Six days to go until Enceladus flyby ( E2? ) at 175 km
We also get NT encounters. I hope we get those images also.
I should be posting my E2 preview either today (maybe...) or early next week on my blog.
That E2 preview is now online:
http://volcanopele.blogspot.com/2005/07/enceladus-2-and-other-rev-11.html
21000 km to Enceladus ![]()
Can't wait to see the images tomorrow
Should be neat to see the images. I have been watching using Celestia to visualize the view of Enceladus from Cassini's vantage point. It is running with a real-time animation using a version of my Enceladus map.
I don't expect anything till monday. When an encouter falls so close to the weekend we get plauged by the red x problem.
Update on the Cassini website:
Enceladus Flyby Update
The Cassini spacecraft conducted its closest flyby yet, coming within 175 kilometers (109 miles) from the surface of Enceladus. Data collected is currently being downloaded. Raw images are expected to appear on this web site at around 10 p.m. PDT.
http://saturn.jpl.nasa.gov/home/index.cfm
http://ciclops.org/view_event.php?id=22
From 545 kilometers
actually, that's distance to target center so the altitude is actually 295 km ![]()
2 m/pixel
Is that Enceladus or a block of London flats after The Blitz?
Fascinating right angles, there...
-the other Doug
First mosaic of this fly-by. Looks like it was take in Saturn shine:
http://paranoid.dechengst.nl/saturn/Enceladus5.jpg
Nice distant view of the http://saturn1.jpl.nasa.gov/multimedia/images/raw/raw-images-details.cfm?feiImageID=45595 (or whatever they're called).
Six frame highres mosaic. Some artifacts due to the changing viewing geometry between frames though
http://paranoid.dechengst.nl/saturn/Enceladus6.jpg
Three frame mosaic. Couldn't get the bottom left quadrant to fit properly
http://paranoid.dechengst.nl/saturn/Enceladus7.jpg
DEChengst: I can't get any of your links tonight to load, either viewing them directly, or using the 'Save As' trick. "The page you are looking for is currently unavailable" message.
Note... that Super-High-Rez image is motion blurred. Nice linear blur. Should be easy to deconvolve to nearly full resolution.
Wonderful images!
Ed, I was able to download DEChengst's images at 6:30AM CDT, FWIW.
--Bill
Am I seeing things?
The Tiger scratches seem to have something coming out of them!?
Like a haze. It could be along the sides of the 3 cracks possible on the ground.
This is speculation on my part.
Here is another version of the crescent mosaic...I processed it to hide the saturn-shine areas so that you can't see the missing areas.
http://img238.imageshack.us/my.php?image=e11mo22yo.jpg
Here is where the closeup image N00037070.jpg fits in the larger one (W00009337.jpg)
Dead on the center
Wow, especially the tiger scratches look amazing!!
Hey... check out that diamond shaped region to the upper right of the "tiger scratches" in the above referenced image. Anyone remember Miranda's "chevron" feature?...
Very strange morphology. Some of the larger "scratches" seem to show evidence of parts of the wall sliding into the valleys. Also notice how some craters show radial cracks in addidion to the main crack pattern and the virtual absence of impact craters in the lower part of the mosaic. This is fairly young terrain.
tty
I was surprised to the the boulders is closest image. I don't remember seeing boulders in the closeups of Europa
I refer to the high res image of Enceladus. I suspect a pixel size of about 6-7 meters because the distance is 545km acc. RAW data and 2x2 binning of the sensor. These boulders must be really large ones !
IMHO the larger distance results from the other black images, that shows smaller distances than Enceldaus radius (for example W00009338.jpg in 210 km distance).
Further it could be still larger away because of the oblique angle of this particular shot.
Robert Schulz
Obviously, remnants of surficial cracking from either gravitic stresses on Enceladus or from internal stresses which caused upwelling from the cracks.
Europa, anyone? This looks like extensive cracking atop a liquid ocean...
-the other Doug
Double post.
Nice work!
My attempt at a colored image. Note I'm new at this!
DEChengst I hope you don't mind me using your stitched image (One of my favs
)
I think there's something more dramatic going on at Enceladus than at Miranda. First, we have the multiple evidence for outgassing, which indicates current activity. Then, we have the extreme youth of some of the tectonic features -- just look, for instance at http://saturn.jpl.nasa.gov/multimedia/images/raw/raw-images-details.cfm?feiImageID=45673 .
I think that what we're seeing at Enceladus -- just as it's believed we're seeing it at the inner three Galilean satellites -- is INTERMITTENT tidally stimulated geological activity over cycles of tens to hundreds of millions of years, produced by the fact that the moons keep drifting into and out of more or less intense resonance relationships as they slowly spiral away from their central planets. In the case of Enceladus, the cycles are a lot slower and less intense than with Europa -- a matter of 100 or 200 million years, rather than just a few tens of millions, and not intense or widespread enough to obliterate most of the moon's craters -- but they are nevertheless there. I suspect Enceladus' remaining outgassing is a result of the fact that it's still cooling off from its last period of maximum tidal heating. But I also wouldn't be surprised if, even at its maximum, Enceladus' geological activity didn't take the form of oozing warm-ice diapirs with only a relatively small amount of liquid water/ammonia mixed in, just as Jason suggests.
Having said that, let me add that the geology of the Uranian satellites is one of my biggest remaining areas of ignorance about the Solar System -- I just haven't quite gotten round to studying them yet, for some reason.
Looking at the raw images of the south polar region on Enceladus, I don't see *** ANY *** impact craters in large swaths of the swirly-ridge-and-trough terrains. This surface is young. Damn young. ?tens? of millions of years max, maybe.
A nice little shot of Pandora over the clouds of Saturn has come in!
http://www.imageshack.us
That was quick: updated map of Enceladus on Steve Albers website
http://laps.fsl.noaa.gov/albers/sos/sos.html
Does steve have polar projections?
I shamelessly stole Steve Albers' cylindrical projection of Enceladus (thanks!) and made this polar projection of the southern hemisphere (just using the polar coordinates function in Photoshop):
Very nice.
I wonder how enceladus magnetic field/south pole lines up with those "4 cat scratches"
Another attempt at a coloring. ![]()
I'm not sure how this is done correctly.
Is there a site that explains how to this in adobe?
I think that we got some pretty good coverage of the North Polar region on the leading hemisphere from Saturnshine images. As for the other side, the highest resolution Voyager set covers much of it. I am working on a super-res image.
I don't know about anyone else, but I haven't found any signs of ice volcanoes or guysers yet.
Here is all I could do...the images are at impossibly different angles.
http://img79.imageshack.us/my.php?image=sup13da.jpg
Bizarre boulders litter Saturn moon's icy surface
Post-Voyager, there was a spate of studying the potential of ammonia/water volcanism. Assorted studies of the very complex phase diagram of the two ices and the physical properties of melts. Some melts at low temperatures are very runny-liquid, while higher temperature melts with a different ammonia/water molecular ratio is like soft-taffy! Certainly there were a number of abstracts in the yellow-books: LPSC conference Abstracts from the period. Where final papers were published, I don't know.
Note that it's unlikely ammonia will be dectected on Enceladus's surface even if eruption is happening recently in geologic terms.. It takes hard UV to split oxygen and hydrogen. Quite soft UV, of which sunlight has a lot more, is all you need to split nitrogen and hydrogen. Exposed ammonia ice will have a quite short <years? decades?> lifetime.
Any news about the INMS and UVIS observations ?
New update.
http://ciclops.org/view_event.php?id=23
The magnetometer instrument confirmed an atmosphere at Enceladus during the July 14 flyby. Data from this flyby and modeling work of previous data shows that the atmosphere is concentrated over the south polar region and is much more rarified over the rest of the surface.
The plot thickens...
http://www.pparc.ac.uk/Nw/enceladus_flyby.asp
http://volcanopele.blogspot.com/2005/07/press-release-magnetometer-instrument.html
UVIS detects Enceladus' atmosphere (and also sees the same spatial non-uniformity that MAG found):
http://photojournal.jpl.nasa.gov/catalog/PIA06431
And now for the punch-line: CIRS found a hot spot near Enceladus' south pole:
http://photojournal.jpl.nasa.gov/catalog/PIA06432
news release:
http://saturn.jpl.nasa.gov/news/press-release-details.cfm?newsID=592
very interesting indeed! Looks more and more like Europa, only active!
Sorry for the double post, didn't realize I was posting in the wrong thread:
nope, still an image artifact. If it were real, then when viewed from the same geometry, here are plumes over Mimas, Rhea, Tethys, and Titan over the same area of the crescent.
However, I can't deny we haven't gone back and taken another look at it. but mostly likely the activity we are seeing is do to evaporation or outgassing rather than a full fledged plume.
Enceladus looks more like Ganymede instead of Europa.
How neat that this is the punchline to the evidence building up over months and even decades. Perhaps 6-12 months ago, the Y shaped features looked at low resolution like some sort of amorphous petals of a giant flower ringing the south pole. Even then something strange was being foreshadowed and how fun it has been to see the resolution gradually increase since then.
Yesterday (July 29) there was a CICLOPS release of the tiger scratches in enhanced color close up. Overlain are 10 squares showing the CIRS temperature measurement pixels. It actually can pinpoint the tiger scratches as the heat source.
Sorry for my insistence, Jason. Can you kindly pinpoint an image showing similar artifact on Mimas, Rhea, Tethys, and Titan? thkx
I wonder could those "tiger scratches" be something analogous to mid-ocean ridges where "lava" from below intrudes and pushes "lithospheric" plates apart?
tty
grrr....true, very true. It was a Sunday morning..I'm never awake on a sunday morning.
This might be a better example than just pointing out the poles....a side by side comparison of the terrain around each polar region.
Greetings,
Thought I'd mention some speculations about a couple of items in this topic. I wonder if it would be that surprising to be able to obtain enough tidal heat to warm Enceladus? Note its orbital eccentricity of .004 and the significant tidal distortion of its equatorial radius in the X and Y directions (5-10km?). A rough guestimate of the tidal flexing within each orbit might then be 10-20m? Would this be of the same order of magnitude as the tidal flexing on Europa? On the other hand, this line of reasoning would suggest much more tidal heating of Mimas, having a more elliptical shape and greater orbital eccentricity.
Will be interesting to hear more of VP's investigation of the glare/artifact that looks like a plume. My speculation is that it would not be caused by the sun if it is well correlated by Enceladus' position. Also, given that it appears to emanate from the S polar region and not other portions of the crescent, it's difficult for me to imagine a type of glare pattern that would do this, since the crescent should have relatively uniform illumination over its area.
That's an interesting tidbit about Enceladus wandering back and forth through the Dione 2:1 resonance. I hadn't heard that. Do you have a link handy?
Well, that means YOU'RE very lucky, but the same can't be said for scientific observations of Enceladus as a whole during the next flyby. Once again, several more flybys are obviously needed during the extended mission.
Don't be so shy, Steve! Put in http://laps.fsl.noaa.gov/albers/sos/sos.html#ENCELADUS
I talked this afternoon with Dr. Linda Spilker -- and it turns out that the puzzle
of that quote from her in the Planetary Society article (
http://www.planetary.org/news/2005/enceladus_active_0730.html )...
"The water vapor is very different from the E ring particles themselves. So
we have this sort of cloud, patchy atmosphere over the south pole, and then
the E ring particles seem to be coming uniformly off of Enceladus, probably
through micrometeorite impact kicking up particles. So the vents are not the
source of the E ring."
...is explained by the simple fact that Emily Lacdawalla misquoted her, and
in fact apparently made the last sentence up out of thin air. (Upon being
informed of what she was being quoted as saying, Spilker promised to give
Emily a Talking To.) So here's the real story:
What she actually told Lackdawalla is that the E Ring particles, as analyzed by Cassini's Cosmic Dust Analyzer, are basically just water ice, while the stuff that Cassini detected at Enceladus' south pole is water VAPOR. Period. End of story. No meaningful compositional difference to indicate that the E Ring particles are not coming originally from Enceladus' southern vents -- in fact, she agreed that it's very hard to explain the E Ring particles as having been knocked off Enceladus by meteoroid impacts, for the simple reason that in that case we'd see comparable rings centered around the orbits of Saturn's other icy moons.
When I suggested the following model of what is actually going on, she also
agreed with it: Water/ammonia mixture, with a little methane mixed into it (as also detected by Cassini), is spurting from vents near Enceladus' south pole -- indeed, the vaporizing methane is probably largely responsible for driving the venting. (The vents are probably those little dark speckles, near the cracks, that look like Enceladan blackheads -- at any rate, http://www.aas.org/publications/baas/v37n3/dps2005/450.htm says so.
Presumably their blackness results from the fact that a small amount of the
methane has been locally radiolyzed into dark carbon compounds, just as on
Pluto.)
The NH3 vapor is almost immediately broken down by solar UV into nitrogen
and hydrogen, thus explaining both the lack of NH3 in Cassini's gas analyses
and the surprisingly large amount of molecular hydrogen in it. This also
means that most of the 28 AMU gas detected by Cassini is indeed nitrogen
rather than carbon monoxide. (It turns out that Cassini's UVIS can measure both
CO and atomic N --http://www.aas.org/publications/baas/v37n3/dps2005/452.htm -- but, like a
fool, I forgot to ask Spilker about its findings. However, we already know
that most of the atomic N in Saturn's magnetosphere is concentrated around the E
Ring, with very little coming from Titan's atmosphere.)
The H2O and CH4 are broken down by solar UV a lot more slowly, although
Spilker said that Cassini did indeed detect a large amount of OH in the
cloud from water breakdown. (The carbon released from the decomposing methane -- or, alternatively, carbon monixide also released from Enceladus' subsurface -- may react with the atomic oxygen to produce the carbon dioxide gas detected by Cassini, which is rather hard to explain otherwise given the low temperatures.) However, a lot of the water vapor spreads all the way around Enceladus -- and, in fact, out into the E Ring -- without breaking down, and then refreezes as those tiny particles of ice in the Ring, which are relatively even in size (unlike the power-law distribution of various-sized fragments of material in all the other rings, including the F and G Rings). Spilker actually dropped another tidbit backing this up: the CDA team has seen what may be an asymmetry in the distribution of water-ice particles around Enceladus, but are still trying to decide whether it's statistically significant.
A lot of that refreezing water vapor also forms the pure-water, fine-particle "snow" that seems to coat all of Enceladus evenly, including the parts that haven't ever had surface geological activity. (And is it possible that those big "boulders" that so surprised everyone in the very high-resolution photo of the active region are actually "snowballs", made of water-ice particles that are clumping together in the immediate vicinity of the vents -- maybe because of influence by the local high concentration of ammonia vapor?)
A neat picture -- although, of course, it does nothing to answer the billion-dollar questions: what's driving the heating that causes the vents, and just how much liquid water/ammonia mixture is there in the subsurface underneath them? There is, by the way, one hell of a lot of other interesting new stuff from Cassini/Huygens in the new DPS abstracts, brief as they are. More on those other items later.
It occurs to me that what I said about Emily Lackdawalla was very tactlessly phrased -- but, unfortunately, it remains true. Linda Spilker DID say that Ms. Lackdawalla completely misinterpreted what Spilker had told her, and she did say that she hadn't said anything remotely suggesting that the E Ring particles definitely did not come from the vents. She did say that the science teams themselves are still not entirely certain on that point -- but she added (as other members of this group have also said) that in that case it's very hard to see why Saturn's other moons aren't also producing comparable numbers of E Ring particles.
As for the Enceladan "blackheads", they turn up on a very large number of photos in all three close flybys -- they jumped out at viewers immediately even during the first, "untargeted" close flyby in February. Here's a few examples:
http://saturn.jpl.nasa.gov/multimedia/images/raw/raw-images-details.cfm?feiImageID=45675
http://saturn.jpl.nasa.gov/multimedia/images/raw/raw-images-details.cfm?feiImageID=45662
http://saturn.jpl.nasa.gov/multimedia/images/raw/raw-images-details.cfm?feiImageID=34984
http://saturn.jpl.nasa.gov/multimedia/images/raw/raw-images-details.cfm?feiImageID=34976
Ms. Lakdawalla has indeed -- understandably -- hit the ceiling about my accusation. Another conversation I've just had with Dr. Spilker confirms that the key erroneous statement "So the vents are not the source of the E Ring" was indeed made to Ms. Lakdawalla, in just those words, by Dr. Spilker herself, because it was the tentative very early conclusion of the Cassini science team themselves (which they have now completely changed their minds about, on what would seem to be the obvious grounds that Saturn's other moons aren't throwing off E Rings of their own).
So Ms. Lakdawalla concocted exactly nothing; the error was entirely one by her source. My profound apologies to her. (Also, my embarrassed apologies for managing to misspell her name twice in a row. You'd think that someone whose name is misspelled as often as mine is would be a bit more sensitive to that point as well.)
Can I just say how impressed I've been with Emily Lakdawalla's coverage of Cassini on the Planetary Society Web site?
Quite an impressive U-turn from Dr. Spilker. I thought only politicians could pull these up
The real story turns out to be, apparently, that Spilker stated so forcefully to Ms. Lakdawalla that the Cassini science team was certain that "The vents are not the source of the E Ring" that Ms. Lakdawalla jumped to the conclusion that the team had actual chemical-composition evidence to that effect. After which I jumped to the conclusion that she must have actually drastically misquoted Spilker in that line. In short, we both jumped to false conclusions as a result of the Cassini science team jumping to its OWN (seriously dumb) false conclusion immediately after the flyby, and then reversing it later.
I agree that the articles on the planetary society site are excellent. I hope to see many more like them!
It's good to see that whatever misunderstandings took place along the way, the facts (for lack of a better word to describe our present knowledge) are coming to the forefront.
I will definitely go along with that. (I'll also go along with the statement that Ms. Lakdawalla's Planetary Society articles -- despite that one mistake -- have been excellent, and extremely useful to me personally.)
Now, then. Since it does seem highly probable that the E Ring particles are being expelled by Enceladus' vents, what are we to make of the sudden dramatic eruption observed by Cassini during its final approach to Saturn, which doubled the E Ring's total vapor mass for a few weeks before it dropped back to normal? We seem to have, just from this incident, proof that the vents are not just trickling out vapor at a very low constant rate, with the E Ring particles having a very long lifetime. Is the team looking for evidence in the Enceladus photos of a very recent venting event? It would seem the logical thing for them to do.
I wholeheartedly agree with your sentiment, Emily. But we have to face the fact that we live in the world of the sound bite, the news cycle, and the MTV attention span.
Those of us who enjoy news of planetary exploration generally have longer-than-average attention spans and an ability to retain interest in a subject for longer than a single news cycle. But, more and more, I've come to the conclusion that we're the exceptions. Of course, we have resources like this forum with which to supplement what the organized media offer, and without it I think most of us would be going slowly insane...
As for my own two cents -- I'm glad to have both you and Bruce as contributors to this forum. I know that, even though you both write for special-interest publications, you have to keep your professional work at a certain level. Whereas here, y'all can get as detailed and as esoteric as you want, and anyone who wants any further background to help them understand just asks for clarification. It's refreshing and vastly more satisfying (to me and, I suspect, to a lot of the people here) than any other newsgroup, chat group, forum or single publication could hope to be.
-the other Doug
I didn't know Emily Lakdawalla became a member
Glad to have you join us.
A view of Enceladus cracks.
http://img338.imageshack.us/my.php?image=enceladocracks3d5zs.jpg
Great work!
Two new notes on the E Ring from the new "Dust In Planetary Systems" abstracts ( http://www.lpi.usra.edu/meetings/dust2005/pdf/program.pdf ):
(1) In absract #4047, Cassini's CDA "found that the particles predominantly consisted of water ice (manifesting itself in the TOFMS as hydronium ions, with varying numbers of water molecules attached) and minor silicate impurities." If the E Ring particles really are made of water vapor spewed out of Enceladus' vents and then refreezing, where did even those small amounts of silicates come from? Is the speed with which material is sprayed out of the vents fast enough to propel small bits of Enceladan rock to the moon's escape velocity? Or...
(3) ...Is it possible after all that the E Ring does consist of material blasted off Enceladus by meteoroid impacts? Paper #4059 reports the results of simulations based on the assumption that this is the cause, with Enceladus and Tethys as the only sources -- but, once again, it never provides any explanation of why meteoroids would only spatter material off those two moons and not the others. One interesting note, though: in these simulations Tethys provided fully 30% of the E Ring material -- "a dust supply necessary to explain the large extent of that Ring and also the additional density hump near Tethys' orbit seen in ground-based [Keck] observations."
Maybe we're seeing a snapshot in terms of the E ring -- in other words, maybe it usually consists of mostly water ice derived from Enceladian venting, and it's been recently enriched with silicates from an impact at Tethys? As time goes on, the water ice will continue to be replenished, while the silicates might sort out?
I'm just trying to point out that we tend to observe things and assume that they're in some type of steady state -- not changing much over time. Perhaps we're seeing the E ring in a far different state than it was, say, 30 years ago, and that it'll be in a different state in another 30 years....
-the other Doug
Damned if I know. It would seem to contradict Occam's Razor; but then, if you shave often enough with Occam's Razor it occasionally cuts you.
In any case, any explanation of the E Ring must explain that huge eruption Cassini saw 5 months before its arrival at Saturn that doubled the E Ring's vapor mass instantly -- and then completely faded away in a few weeks. Either that was one hell of a big impact on something, or one hell of a big eruption of material from Enceladus (or Tethys). Which is more likely? The latter, I suspect.
WOW! Nice Update!
North and South Polar projections.
http://ciclops.org/view_event.php?id=27
Jason - are you trying to say something about this fair isle ![]()
http://ciclops.org/view.php?id=1381![]()
Nice pic from Modis on either Terra or Aqua though - I have one a bit like that, but a bit clearer - printed really large on my wall - you can make out Leicester quite clearly - and infact you almost can on that tiny version of it ![]()
Doug
Well - I recognise the colour and the size as being from MODIS on either Terra or Aqua for sure...
http://rapidfire.sci.gsfc.nasa.gov/ is their website, and it cant be TOO hard to find, after all - how many years must you wait for a clear view of the UK from orbit
- The Gallery is nicely present imagery, the real-time is raw - usually about 2hrs delayed.
Ahh - found it..
http://rapidfire.sci.gsfc.nasa.gov/gallery/?2003107-0417/NorthSea.A2003107.1200.2km.jpg
Whadda you know -it's a composite of imagery from both Terra AND Aqua ( I think Terra orbits at abour 1200 local, and Aqua about 2 hrs later ) - to get the width they wanted in the one day.
http://modis.gsfc.nasa.gov/gallery/# has imagery as well
Not sure if you coult botch something together from multiple images to make the whole USA
http://rapidfire.sci.gsfc.nasa.gov/gallery/?2004116-0425/UnitedStates.A2004116.2115.2km.jpg (West)
http://rapidfire.sci.gsfc.nasa.gov/gallery/?2003304-1031/Maine.A2003304.1535.1km.jpg (East)
http://rapidfire.sci.gsfc.nasa.gov/gallery/?2003295-1022/UnitedStates.A2003295.2040.2km.jpg
(Central)
Doug
I assume most of you are familiar with this one:
http://earthobservatory.nasa.gov/Newsroom/BlueMarble/BlueMarble.html
Unfortunately no political boundaries but this site has the entire Earth at 1 km/pixel resolution.
Check out the series of posts on my blog on today's announcements. I have one more up my sleeves for today. Just amazing, the tiger stripes may only be a few tens to a thousand years old.
http://volcanopele.blogspot.com/
After this, I take for granted not only that the Enceladus-3 flyby in 2008 will probably be modified, but that there are going to be LOTS more during the Extended Mission.
Something else that would be useful would be long exposure images taken as often as possible, say once a day, from any distance, in the hope of catching a plume in action. Restricting a plume search to the occasional non-targeted approach is probably not enough.
Phil
I presume that what Jason meant.
Tiger Stripes articles:
http://www.spacedaily.com/news/cassini-05zzz.html
http://www.spaceflightnow.com/cassini/050830enceladus.html
More tidbits from "The Independent" ( http://news.independent.co.uk/world/science_technology/article309205.ece ):
"An analysis of its atmosphere revealed it was about 91 per cent water vapour, 3 per cent carbon dioxide, 4 per cent nitrogen or carbon monoxide and about 2 per cent organic molecules...
"Candy Hansen, a Nasa scientist working on Cassini's ultraviolet instruments, said that half a ton of material a second was ejected from Enceladus's south pole, which would, over the four billion-year lifetime of the solar system, amount to a loss of 5 per cent of the moon's original mass."
In connection with the latter, is it not likely that a lot of the bizarre relief on the surface is wrinkle ridges?
I asked my question above before I saw http://saturn.jpl.nasa.gov/news/press-release-details.cfm?newsID=598, which begins, ' The Cassini spacecraft has discovered the long, cracked features dubbed "tiger stripes" on Saturn's icy moon Enceladus are very young - between 10 and 1,000 years young.'
Part of the problem is the terminology. "Tiger stripes" is ambiguous. It could refer to the fissures themselves (which is the way I've been thinking of them), or it could refer to the pattern of fresh crystalline ice. The opening sentence in that press release sure makes it sound like they're referring to the fissures, and not the pattern of deposition.
If the Cassini team really means the fissures are that young, I'd love to know the details.
It sure is hard to imagine that this decades-to-centuries resurfacing process could extend very far below the surface. Otherwise Enceladus would look like an icy Io -- those old craters in the northern hemisphere just wouldn't have been able to last this long. Sooner or later, some big melting event would have wiped them out.
We can presumably expect this whole thing to turn out to be immensely more complicated than is currently anticipated. (At least, we can hope it does.)
I sure don't anticipate it being simple!
One thing that's perplexed me since even before Cassini is not just the question of how such a tiny body can be so active, but how it can be so active over parts of its surface, and so old on others.
It almost makes one wonder whether it'd be worth trying to target Mimas for a close flyby if Cassini lasts long enough, maybe during a second extended mission, just to see whether there is any evidence of depositional "fuzziness" of the type we see in Enceladus' old terrain. That type of thing wouldn't necessarily have been all that easy to see during the distant flybys.
Although this seems extremely unlikely, wouldn't it be a hoot if "cold, dead" little Mimas turned out to have had some small amount of internal activity in the distant past? Although Mimas is smaller than Enceladus, it's not that much smaller, and it _is_ closer to Saturn. If Enceladus can be active to the extent we're now seeing, it's not that much of a stretch to think that this could at some time have happened to Mimas, albeit in a much smaller way.
Greetings,
I've increased the resolution of my Enceladus map to 8K and posted this on my website at http://laps.fsl.noaa.gov/albers/sos/sos.html#ENCELADUS. Still some tweaking to do (as always), but this should give a feel for what I've arrived at so far.
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