See other posts from January 2008
Looking over Mercury's limb
Posted By Emily Lakdawalla
2008/01/17 12:45 CST
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This is just a brief post as I'm hard at work on a lengthy story wrapping up the MESSENGER Mercury flyby. There is a steady trickle of images coming out from the MESSENGER mission, and one of the ones from this morning's release really tickled my imagination. In this view, taken as MESSENGER approached Mercury, we're looking across Mercury's limb at black space. I love the slanting perspective of photos across the edges of planetary disks, and the slanting light in this high-phase view makes it all the more dramatic. Here's the dynamic visualization for context.

NASA / JHUAPL / CIW
Across Mercury's horizon
This view of Mercury's limb against black space is part of a large mosaic of a crescent Mercury that MESSENGER saw on its approach to its first flyby of the planet, on January 14, 2008 at 18:10 UTC. The large crater at lower right was seen by Mariner 10 and named Sholem Aleichem.I wanted to see if Mercury's craters really were unusually smooth, so I hunted down an image of the Moon with similar geometry to compare it to. I was looking for a crescent phase view that would have the same dramatic lighting as the MESSENGER Mercury approach images. Again, I'm grateful to the Lunar and Planetary Institute for their efforts to place the entire archive of Lunar Orbiter images online, because it contains a lot of treasures, including this lovely view of a crescent-phase Moon, taken from its far side. I prefer farside images of the Moon for comparison to Mercury, because the near side of the Moon is so completely covered with dark mare basalts that its geology has a totally different character to Mercury's. The lunar far side is much more similar to Mercury, at least superficially.
And here's a closeup of the northern edge of the limb, with roughly similar geometry to the MESSENGER one.I think the image of the Moon is qualitatively lumpier, though some craters do have very smooth floors. I suppose most of the difference can be explained by the difference in surface gravity between the two worlds; Mercury's gravity is (owing to its larger diameter and much larger bulk density) more than twice as large as the Moon's. (The Moon's gravity is about 17% that of Earth's; Mercury's is 37%.) Lower gravity allows a planet to support steeper cliffs.Blog Search
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