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Headshot of Emily Lakdawalla

New MESSENGER image release: Mercury at high resolution

Posted by Emily Lakdawalla

16-01-2008 14:31 CST

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Today's image release from the MESSENGER team is really gorgeous. I'd better go ahead and post it at the top before I start writing volumes:

Vivaldi crater and environs from MESSENGER

NASA / JHUAPL / CIW

Vivaldi crater and environs from MESSENGER
MESSENGER took this image of Mercury on January 14, 2008 at 18:06, about an hour before the closest approach of its first flyby. The image is one frame from a 55-image mosaic of Mercury's crescent. The most prominent feature in the image is the double-ringed Vivaldi crater and its rays of secondary craters. The outer ring of Vivaldi is about 200 kilometers in diameter. Other craters in the image display a variety of degradation states; some are deep bowls with sharp central peaks, while others are flat-floored, so must have been filled in (most likely by volcanic eruptions).
What are we looking at here? This is one frame from a large mosaic (5 columns by 11 rows) that MESSENGER's narrow-angle camera tiled across the crescent view of Mercury as it approached. After some noodling around with the dynamic visualization tool I found the moment that it was captured; click here to see the exact location of the image (heavily outlined blue square in the "Sensor Footprint" section).

The image geometry is a little unusual, so I'd better explain that before I try to interpret it. Sunlight is coming from the left, and the image covers some areas that are well lit by the Sun, but toward the right side of the image we are getting into the terminator, the day/night boundary on Mercury. By the rightmost edge of the image the Sun slants almost horizontally onto the raised rim of the double-ringed crater Vivaldi, so that the entire floor of Vivaldi is in nighttime darkness, but the peaks of its double rim, especially the inner ring, are brightly side-lit by the Sun. Because MESSENGER had only a crescent-phase view of Mercury at this point, we're looking at the edge of Mercury's globe, so all the craters appear squashed left-to-right from foreshortening.

So what do I see in this image? There's lots of craters, of course, but if you look closely at the craters you can see that there's a lot of differences among them. In particular, my eye is immediately drawn to the fact that the craters at the left side of the image mostly have very flat floors, but among them are a few craters that have fairly pristine bowl shapes and central peaks. When craters first form, they all have bowl shapes, or bowls with central peaks, or peak rings. Craters do not form with smooth, flat floors. So something must have happened -- some geologic activity -- to flatten the floors of all those flat craters; most likely they got filled in by some volcanic eruptions. Those volcanic eruptions had to happen before the central-peak craters, which never got filled in by lava. So already there is a geologic history to tell about this tiny area of Mercury, coming out of this one image.

Another thing that leaps out at me is chains or lines of small craters. You can draw lines through them and they mostly converge at the position of Vivaldi, so that suggests to me that these are secondaries, craters that formed when something big smashed into Mercury to make Vivaldi, which threw mountains of Mercurian crust into the air, which smashed back down to the ground to make a splash of small, secondary craters surrounding the big one.

Another thing I see is subtle linear features running roughly north-south among the smooth plains between the craters on the left side of the image. I spoke with MESSENGER MASCS instrument scientist Noam Izenberg about those today, and asked him if they were wrinkle ridges or rupes or maybe the steep fronts of ancient volcanic flows. He told me they could be all of the above! Hopefully the color data from MESSENGER's other camera will help tease out if they are lava flows; every lava flow has a slightly different composition, and if MESSENGER's science team is lucky, they'll be able to process the color images in such a way that different lava flows with different compositions will leap off the screen in different colors. We'll see.

One thing that the MESSENGER team is pointing out about this image is the fact that although Vivaldi was identified and named based on Mariner 10 images, the topographic depression to the lower left of Vivaldi was nowhere to be seen in the Mariner 10 data. Because there's been a lot of talk about how MESSENGER will be adding to Mariner 10's coverage of Mercury, I thought it would be a valuable exercise to track down the actual, original Mariner 10 images of this same area for comparison.

To track them down, I checked out the United States Geological Survey's shaded relief maps of Mercury, derived from the Mariner 10 data. The USGS maps, which were produced in 1977, are actually artworks, airbrushed paintings based on the original photos. This works well for making planetary maps because images from missions are often taken from many points of view, at different times of day, with lighting coming from all different directions, so to make a map with consistent lighting they really have to draw it from scratch. After looking at the map of the whole planet I figured out that Vivaldi can be found on the Beethoven Quadrangle. The Beethoven Quadrangle map includes a little detail map that shows which actual Mariner 10 images formed the reference points for each area on the map: in this case it seemed the images with numbers 166766, 166767, and 166768 were the ones that contained Vivaldi and environs. Those numbers can be plugged in to the Advanced Image Search tool at the Mariner 10 Image Archive to find the actual images; this archive is great because it contains cleaned-up versions of the images (which originally were marred by lots of noise and reseau markings). Finally, I brought the images into Photoshop, and pasted two of them together that cover the area in the MESSENGER image. The original Mariner 10 images were significantly foreshortened, squashed north to south, so I stretched them vertically to make Vivaldi crater look more round. With this stretching, the Mariner 10 image below has somewhat smilar pixel resolution as the MESSENGER photo above.

Vivaldi crater and environs from Mariner 10

NASA / JPL / Emily Lakdawalla

Vivaldi crater and environs from Mariner 10
Mariner 10 took the images for this mosaic (166766 and 166767) on September 21, 1974 at 21:13 and 21:14 UTC as it was departing from its second flyby of Mercury.
You can instantly see that MESSENGER has provided us with tons more detail on the topography of this area than you could get from the Mariner 10 data. That's not so much because of differences between the cameras but because of the different lighting geometry. The raking light in the MESSENGER image picks out topographic details that are totally invisible in the Mariner 10 image. However, there's a cost. With such extreme lighting geometry, all the variation in brightness and darkness across the MESSENGER image results from topography: slopes tilted toward the Sun are bright, slopes tilted away are dark, and flat areas intermediate. In the Mariner 10 image, where the Sun was higher, you don't see topography; instead, you see variations in brightness (referred to as "albedo" variations), which have to do with differences in composition or texture among the surface materials. Vivaldi's inner ring shows up as a strange bright crescent. In fact, many of the craters, particularly the ones that still have their central peaks, are outlined by bright rims. At the same time, there are enigmatic bright streaks and dark splotches here and there. All of this is invisible in the MESSENGER image. So I think this comparison proves that as gorgeous as the data will be from MESSENGER, there is still going to be value in the Mariner 10 data set. Or, looking at it from a different direction, even though half of Mercury has already been mapped by Mariner 10, there will of course be great value in MESSENGER's fresh look at it.
First look at the unseen face of Mercury

NASA / JHUAPL / CIW

First look at the unseen face of Mercury
This image was taken by the MESSENGER spacecraft at about 20:24 UTC on January 14, 2008, about 80 minutes after its closest approach to Mercury. Most of the face of Mercury visible in this image was not seen by Mariner 10.
On a different topic, one of the things I neglected to discuss yesterday was how amazing it is that Mercury was precisely where MESSENGER expected it to be. That image of Mercury just about fills the field of view of MESSENGER's wide-angle camera, and it's just about exactly centered in the frame, which means that the spacecraft's pointing had to be absolutely spot-on. You can't just tell a spacecraft "point at Mercury and click." You have to command every little rotation of the spacecraft: so much roll about each of the three spacecraft axes to align the spacecraft with wherever Mercury was at each second of the flyby, plus how many degrees the camera should be tilted, and then click at precisely this hundredth of a second for the part of Mercury you're interested in to be in the field of view. Louise pointed out to me that the wide-angle camera departure image released last night was taken late in the flyby, and for it to be so precisely framed boded well for the pointing of all the images taken before it.

The precision of the pointing is even more amazing than I realized. I've been exchanging emails with MESSENGER mission design lead engineer Jim McAdams, who pointed out to me that the last time MESSENGER fired its rockets to fine-tune its trajectory and aim for the 200-kilometer-altitude flyby point was nearly a month before the flyby, on December 19, 2007, when the spacecraft was more than 100 million kilometers away from Mercury. They missed their aimpoint by only 1.43 kilometers in altitude after traveling that 100-million-kilometer distance! This is, in Jim's words, "spectacular" targeting.

They did have a planned opportunity for another rocket firing to take place on January 10, but were able to skip it through an ingenious application of a spacecraft navigation technique that is near and dear to the hearts of Planetary Society members: solar sailing. Jim told me,

We were able to cancel the planned TCM-20 [Trajectory Correction Maneuver number 20] on January 10 by "solar sailing" the spacecraft closer to the intended aimpoint. Analysis performed by our Guidance & Control, Navigation, and Mission Design teams all indicated that TCM-20 could be cancelled if we achieved the needed shift toward the target point by tilting the solar panels an extra 20 degrees away from the Sun about three days earlier than planned.
I asked him to elaborate a bit on how they have to take the pressure of solar radiation on MESSENGER's heat shield and solar panels into account when they predict its future trajectory, and he said:
We have computer models of the spacecraft that link the actual (past) and predicted spacecraft attitude to distance from the Sun, solar flux, and surface reflectance properties for all components of the spacecraft that face the Sun. The net solar radiation pressure acceleration is computed for each of the sunlit components of the spacecraft, and the resultant sum is applied as a trajectory perturbation. These models are frequently updated as more orbit data is collected and analyzed. Accurate computation is very important in Mercury orbit, especially since trajectory correction maneuvers occur in pairs only once per 88 days after Mercury orbit insertion.

 
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