{"id":1178299,"date":"2026-08-31T02:54:23","date_gmt":"2026-08-31T02:54:23","guid":{"rendered":"https:\/\/www.europesays.com\/uk\/1178299\/"},"modified":"2026-08-31T02:54:23","modified_gmt":"2026-08-31T02:54:23","slug":"hundreds-of-hidden-earthquakes-found-at-antarcticas-doomsday-glacier","status":"publish","type":"post","link":"https:\/\/www.europesays.com\/uk\/1178299\/","title":{"rendered":"Hundreds of hidden earthquakes found at Antarctica\u2019s Doomsday Glacier"},"content":{"rendered":"<p id=\"first\">Glacial earthquakes are a special type of earthquake generated in  cold, icy regions. First discovered in the northern hemisphere <a href=\"https:\/\/doi.org\/10.1126\/science.1088057\" rel=\"nofollow noopener\" target=\"_blank\">more than 20 years ago<\/a>, these quakes occur when huge chunks of ice fall from glaciers into the sea.<\/p>\n<p>Until now, only a very few have been found in the Antarctic. In a\u00a0<a href=\"https:\/\/doi.org\/10.1029\/2025GL118885\" rel=\"nofollow noopener\" target=\"_blank\">study<\/a>  published in Geophysical Research Letters, I present evidence for  hundreds of these quakes in Antarctica between 2010 and 2023, mostly at  the ocean end of the Thwaites Glacier \u2013 the so-called Doomsday Glacier  that could send sea levels rising rapidly if it were to collapse.<\/p>\n<p>A recent discovery<\/p>\n<p>A glacial earthquake is created when tall, thin icebergs fall off the end of a glacier into the ocean.<\/p>\n<p>When these icebergs <a href=\"https:\/\/doi.org\/10.1126\/science.aab0460\" rel=\"nofollow noopener\" target=\"_blank\">capsize<\/a>,  they clash violently with the \u201cmother\u201d glacier. The clash generates  strong mechanical ground vibrations, or seismic waves, that propagate  thousands of kilometres from the origin.<\/p>\n<p>What makes glacial earthquakes unique is that they do not generate  any high-frequency seismic waves. These waves play a vital role in the  detection and location of typical seismic sources, such as earthquakes,  volcanoes and nuclear explosions.<\/p>\n<p>Due to this difference, glacial earthquakes were only discovered relatively recently, despite other seismic sources having been <a href=\"https:\/\/www.usgs.gov\/programs\/earthquake-hazards\/earthquakes\" rel=\"nofollow noopener\" target=\"_blank\">documented routinely<\/a> for several decades.<\/p>\n<p>Varying with the seasons<\/p>\n<p>Most glacial earthquakes detected so far have been located near the <a href=\"https:\/\/doi.org\/10.1146\/annurev-earth-040809-152414\" rel=\"nofollow noopener\" target=\"_blank\">ends of glaciers in Greenland<\/a>, the largest ice cap in the northern hemisphere.<\/p>\n<p>The Greenland glacial earthquakes are relatively large in magnitude. The largest ones are similar in size to those caused by <a href=\"https:\/\/earthquake.usgs.gov\/earthquakes\/eventpage\/us10006n8a\/executive#executive\" rel=\"nofollow noopener\" target=\"_blank\">nuclear tests<\/a>  conducted by North Korea in the past two decades. As such, they have  been detected by a high-quality, continuously operating seismic  monitoring network worldwide.<\/p>\n<p>The Greenland events <a href=\"https:\/\/doi.org\/10.1126\/science.1122112\" rel=\"nofollow noopener\" target=\"_blank\">vary with the seasons<\/a>, occurring more often in late summer. They have also <a href=\"https:\/\/doi.org\/10.1017\/jog.2017.78\" rel=\"nofollow noopener\" target=\"_blank\">become more common<\/a> in recent decades. The signs may be associated with a faster rate of global warming in the polar regions.<\/p>\n<p>Elusive evidence<\/p>\n<p>Although Antarctica is the largest ice sheet on Earth, direct  evidence of glacial earthquakes caused by capsizing icebergs there has  been elusive. Most previous attempts to detect Antarctic glacial  earthquakes used the worldwide network of seismic detectors.<\/p>\n<p>However, if Antarctic glacial earthquakes are of much lower magnitude  than those in Greenland, the global network may not detect them.<\/p>\n<p>In my new study, I used seismic stations in Antarctica itself to look  for signs of these quakes. My search turned up more than 360 glacier  seismic events, most of which are not yet included in any earthquake  catalogue.<\/p>\n<p>The events I detected were in two clusters, near Thwaites and Pine Island glaciers. These glaciers have been the <a href=\"https:\/\/doi.org\/10.1126\/sciadv.abg3080\" rel=\"nofollow noopener\" target=\"_blank\">largest sources<\/a> of sea-level rise from Antarctica.<\/p>\n<p>Earthquakes at the Doomsday Glacier<\/p>\n<p>Thwaites Glacier is sometimes known as the <a href=\"https:\/\/www.science.org\/content\/article\/doomsday-may-be-delayed-antarctica-s-most-vulnerable-glacier\" rel=\"nofollow noopener\" target=\"_blank\">Doomsday Glacier<\/a>.  If it were to collapse completely it would raise global sea levels by 3  metres, and it also has the potential to fall apart rapidly.<\/p>\n<p>About two-thirds of the events I detected \u2013 245 out of 362 \u2013 were  located near the marine end of Thwaites. Most of these events are likely  glacial earthquakes due to capsizing icebergs.<\/p>\n<p>The strongest driver of such events does not appear to be the annual oscillation of warm air temperatures that drives the <a href=\"https:\/\/doi.org\/10.1029\/2009JF001405\" rel=\"nofollow noopener\" target=\"_blank\">seasonal behaviour<\/a> of Greenland glacier earthquakes.<\/p>\n<p>Instead, the most prolific period of glacial earthquakes at Thwaites,  between 2018 and 2020, coincides with a period of accelerated flow of  the glacier\u2019s ice tongue towards the sea. The ice-tongue speed-up period  was independently confirmed by <a href=\"https:\/\/doi.org\/10.1038\/s41561-022-01097-9\" rel=\"nofollow noopener\" target=\"_blank\">satellite<\/a> observations.<\/p>\n<p>This speed-up could have been caused by ocean conditions, the effect of which is not yet well understood.<\/p>\n<p>The findings suggest the short-term scale impact of ocean states on  the stability of marine-terminating glaciers. This is worth further  exploration to assess the potential <a href=\"https:\/\/doi.org\/10.1126\/science.adt9619\" rel=\"nofollow noopener\" target=\"_blank\">contribution<\/a> of the glacier to future sea-level rise.<\/p>\n<p>The second largest cluster of detections occurred near the Pine  Island Glacier. However, these were consistently located 60\u201380  kilometres from the waterfront, so they are not likely to have been  caused by capsizing icebergs.<\/p>\n<p>These events remain puzzling and require follow-up research.<\/p>\n<p>What\u2019s next for Antarctic glacial earthquake research<\/p>\n<p>The detection of glacial earthquakes associated with iceberg calving  at Thwaites Glacier could help answer several important research  questions. These include a fundamental question about the <a href=\"https:\/\/doi.org\/10.1126\/sciadv.adr5921\" rel=\"nofollow noopener\" target=\"_blank\">potential instability<\/a> of the Thwaites Glacier due to the interaction of the ocean, ice and solid ground near where it meets the sea.<\/p>\n<p>Better understanding may hold the key to resolving the current large <a href=\"https:\/\/doi.org\/10.1126\/science.adt9619\" rel=\"nofollow noopener\" target=\"_blank\">uncertainty<\/a> in the projected sea-level rise over the next couple of centuries.<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.europesays.com\/uk\/wp-content\/uploads\/2026\/01\/1767829751_657_count.gif\" alt=\"The Conversation\" width=\"1\" height=\"1\" style=\"border: none !important; box-shadow: none !important; margin: 0 !important; max-height: 1px !important; max-width: 1px !important; min-height: 1px !important; min-width: 1px !important; opacity: 0 !important; outline: none !important; padding: 0 !important\" referrerpolicy=\"no-referrer-when-downgrade\"\/><\/p>\n","protected":false},"excerpt":{"rendered":"Glacial earthquakes are a special type of earthquake generated in cold, icy regions. First discovered in the northern&hellip;\n","protected":false},"author":2,"featured_media":1178300,"comment_status":"","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"footnotes":"","_share_on_mastodon":"0"},"categories":[3843],"tags":[728,319335,70,16,15],"class_list":["post-1178299","post","type-post","status-publish","format-standard","has-post-thumbnail","category-environment","tag-environment","tag-global-warming-earthquakes-air-quality-environmental-issues-natural-disasters-environmental-science-pollution-air-pollution","tag-science","tag-uk","tag-united-kingdom"],"share_on_mastodon":{"url":"https:\/\/pubeurope.com\/@uk\/117187868520407054","error":""},"_links":{"self":[{"href":"https:\/\/www.europesays.com\/uk\/wp-json\/wp\/v2\/posts\/1178299","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.europesays.com\/uk\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.europesays.com\/uk\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.europesays.com\/uk\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.europesays.com\/uk\/wp-json\/wp\/v2\/comments?post=1178299"}],"version-history":[{"count":0,"href":"https:\/\/www.europesays.com\/uk\/wp-json\/wp\/v2\/posts\/1178299\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.europesays.com\/uk\/wp-json\/wp\/v2\/media\/1178300"}],"wp:attachment":[{"href":"https:\/\/www.europesays.com\/uk\/wp-json\/wp\/v2\/media?parent=1178299"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.europesays.com\/uk\/wp-json\/wp\/v2\/categories?post=1178299"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.europesays.com\/uk\/wp-json\/wp\/v2\/tags?post=1178299"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}