{"id":631523,"date":"2026-09-21T15:36:22","date_gmt":"2026-09-21T15:36:22","guid":{"rendered":"https:\/\/www.newsbeep.com\/ie\/631523\/"},"modified":"2026-09-21T15:36:22","modified_gmt":"2026-09-21T15:36:22","slug":"a-quebec-amateur-astronomer-was-scouting-a-campsite-using-satellite-imagery-in-2024-when-he-spotted-a-25-kilometre-ring-around-lake-marsal-and-geologists-who-reached-it-by-floatplane-the-following-ye","status":"publish","type":"post","link":"https:\/\/www.newsbeep.com\/ie\/631523\/","title":{"rendered":"A Quebec amateur astronomer was scouting a campsite using satellite imagery in 2024 when he spotted a 25-kilometre ring around Lake Marsal, and geologists who reached it by floatplane the following year found shatter cones confirming a roughly 390-million-year-old impact structure now provisionally named Uhackatik"},"content":{"rendered":"<p>In 2024, Quebec amateur astronomer Jo\u00ebl Lapointe was <a href=\"https:\/\/science.nasa.gov\/earth\/earth-observatory\/an-accidental-impact-crater-discovery\/\" target=\"_blank\" rel=\"noopener nofollow\">planning a camping trip<\/a> in Quebec\u2019s C\u00f4te-Nord region and scrolling through satellite imagery when a nearly circular pattern of ridges caught his attention, arranged around a body of water called Lake Marsal. The feature was roughly 25 kilometres across, large enough that it should have been an obvious landmark, yet it did not correspond to any catalogued geological structure.<\/p>\n<p>Lapointe was not the first person to notice unusual terrain on a map and wonder about its origin, and most such observations turn out to be nothing. What made this one different is that there was a specific place to send it: a public reporting channel built by a research group that spends its time fielding exactly these kinds of tips.<\/p>\n<p>A screening database built for exactly this kind of tip<\/p>\n<p>Lapointe submitted his find through <a href=\"https:\/\/impact.uwo.ca\/about\/\" target=\"_blank\" rel=\"noopener nofollow\">Impact Earth<\/a>, a project run out of Western University\u2019s Department of Earth Sciences by planetary geologist Gordon Osinski, who also maintains the associated impact-crater database. Osinski has said he receives frequent submissions from members of the public convinced they have spotted a crater, and that the overwhelming majority, as he put it to <a href=\"https:\/\/www.zmescience.com\/science\/geology\/a-campers-google-maps-hunch-revealed-a-390-million-year-old-meteorite-crater\/\" target=\"_blank\" rel=\"noopener nofollow\">ZME Science<\/a>, \u201cturn out not to be the case.\u201d Lapointe\u2019s ring was one of the rare exceptions that survived that first filter and warranted an actual field visit.<\/p>\n<p>Reaching the ring took a floatplane and a long wade through water<\/p>\n<p>The team that eventually confirmed the structure \u2014 four researchers including Osinski and French geophysicist Pierre Rochette \u2014 flew into the site by floatplane in October 2025. According to <a href=\"https:\/\/www.earth.com\/earth-science\/huge-impact-crater-in-quebec-went-unnoticed-for-390-million-years\/\" target=\"_blank\" rel=\"noopener nofollow\">Earth.com\u2019s reporting<\/a>, the aircraft could not get close enough to shore, forcing the researchers to wade through roughly 50 metres of water while carrying their equipment. Osinski, who has led geological expeditions across six continents and to the Arctic, described the trip to <a href=\"https:\/\/www.livescience.com\/planet-earth\/geology\/this-was-one-of-the-most-arduous-expeditions-ive-ever-done-scientists-confirm-that-15-mile-wide-pit-found-on-google-maps-is-ancient-meteor-crater\" target=\"_blank\" rel=\"noopener nofollow\">Live Science<\/a> as \u201cone of the most arduous expeditions I\u2019ve ever done.\u201d<\/p>\n<p>Once on the ground, the terrain matched what satellite images had hinted at from orbit: a ring of raised, structurally deformed rock consistent with a complex impact crater, the kind that develops a central uplift when a large enough object strikes at high speed. Confirming that visual impression required physical evidence collected by hand, from actual outcrops \u2014 something satellite imagery alone cannot provide.<\/p>\n<p>Shatter cones are the evidence that turns a ring into a crater<\/p>\n<p>The rock feature the team was hunting for is called a shatter cone: a branching, cone-shaped fracture pattern etched into rock by the passage of an extremely high-pressure shockwave. Shatter cones do not form from volcanic activity, erosion, glacial scouring or any other ordinary geological process capable of producing a circular landform, which is why geologists treat them as close to definitive. Osinski has called them, in comments reported by Earth.com, \u201cthe only unequivocal evidence of an impact event that you can see in the field with the naked eye.\u201d<\/p>\n<p>\t\t\t\t\t\tWhat changed in the universe since you were born?<\/p>\n<p class=\"sd-universe-entry__trust\">Six sourced measurements. No predictions. No astrology.<\/p>\n<p>Alongside the shatter cones, the team documented cliffs of impact melt rock roughly four kilometres from the structure\u2019s centre. Impact melt forms when the heat and pressure of a collision are intense enough to liquefy the target rock outright, which then cools and recrystallizes into a distinct texture rarely produced any other way, as <a href=\"https:\/\/www.space.com\/astronomy\/earth\/a-massive-crater-was-spotted-on-google-earth-it-could-be-a-scar-from-an-ancient-meteorite-impact\" target=\"_blank\" rel=\"noopener nofollow\">Space.com\u2019s coverage<\/a> of the expedition explains.<\/p>\n<p>Together, the shatter cones and the melt rock are the kind of layered physical evidence that separates a confirmed impact structure from a merely suggestive shape on a map \u2014 a distinction that matters, because ring-like landforms can also arise from volcanic calderas, salt domes or plain erosion, none of which produce shatter cones.<\/p>\n<p>Provisionally named Uhackatik, formal recognition still pending<\/p>\n<p>After consulting the Innu Council of Ekuanitshit, whose traditional territory includes the area, the research team is calling the structure Uhackatik. Laboratory analysis of the collected rock samples places the impact in the Devonian period, roughly 390 million years ago. That figure describes when the impact happened. The crater\u2019s present, softened shape is a separate story: 390 million years of erosion, glaciation and vegetation growth have reduced what was once a sharp-edged crater into the ring of ridges Lapointe noticed on a map.<\/p>\n<p>The team considers the impact origin essentially settled based on the shatter cones and melt rock, but formal recognition remains pending. The researchers <a href=\"https:\/\/www.hou.usra.edu\/meetings\/metsoc2026\/technical_program\/?session_no=751\" target=\"_blank\" rel=\"noopener nofollow\">presented Uhackatik<\/a> at the 88th Annual Meeting of the Meteoritical Society in Frankfurt on 14 August 2026. <a href=\"https:\/\/science.nasa.gov\/earth\/earth-observatory\/an-accidental-impact-crater-discovery\/\" target=\"_blank\" rel=\"noopener nofollow\">NASA reported on 15 September<\/a> that a Meteoritical Society committee was still expected to consider formal recognition when it next meets. At an estimated 25 kilometres across, it would be the largest crater reported anywhere since Greenland\u2019s 31-kilometre Hiawatha structure \u2014 itself an ice-buried, still-debated find from 2018.<\/p>\n<p>Why a hole in the Quebec bush matters for planetary science<\/p>\n<p>Impact cratering is a defining process across the Solar System, not just a footnote in Earth\u2019s geological history. Western University\u2019s Impact Earth project describes it as \u201cone of the most important and fundamental geological process in the Solar System.\u201d Every rocky body has been struck repeatedly since its formation, but the record of those strikes survives very unevenly. According to figures cited by <a href=\"https:\/\/abcnews.com\/International\/amateur-astronomer-discovers-390-million-year-meteorite-impact\/story?id=135016127\" target=\"_blank\" rel=\"noopener nofollow\">ABC News<\/a>, roughly 200 impact craters have been confirmed on Earth in total, compared with an estimated two million-plus on the Moon. The gap exists because Earth actively erases its own scars: plate tectonics recycles crust, weathering and glaciers grind down rims, and vegetation and sediment bury what is left. The Moon has none of those processes, so a crater formed there billions of years ago can look almost as fresh today as the week it formed.<\/p>\n<p>That imbalance is precisely why finds like Uhackatik carry weight beyond Quebec. With so few terrestrial impact structures available for direct, hands-on study, each new confirmed crater adds to a small dataset that planetary scientists use to understand cratering mechanics \u2014 central uplift formation, melt-sheet behavior, shock deformation \u2014 that are otherwise studied mainly through remote imagery of the Moon and Mars, where no one can walk up and check a rock face for shatter cones. Osinski\u2019s own work makes the link explicit: beyond running Impact Earth, he helps train NASA\u2019s Artemis astronauts in impact geology at Mistastin (Kamestastin) crater in Labrador, a Canadian structure chosen specifically because its shocked, melt-rich terrain resembles what astronauts will encounter on the lunar surface. A crater like Uhackatik is built from the same physical evidence, and reasoned about with the same tools, that scientists rely on to read the impact history of worlds no one has ever set foot on \u2014 evidence that here, unusually, can be reached on foot.<\/p>\n<p>Video recommendation: That same lunar surface is now the subject of a quiet contest of its own. No nation can legally own the Moon, yet several are already moving to secure lasting control over its most valuable ground. Space Daily has covered this in a video titled <a href=\"https:\/\/www.youtube.com\/watch?v=Zy23WDC-VjE\" target=\"_blank\" rel=\"noopener nofollow\">The Race to Own the Moon Has Already Started<\/a>.<\/p>\n<p class=\"bbm-disclaimer__heading\">About this article<\/p>\n<p class=\"bbm-disclaimer__body\">This article is for general information and reflection. It is not professional advice. For your specific situation, consult a qualified professional.<\/p>\n","protected":false},"excerpt":{"rendered":"In 2024, Quebec amateur astronomer Jo\u00ebl Lapointe was planning a camping trip in Quebec\u2019s C\u00f4te-Nord region and scrolling&hellip;\n","protected":false},"author":2,"featured_media":631524,"comment_status":"","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[23],"tags":[61,60,82,247],"class_list":["post-631523","post","type-post","status-publish","format-standard","has-post-thumbnail","category-space","tag-ie","tag-ireland","tag-science","tag-space"],"_links":{"self":[{"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/posts\/631523","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=631523"}],"version-history":[{"count":0,"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/posts\/631523\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/media\/631524"}],"wp:attachment":[{"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/media?parent=631523"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/categories?post=631523"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.newsbeep.com\/ie\/wp-json\/wp\/v2\/tags?post=631523"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}