Mercury's shadowy North Pole revealed by M-CAM 1
The BepiColombo mission captured images of Mercury's north pole, revealing shadowy craters that may contain frozen water and showcasing ancient volcanic activity, aiming to investigate Mercury's geological history.
Read original articleThe European Space Agency (ESA) and Japan Aerospace Exploration Agency (JAXA) BepiColombo mission captured significant images of Mercury's north pole during its sixth gravity assist maneuver on January 8, 2025. The spacecraft's monitoring camera, M-CAM 1, took a long-exposure photograph from approximately 787 km above the surface, revealing the shadowy polar craters. The images show the terminator line, which separates day from night, highlighting sunlit crater rims such as Prokofiev, Kandinsky, Tolkien, and Gordimer. These craters cast permanent shadows due to Mercury's nearly perpendicular spin axis, making them some of the coldest locations in the Solar System. Preliminary evidence suggests that these dark craters may contain frozen water, a key aspect of BepiColombo's ongoing investigation. The images also depict Borealis Planitia, Mercury's largest volcanic plains formed by ancient lava flows. The geological features observed, including the solidified lava and crater formations, provide insights into Mercury's volcanic history, comparable to significant volcanic events on Earth. The BepiColombo mission aims to further explore these mysteries once it enters orbit around Mercury.
- BepiColombo captured images of Mercury's north pole during a gravity assist maneuver.
- The images reveal shadowy craters that may contain frozen water.
- Mercury's craters are among the coldest places in the Solar System.
- Borealis Planitia showcases ancient volcanic activity on Mercury.
- The mission aims to investigate Mercury's geological history and potential water presence.
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This framing is reminiscent of similar oversights in planetary science, such as the perplexing case of Mars' north pole. Studies suggest a cyclical process where subsurface vapor escapes through a thinned crust during colder seasons, freezing into massive ice deposits, like those seen in the Korolev Crater. These ice layers, some over 1.2 miles thick (see the ESA Korolev Crater Study), challenge the traditional narrative of Mars' geophysical activity. Observations from missions like Mars Express and Mars Reconnaissance Orbiter reveal hints of dynamic interactions between the crust and atmosphere, yet much of this is glossed over in mainstream discussions.
Why is there a persistent pattern of incomplete or opaque presentations regarding planetary poles? The public deserves transparency and detailed interpretations, not handwaving claims. If the evidence of crustal thinning and volatile release is as compelling as the imagery suggests, why the reluctance to address it head-on???
A commitment to clarity would foster trust in scientific institutions, rather than leaving informed observers to speculate about what's being left unsaid. This is frustrating.
I'm curious how this works. The dynamic range between the sunlit parts and the dark portions must be huge at that distance from the Sun. Anyone have the technical details on the camera or post processing they use to achieve this? Is it really a long exposure or is it a series of photos at different exposures stitched together?
Edit: details at the bottom seem to imply a single photo, but that "long exposure" really isn't that long
>This image of Mercury's surface was taken by M-CAM 1 [...] using an integration time of 40 milliseconds.
Update: From this map [3], the pole appears to be on the rim of the crater touching crater Tolkein on the latter's right (see ahazred8ta's comment for a link to an annotated copy of the photograph), and in the photograph, that part of the rim is illuminated.
[1] https://nssdc.gsfc.nasa.gov/planetary/factsheet/mercuryfact....
[2] Data from [1] and https://en.wikipedia.org/wiki/Sun:
Solar radius: 7e8 M
Mercury aphelion: 7e10 M
Angular radius at aphelion = arctan 0.01 = 0.57 degrees.
[3] https://pubs.usgs.gov/sim/3404/sim3404_sheet2_.pdfRelated
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