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Seafloor sediments reveal how East Antarctic ice temporarily halted its retreat and advanced 40 miles

Attributed to Phys.org. ENC is not independently verifying these facts.

Seafloor sediments reveal how East Antarctic ice temporarily halted its retreat and advanced 40 miles

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Phys.org reports the following. ENC is republishing it as an attributed briefing, not as independently confirmed fact. If this item is false or incomplete, the responsibility sits with Phys.org, which released it. Off the coast of East Antarctica, researchers led by Kiel University (CAU) and the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI), have investigated an exceptionally large sedimentary body embedded in the seafloor of Vincennes Bay: a so-called "grounding-zone wedge"—symmetrical, wedge-shaped, approximately 260 meters (853 feet) high and 65 kilometers (40 miles) long. With a volume of more than 580 cubic kilometers (139 cubic miles), it is the largest known isolated grounding-zone wedge on a glaciated continental shelf to date and constitutes an exceptional archive of East Antarctica's glacial history. Original link: https://phys.org/news/2026-10-seafloor-sediments-reveal-east-antarctic.html

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