In 2024, amateur astronomer Joël Lapointe noticed an unusual circular landform near Lake Marsal while looking at online satellite maps for a camping trip. The satellite image was only a lead: shatter cones, impact melt rock and dating analyses provided the evidence for a hypervelocity impact.
Published byEdited with GPT-5.6 TerraImages generated with GPT Image 2
Research answer

Create a landscape editorial hero image for this Studio Global article: How did French amateur astronomer Joël Lapointe’s 2024 Google Maps search for a campsite near Lake Marsal lead to the discovery and likely f. Article summary: Lapointe’s campsite search turned into a scientific lead because he recognized that the 25-kilometer ring centered on Lake Marsal looked like an impact structure, reported it to researchers, and their mapping, fieldwork,. Topic tags: general, government, general web, education. Style: premium digital editorial illustration, source-backed research mood, clean composition, high detail, modern web publication hero. Use reference image context only for broad subject, composition, and topical grounding; do not copy the exact image. Avoid: logos, brand marks, copyrighted characters, real person likenesses, fake screenshots, UI text, readable text, watermarks, charts
A circular pattern on an online map is not, by itself, proof of an impact crater. But near Lake Marsal in Quebec’s remote Côte-Nord region, one such pattern set off a chain of scientific checks that led to a remarkable conclusion: Uhackatik is a roughly 25-kilometre-wide structure formed by a hypervelocity impact about 390 million years ago. 1
2
In 2024, French amateur astronomer Joël Lapointe was examining online satellite maps while preparing for a camping trip in Côte-Nord. Near Lake Marsal, he noticed an unusually circular feature in the landscape. Rather than dismissing it as a quirk of the terrain, Lapointe wondered whether it could mark an ancient impact and contacted specialists in Europe and North America. 1
His report directed researchers’ attention to the Lake Marsal area as a possible impact structure. The feature’s subtle circular outline can also be seen in Landsat imagery, with Lake Marsal close to its centre. 1
Circular landforms can be produced by many geological processes, including volcanism, tectonic activity and erosion. A satellite image can identify a site worth investigating, but cannot establish how it formed.
Researchers therefore reviewed geological maps, topographic data and available rock samples before conducting a dedicated field expedition. That October 2025 investigation included planetary geologist Gordon Osinski of Western University and produced much stronger on-the-ground evidence. 2
At the structure’s centre, the team found decimetre-scale shatter cones in Grenvillian basement rock. These cone-shaped fracture patterns form when exceptionally powerful shock waves travel through rock, making them a particularly compelling large-scale indicator of an impact event. 1
2
The researchers also reinterpreted the nearby Marsal Breccia Formation. Previously described as volcanic material, it is now understood to be impact-melt rock: a layer potentially up to about 50 metres thick, with columnar joints and fragments of the underlying basement rock. Those features add to the evidence from the shatter cones. 2
Measurements from oriented core samples indicate an age of about 390 million years, within a range of 370 million to 400 million years. Preliminary lead-isotope data from zircon also point to a compatible youngest age range of roughly 350 million to 400 million years. Together, the analyses support a Devonian-age impact at around 390 million years ago. 2
The research team’s scientific summary concludes that the combined evidence confirms a hypervelocity-impact structure approximately 25 kilometres across. 2
After discussions with the Innu Council of Ekuanitshit, the researchers chose the name Uhackatik for the structure. 2
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The team considers its impact origin essentially confirmed. However, formal listing in official impact-structure catalogues is still subject to review by a Meteoritical Society committee. The most accurate description, therefore, is that Uhackatik has very strong evidence for an impact origin and is awaiting formal recognition rather than having completed that process. 8
Uhacakik’s story is a clear example of public observation and specialist research working together. Lapointe did not confirm an impact crater from Google Maps; he identified an intriguing pattern and brought it to experts. The scientific case came from shock features in rock, geological interpretation and age measurements. 1
2
That process turned a faint ring around Lake Marsal into one of Canada’s most notable ancient impact structures.
Studio Global AI
This page includes a source-backed answer you can continue inside Studio Global.
In 2024, amateur astronomer Joël Lapointe noticed an unusual circular landform near Lake Marsal while looking at online satellite maps for a camping trip.
In 2024, amateur astronomer Joël Lapointe noticed an unusual circular landform near Lake Marsal while looking at online satellite maps for a camping trip. The satellite image was only a lead: shatter cones, impact melt rock and dating analyses provided the evidence for a hypervelocity impact.
Researchers chose the name Uhackatik following discussions with the Innu Council of Ekuanitshit; formal catalogue recognition is still pending.
In 2024, amateur astronomer Joël Lapointe noticed an unusual circular landform near Lake Marsal while looking at online satellite maps for a camping trip. The satellite image was only a lead: shatter cones, impact melt rock and dating analyses provided the evidence for a hypervelocity impact.
Published byEdited with GPT-5.6 TerraImages generated with GPT Image 2
Research answer

Create a landscape editorial hero image for this Studio Global article: How did French amateur astronomer Joël Lapointe’s 2024 Google Maps search for a campsite near Lake Marsal lead to the discovery and likely f. Article summary: Lapointe’s campsite search turned into a scientific lead because he recognized that the 25-kilometer ring centered on Lake Marsal looked like an impact structure, reported it to researchers, and their mapping, fieldwork,. Topic tags: general, government, general web, education. Style: premium digital editorial illustration, source-backed research mood, clean composition, high detail, modern web publication hero. Use reference image context only for broad subject, composition, and topical grounding; do not copy the exact image. Avoid: logos, brand marks, copyrighted characters, real person likenesses, fake screenshots, UI text, readable text, watermarks, charts
A circular pattern on an online map is not, by itself, proof of an impact crater. But near Lake Marsal in Quebec’s remote Côte-Nord region, one such pattern set off a chain of scientific checks that led to a remarkable conclusion: Uhackatik is a roughly 25-kilometre-wide structure formed by a hypervelocity impact about 390 million years ago. 1
2
In 2024, French amateur astronomer Joël Lapointe was examining online satellite maps while preparing for a camping trip in Côte-Nord. Near Lake Marsal, he noticed an unusually circular feature in the landscape. Rather than dismissing it as a quirk of the terrain, Lapointe wondered whether it could mark an ancient impact and contacted specialists in Europe and North America. 1
His report directed researchers’ attention to the Lake Marsal area as a possible impact structure. The feature’s subtle circular outline can also be seen in Landsat imagery, with Lake Marsal close to its centre. 1
Circular landforms can be produced by many geological processes, including volcanism, tectonic activity and erosion. A satellite image can identify a site worth investigating, but cannot establish how it formed.
Researchers therefore reviewed geological maps, topographic data and available rock samples before conducting a dedicated field expedition. That October 2025 investigation included planetary geologist Gordon Osinski of Western University and produced much stronger on-the-ground evidence. 2
At the structure’s centre, the team found decimetre-scale shatter cones in Grenvillian basement rock. These cone-shaped fracture patterns form when exceptionally powerful shock waves travel through rock, making them a particularly compelling large-scale indicator of an impact event. 1
2
The researchers also reinterpreted the nearby Marsal Breccia Formation. Previously described as volcanic material, it is now understood to be impact-melt rock: a layer potentially up to about 50 metres thick, with columnar joints and fragments of the underlying basement rock. Those features add to the evidence from the shatter cones. 2
Measurements from oriented core samples indicate an age of about 390 million years, within a range of 370 million to 400 million years. Preliminary lead-isotope data from zircon also point to a compatible youngest age range of roughly 350 million to 400 million years. Together, the analyses support a Devonian-age impact at around 390 million years ago. 2
The research team’s scientific summary concludes that the combined evidence confirms a hypervelocity-impact structure approximately 25 kilometres across. 2
After discussions with the Innu Council of Ekuanitshit, the researchers chose the name Uhackatik for the structure. 2
8
The team considers its impact origin essentially confirmed. However, formal listing in official impact-structure catalogues is still subject to review by a Meteoritical Society committee. The most accurate description, therefore, is that Uhackatik has very strong evidence for an impact origin and is awaiting formal recognition rather than having completed that process. 8
Uhacakik’s story is a clear example of public observation and specialist research working together. Lapointe did not confirm an impact crater from Google Maps; he identified an intriguing pattern and brought it to experts. The scientific case came from shock features in rock, geological interpretation and age measurements. 1
2
That process turned a faint ring around Lake Marsal into one of Canada’s most notable ancient impact structures.
Studio Global AI
This page includes a source-backed answer you can continue inside Studio Global.
In 2024, amateur astronomer Joël Lapointe noticed an unusual circular landform near Lake Marsal while looking at online satellite maps for a camping trip.
In 2024, amateur astronomer Joël Lapointe noticed an unusual circular landform near Lake Marsal while looking at online satellite maps for a camping trip. The satellite image was only a lead: shatter cones, impact melt rock and dating analyses provided the evidence for a hypervelocity impact.
Researchers chose the name Uhackatik following discussions with the Innu Council of Ekuanitshit; formal catalogue recognition is still pending.