400-768x511.avif 768w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Heinrich-Berann-NPS-Panorama-Yosemite-2400-1300x866.avif 1300w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Heinrich-Berann-NPS-Panorama-Yosemite-2400.avif 2400w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\" type=\"image\/avif\"\/><img decoding=\"async\" width=\"650\" height=\"433\" fetchpriority=\"low\" data-wp-class--hide=\"state.isContentHidden\" data-wp-class--show=\"state.isContentVisible\" data-wp-init=\"callbacks.setButtonStyles\" data-wp-on--click=\"actions.showLightbox\" data-wp-on--load=\"callbacks.setButtonStyles\" data-wp-on--pointerdown=\"actions.preloadImage\" data-wp-on--pointerenter=\"actions.preloadImageWithDelay\" data-wp-on--pointerleave=\"actions.cancelPreload\" data-wp-on-window--resize=\"callbacks.setButtonStyles\" src=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Heinrich-Berann-NPS-Panorama-Yosemite-2400-650x433.jpg\" alt=\"Panoramic painting of Yosemite National Park from a bird's eye view, showing snowy peaks, lakes, and green valleys.\" class=\"wp-image-127479 sotp-avif-images\" srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Heinrich-Berann-NPS-Panorama-Yosemite-2400-650x433.jpg 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Heinrich-Berann-NPS-Panorama-Yosemite-2400-1300x866.jpg 1300w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Heinrich-Berann-NPS-Panorama-Yosemite-2400-768x511.jpg 768w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Heinrich-Berann-NPS-Panorama-Yosemite-2400-325x216.jpg 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Heinrich-Berann-NPS-Panorama-Yosemite-2400.jpg 2400w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\"\/><\/picture><button class=\"lightbox-trigger\" type=\"button\" aria-haspopup=\"dialog\" data-wp-bind--aria-label=\"state.thisImage.triggerButtonAriaLabel\" data-wp-init=\"callbacks.initTriggerButton\" data-wp-on--click=\"actions.showLightbox\" data-wp-style--right=\"state.thisImage.buttonRight\" data-wp-style--top=\"state.thisImage.buttonTop\"><br \/>\n\t\t\t<svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" width=\"12\" height=\"12\" fill=\"none\" viewbox=\"0 0 12 12\">\n\t\t\t\t<path fill=\"#fff\" d=\"M2 0a2 2 0 0 0-2 2v2h1.5V2a.5.5 0 0 1 .5-.5h2V0H2Zm2 10.5H2a.5.5 0 0 1-.5-.5V8H0v2a2 2 0 0 0 2 2h2v-1.5ZM8 12v-1.5h2a.5.5 0 0 0 .5-.5V8H12v2a2 2 0 0 1-2 2H8Zm2-12a2 2 0 0 1 2 2v2h-1.5V2a.5.5 0 0 0-.5-.5H8V0h2Z\"\/>\n\t\t\t<\/svg><br \/>\n\t\t<\/button><figcaption class=\"wp-element-caption\">Panorama of Yosemite National Park, 1989<\/figcaption><\/figure>\n<p class=\"wp-block-paragraph\">Berann was internationally known for panoramic cartography: painted maps that combined geographic information with the drama, depth and atmosphere of landscape painting. Before the <em>World Ocean Floor<\/em> map, he had produced alpine panoramas, Olympic maps and other works for <em>National Geographic<\/em>; his collaboration with Tharp and Heezen began with ocean-basin maps before culminating in the 1977 global panorama.<\/p>\n<p class=\"wp-block-paragraph\">For the <em>World Ocean Floor<\/em> map, Berann faced an unusual challenge: How do you make a hidden terrain visible, legible and beautiful, while still respecting the underlying science?<\/p>\n<p class=\"wp-block-paragraph\">His solution was to treat the seafloor as a landscape. Using perspective, lighting, shadow, color and vertical exaggeration, Berann depicted steep mountain chains rising from the ocean depths, trenches descending into darkness, and ridges and valleys as interconnected systems. These techniques helped viewers understand complex <strong>bathymetry<\/strong>\u2014the depths and shapes of underwater terrain\u2014at a glance.<\/p>\n<p class=\"wp-block-paragraph\">Berann\u2019s technique ensured that the <em>World Ocean Floor<\/em> map balanced scientific accuracy with clarity, and his artistry helped make it one of the most memorable scientific visualizations of the twentieth century.<\/p>\n<\/div>\n<div class=\"wp-block-group has-global-padding is-layout-constrained wp-block-group-is-layout-constrained\">\n<h2 class=\"wp-block-heading\"><strong>A Rift Through the Atlantic: A Discovery That Changed Geology<\/strong><\/h2>\n<p class=\"wp-block-paragraph\">At the center of the Atlantic Ocean, the <em>World Ocean Floor<\/em> map shows a vast underwater mountain chain: the Mid-Atlantic Ridge. Running along its crest is one of Tharp\u2019s most important discoveries: a narrow rift valley that revealed the seafloor was far more active than many scientists had imagined.<\/p>\n<p class=\"wp-block-paragraph\">Tharp first recognized the rift while plotting echo-sounding profiles across the Atlantic in the 1950s. The profiles showed that the ridge was not simply a broad underwater mountain range\u2014it was split by a long valley running down its center. This was a striking clue that the ocean floor might be pulling apart.<\/p>\n<figure class=\"wp-block-image size-medium\"><picture class=\"sotp-avif-images\"><source srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Separate-whoi-325x183.avif 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Separate-whoi-650x366.avif 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Separate-whoi-768x432.avif 768w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Separate-whoi.avif 1046w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\" type=\"image\/avif\"\/><img decoding=\"async\" width=\"650\" height=\"366\" fetchpriority=\"low\" src=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Separate-whoi-650x366.png\" alt=\"A color rendering of seafloor spreading, showing magma, tectonic plates, and a mid-ocean ridge.\" class=\"wp-image-127482 sotp-avif-images\" srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Separate-whoi-650x366.png 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Separate-whoi-768x432.png 768w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Separate-whoi-325x183.png 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Separate-whoi.png 1046w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\"\/><\/picture><figcaption class=\"wp-element-caption\"><a href=\"https:\/\/divediscover.whoi.edu\/plate-tectonics\/plate-movements\/\">Woods Hole Oceanographic Institution<\/a><\/figcaption><\/figure>\n<p class=\"wp-block-paragraph\">The evidence became even stronger when Tharp and Heezen compared their maps with earthquake data. Although earthquake locations were imprecise, Tharp later recalled that when they overlaid the datasets, the earthquake epicenters \u201clined up within the valley.\u201d The rift was not just a landform; it was a zone of geologic activity.<\/p>\n<figure data-wp-context=\"{\" imageid=\"\" data-wp-interactive=\"core\/image\" data-wp-key=\"6a6cd2c1e0b08\" class=\"wp-block-image size-medium wp-lightbox-container\"><picture class=\"sotp-avif-images\"><source srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seismicity_of_the_earth_1960-1980_2400-325x179.avif 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seismicity_of_the_earth_1960-1980_2400-650x357.avif 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seismicity_of_the_earth_1960-1980_2400-768x422.avif 768w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seismicity_of_the_earth_1960-1980_2400-1300x714.avif 1300w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seismicity_of_the_earth_1960-1980_2400.avif 2400w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\" type=\"image\/avif\"\/><img decoding=\"async\" width=\"650\" height=\"357\" fetchpriority=\"low\" data-wp-class--hide=\"state.isContentHidden\" data-wp-class--show=\"state.isContentVisible\" data-wp-init=\"callbacks.setButtonStyles\" data-wp-on--click=\"actions.showLightbox\" data-wp-on--load=\"callbacks.setButtonStyles\" data-wp-on--pointerdown=\"actions.preloadImage\" data-wp-on--pointerenter=\"actions.preloadImageWithDelay\" data-wp-on--pointerleave=\"actions.cancelPreload\" data-wp-on-window--resize=\"callbacks.setButtonStyles\" src=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seismicity_of_the_earth_1960-1980_2400-650x357.jpg\" alt=\"A version of the World Ocean Floor map with earthquakes plotted in red, which trace mid-ocean ridges and tectonic plate boundaries.\" class=\"wp-image-127484 sotp-avif-images\" srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seismicity_of_the_earth_1960-1980_2400-650x357.jpg 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seismicity_of_the_earth_1960-1980_2400-1300x714.jpg 1300w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seismicity_of_the_earth_1960-1980_2400-768x422.jpg 768w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seismicity_of_the_earth_1960-1980_2400-325x179.jpg 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seismicity_of_the_earth_1960-1980_2400.jpg 2400w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\"\/><\/picture><button class=\"lightbox-trigger\" type=\"button\" aria-haspopup=\"dialog\" data-wp-bind--aria-label=\"state.thisImage.triggerButtonAriaLabel\" data-wp-init=\"callbacks.initTriggerButton\" data-wp-on--click=\"actions.showLightbox\" data-wp-style--right=\"state.thisImage.buttonRight\" data-wp-style--top=\"state.thisImage.buttonTop\"><br \/>\n\t\t\t<svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" width=\"12\" height=\"12\" fill=\"none\" viewbox=\"0 0 12 12\">\n\t\t\t\t<path fill=\"#fff\" d=\"M2 0a2 2 0 0 0-2 2v2h1.5V2a.5.5 0 0 1 .5-.5h2V0H2Zm2 10.5H2a.5.5 0 0 1-.5-.5V8H0v2a2 2 0 0 0 2 2h2v-1.5ZM8 12v-1.5h2a.5.5 0 0 0 .5-.5V8H12v2a2 2 0 0 1-2 2H8Zm2-12a2 2 0 0 1 2 2v2h-1.5V2a.5.5 0 0 0-.5-.5H8V0h2Z\"\/>\n\t\t\t<\/svg><br \/>\n\t\t<\/button><figcaption class=\"wp-element-caption\">\u201cSeismicity of the earth, 1960-1980\u201d, Rebecca M. Espinosa and Marie Tharp, circa 1982<\/figcaption><\/figure>\n<p class=\"wp-block-paragraph\">The idea was controversial. The theory of continental drift was still widely doubted, and many scientists viewed the ocean basins as old and relatively stable. Tharp\u2019s interpretation suggested something very different: that new oceanic crust could be forming along the ridge as the seafloor spread apart.<\/p>\n<p class=\"wp-block-paragraph\">Reactions ranged from excitement to skepticism. After Heezen presented the expanding mid-ocean rift system at Princeton in 1957, geologist Harry Hess reportedly told him, \u201cYoung man, you have shaken the foundations of geology!\u201d<\/p>\n<\/div>\n<div class=\"wp-block-group has-global-padding is-layout-constrained wp-block-group-is-layout-constrained\">\n<h2 class=\"wp-block-heading\"><strong>Earth in Motion: Fracture Zones and Transform Faults<\/strong><\/h2>\n<p class=\"wp-block-paragraph\">The Mid-Atlantic Ridge revealed where new ocean crust forms. But another pattern on the <em>World Ocean Floor<\/em> map showed how that crust moves.<\/p>\n<p class=\"wp-block-paragraph\">Look closely at the Atlantic seafloor and you can see long, nearly straight lines cutting across the ocean basin. These are <strong>fracture zones<\/strong>, or scars in the ocean crust that extend outward from mid-ocean ridges. They mark places where sections of the ridge have been offset from one another as tectonic plates move.<\/p>\n<figure class=\"wp-block-image size-medium\"><picture class=\"sotp-avif-images\"><source srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Slide-Past-325x191.avif 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Slide-Past-650x381.avif 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Slide-Past-768x451.avif 768w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Slide-Past-1300x763.avif 1300w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Slide-Past.avif 1360w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\" type=\"image\/avif\"\/><img decoding=\"async\" width=\"650\" height=\"381\" fetchpriority=\"low\" src=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Slide-Past-650x381.png\" alt=\"Illustration of two tectonic plates sliding in opposite directions.\" class=\"wp-image-127488 sotp-avif-images\" srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Slide-Past-650x381.png 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Slide-Past-1300x763.png 1300w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Slide-Past-768x451.png 768w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Slide-Past-325x191.png 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/Seafloor-Slide-Past.png 1360w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\"\/><\/picture><figcaption class=\"wp-element-caption\"><a href=\"https:\/\/divediscover.whoi.edu\/plate-tectonics\/plate-movements\/\">Woods Hole Oceanographic Institution<\/a><\/figcaption><\/figure>\n<p class=\"wp-block-paragraph\">The active parts of these breaks are called <strong>transform faults<\/strong>. Unlike spreading ridges, where plates move apart, transform faults are places where plates slide past one another. Earthquakes occur along these active faults, making them another important clue that the seafloor is not fixed but in motion.<\/p>\n<p class=\"wp-block-paragraph\">Fracture zones are important because they preserve a record of plate movement over millions of years. As new crust forms at a ridge and moves away, the offset pattern remains written into the seafloor. On Tharp and Heezen\u2019s maps, these long lineations helped show that ocean crust was not deforming randomly; it was moving in broad, rigid plates.<\/p>\n<\/div>\n<div class=\"wp-block-group has-global-padding is-layout-constrained wp-block-group-is-layout-constrained\">\n<h2 class=\"wp-block-heading\"><strong>Subduction: <\/strong>H<strong>ow Ocean Crust Returns to Earth<\/strong><\/h2>\n<p class=\"wp-block-paragraph\"><strong>Trenches<\/strong> are the deepest places in the ocean. They form where one tectonic plate bends downward and sinks beneath another, carrying old, dense oceanic crust back into Earth\u2019s mantle in a process called <strong>subduction.<\/strong> Along the western edge of South America, the Peru\u2013Chile Trench marks the place where the oceanic Nazca Plate is being forced beneath the South American Plate.<\/p>\n<figure class=\"wp-block-image size-medium\"><picture class=\"sotp-avif-images\"><source srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/seafloor-Subduction-whoi-325x195.avif 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/seafloor-Subduction-whoi-650x390.avif 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/seafloor-Subduction-whoi-768x461.avif 768w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/seafloor-Subduction-whoi-1300x780.avif 1300w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/seafloor-Subduction-whoi.avif 1360w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\" type=\"image\/avif\"\/><img decoding=\"async\" width=\"650\" height=\"390\" fetchpriority=\"low\" src=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/seafloor-Subduction-whoi-650x390.png\" alt=\"Cutaway illustration showing a subducting oceanic plate at the edge of a continent.\" class=\"wp-image-127490 sotp-avif-images\" srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/seafloor-Subduction-whoi-650x390.png 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/seafloor-Subduction-whoi-1300x780.png 1300w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/seafloor-Subduction-whoi-768x461.png 768w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/seafloor-Subduction-whoi-325x195.png 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/seafloor-Subduction-whoi.png 1360w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\"\/><\/picture><figcaption class=\"wp-element-caption\"><a href=\"https:\/\/divediscover.whoi.edu\/plate-tectonics\/plate-movements\/\">Woods Hole Oceanographic Institution<\/a><\/figcaption><\/figure>\n<p class=\"wp-block-paragraph\">Subduction zones are among the most geologically active places on Earth. As one plate descends beneath another, it can generate powerful earthquakes. Water and other materials carried downward with the sinking plate help trigger melting in the mantle, feeding volcanoes at the surface. In some places, these volcanoes form mountain chains like the Andes. In others, they form curved island arcs, such as Japan or the Aleutian Islands.<\/p>\n<\/div>\n<div class=\"wp-block-group has-global-padding is-layout-constrained wp-block-group-is-layout-constrained\">\n<h2 class=\"wp-block-heading\"><strong>Putting the Pieces Together: Plate Tectonics<\/strong><\/h2>\n<p class=\"wp-block-paragraph\">By the late 1960s, the features shown on the <em>World Ocean Floor<\/em> map were beginning to fit together into a new understanding of Earth.<\/p>\n<p class=\"wp-block-paragraph\">The planet\u2019s outer shell, or <strong>lithosphere<\/strong>, is divided into large moving plates. These plates do not drift randomly; they interact along boundaries that are visible across the seafloor: ridges, rift valleys, fracture zones and trenches.<\/p>\n<p class=\"wp-block-paragraph\">At mid-ocean ridges, plates move apart and new oceanic crust forms. Along transform faults, plates slide past one another, offsetting ridge segments and leaving long fracture zones across the seafloor. At trenches, old oceanic crust sinks back into Earth\u2019s interior through subduction. Volcanoes and earthquakes mark many of these active boundaries.<\/p>\n<figure data-wp-context=\"{\" imageid=\"\" data-wp-interactive=\"core\/image\" data-wp-key=\"6a6cd2c1e132b\" class=\"wp-block-image size-medium wp-lightbox-container\"><img decoding=\"async\" width=\"650\" height=\"330\" fetchpriority=\"low\" data-wp-class--hide=\"state.isContentHidden\" data-wp-class--show=\"state.isContentVisible\" data-wp-init=\"callbacks.setButtonStyles\" data-wp-on--click=\"actions.showLightbox\" data-wp-on--load=\"callbacks.setButtonStyles\" data-wp-on--pointerdown=\"actions.preloadImage\" data-wp-on--pointerenter=\"actions.preloadImageWithDelay\" data-wp-on--pointerleave=\"actions.cancelPreload\" data-wp-on-window--resize=\"callbacks.setButtonStyles\" src=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/tectonic_plates_2022-650x330.webp\" alt=\"An illustration of a world map showing the outlines of Earth's tectonic plates.\" class=\"wp-image-127492\" srcset=\"https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/tectonic_plates_2022-650x330.webp 650w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/tectonic_plates_2022-1300x660.webp 1300w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/tectonic_plates_2022-768x390.webp 768w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/tectonic_plates_2022-325x165.webp 325w, https:\/\/media.news.climate.columbia.edu\/wp-content\/uploads\/2026\/07\/tectonic_plates_2022-scaled.webp 2400w\" sizes=\"(max-width: 714px) calc(100vw - calc(clamp(1.5rem, 5vw, 2rem) * 2)), 650px\"\/><button class=\"lightbox-trigger\" type=\"button\" aria-haspopup=\"dialog\" data-wp-bind--aria-label=\"state.thisImage.triggerButtonAriaLabel\" data-wp-init=\"callbacks.initTriggerButton\" data-wp-on--click=\"actions.showLightbox\" data-wp-style--right=\"state.thisImage.buttonRight\" data-wp-style--top=\"state.thisImage.buttonTop\"><br \/>\n\t\t\t<svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" width=\"12\" height=\"12\" fill=\"none\" viewbox=\"0 0 12 12\">\n\t\t\t\t<path fill=\"#fff\" d=\"M2 0a2 2 0 0 0-2 2v2h1.5V2a.5.5 0 0 1 .5-.5h2V0H2Zm2 10.5H2a.5.5 0 0 1-.5-.5V8H0v2a2 2 0 0 0 2 2h2v-1.5ZM8 12v-1.5h2a.5.5 0 0 0 .5-.5V8H12v2a2 2 0 0 1-2 2H8Zm2-12a2 2 0 0 1 2 2v2h-1.5V2a.5.5 0 0 0-.5-.5H8V0h2Z\"\/>\n\t\t\t<\/svg><br \/>\n\t\t<\/button><\/figure>\n<p class=\"wp-block-paragraph\">Seen separately, these features might seem like isolated landforms. Seen together, they reveal a dynamic global system.<\/p>\n<p class=\"wp-block-paragraph\">That is part of what made the <em>World Ocean Floor<\/em> map so powerful: it helped reveal that Earth\u2019s surface is not fixed. It is constantly being created, broken, moved and recycled.<\/p>\n<p class=\"wp-block-paragraph\">Plate tectonics became the unifying theory of modern Earth science. It explains why oceans open and close, why continents move, why mountain ranges rise, why earthquakes cluster in certain regions and why volcanoes form where they do.<\/p>\n<\/div>\n<div class=\"wp-block-group has-global-padding is-layout-constrained wp-block-group-is-layout-constrained\">\n<h2 class=\"wp-block-heading\"><strong>Ocean Mapping Today<\/strong><\/h2>\n<p class=\"wp-block-paragraph\">Today, scientists map the seafloor with tools Tharp could only have imagined. Ships equipped with <strong>multibeam sonar<\/strong> send out sound pulses, measuring depth across wide swaths of ocean instead of along a single track. Autonomous underwater vehicles can survey difficult or remote areas in far greater detail. Satellites can detect subtle variations in sea-surface height caused by gravity, helping scientists infer the shape of large underwater features.<\/p>\n<p class=\"wp-block-paragraph\">Even with these advances, it is estimated that only about 28% of the world\u2019s ocean floor has been mapped to modern standards. The <a href=\"https:\/\/news.climate.columbia.edu\/2025\/06\/08\/leveraging-the-power-of-open-source-data-to-map-the-worlds-oceans\/\">Seabed 2030 project<\/a> aims to change that by bringing governments, research institutions, industry and mariners together to create a complete map of the ocean floor by the end of this decade. Better seafloor maps support marine science, hazard assessment, navigation, habitat protection, climate research and our understanding of Earth\u2019s geologic history.<\/p>\n<p class=\"wp-block-paragraph\">Tharp worked with sparse sounding tracks, scientific insight and a gift for seeing patterns in incomplete data. Modern ocean mappers have more powerful tools, but they are still pursuing the same basic goal: to make the hidden surface of our planet visible.<\/p>\n<\/div>\n<\/div>\n\n","protected":false},"excerpt":{"rendered":"<p>Though nearly three-quarters of Earth\u2019s surface lies beneath the oceans, the seafloor remained largely unexamined until the mid-20th century. Published in 1977, the World Ocean Floor map presented a sweeping panorama that revealed the underwater landscape in remarkable detail. Today, it is regarded as a landmark in oceanography and scientific cartography. This interactive explores key&#8230;<\/p>\n","protected":false},"author":1,"featured_media":1119,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[2],"tags":[],"class_list":["post-1118","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-berita"],"_links":{"self":[{"href":"https:\/\/cn-seo.org\/index.php?rest_route=\/wp\/v2\/posts\/1118","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/cn-seo.org\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/cn-seo.org\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/cn-seo.org\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/cn-seo.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=1118"}],"version-history":[{"count":0,"href":"https:\/\/cn-seo.org\/index.php?rest_route=\/wp\/v2\/posts\/1118\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cn-seo.org\/index.php?rest_route=\/wp\/v2\/media\/1119"}],"wp:attachment":[{"href":"https:\/\/cn-seo.org\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=1118"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cn-seo.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=1118"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cn-seo.org\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=1118"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}