I heard about a peak on Iapetus that may be taller than Olympus Mons on Mars. I was wondering if the RADAR instrument will be used in the January encounter to verify this. What is the maximum distance the RADAR can be used?
I have an animation of this flyby. It shows what to expect during the flyby.
Let me know if you want this.
Please! Can you post it here?
It's 13.7 Mb
I think I would have to do a file transfer for that. Got ICQ or MSN?
ICQ# 6840999
In addition to the encounter on December 30, we can also look forward to the following encounters:
Nov. 2005 416,000 km (2.5 km/pixel, should show eastern Cassini Regio an d some of the bright terrain)
Jan. 2006 879,000 km (5.3 km/pixel, ring east of Cassini Regio, and eastern Cassini Regio)
Apr. 2006 603,000 km (3.6 km/pixel, southern leading hemisphere)
Sep. 10, 2007 1250 km (12 m/pixel, central cassini regio)
I did an animation showing 24 hours of the Iapetus flybys around the time of closest approach. It's fairly big (4 MB) but I could upload it temporarily to my website if there's interest in seeing it. However, it's not very impressive, it only shows Iapetus with a lat/lon grid, no instrument FOVs or observations are shown since needless to say I have no information on these. Needless to say I also have stills from the animation.
This is going to be an interesting flyby with images that should be better than the best Voyager 1 images of Rhea.
These three stills show Iapetus near the time of closest approach which occurs near 1900 UTC on December 31. This is a very slow flyby, the distance varies by less than 5000 km over the 8 hour interval shown here. The field of view is two times the field of view of Cassini's narrow angle camera.

WOW!!!
In the meantime two smaller Iapetus WOWs
:
http://photojournal.jpl.nasa.gov/catalog/PIA06146
and
http://photojournal.jpl.nasa.gov/catalog/PIA06145
How close will Cassini come to Iapetus during Tb?
Wow, those images got release quickly
I anticipated them getting released much later (like nearer to the Iapetus encounter).
A few notes: Note the giant crater near the terminator (EDIT: I see T.R. did mention that in the caption). Iapetus is definitely a battered, ancient world with no less than three giant impact basins on the order of Odysseus in size (relative to satellite radius). That impact structure is on the order of 550 km across ![]()
Here, BTW, is a look at those mountains by Voyager 2:
SO cassini will use Radar on this approach?
Before the last Titan encounter I noticed many raw images that were labeled as pointing at Iapetus almost missed or missed altogether. Anyone know what happened with those. Was there a problem with the pointing? Or were they looking for the dust from Phoebe that some claim as the reason for Iapetus's leading hemisphere being so dark?
the all seeing eye
http://saturn.jpl.nasa.gov/multimedia/images/raw/casJPGFullS06/N00025365.jpg
Will Cassini start to take some approach images soon?
I'm hoping to see that Huge Impact crater hiding in the Dark area Missed buy Voyager but seen in the Cassini Images.
Some early science results for Iapetus
In the same session at the Division of Planetary Sciences meeting, Bonnie Buratti of the Jet Propulsion Laboratory reported on the first Visual and Infrared Mapping Spectrometer measurements of Iapetus. The encounter was too distant for VIMS to be able to capture pretty pictures as the cameras did. In fact, Buratti got a laugh from the meeting attendees when she flashed her VIMS "image" up on the screen: a mere four pixels covered the entire moon. But she cautioned the scientists not to laugh so quickly. The VIMS image was "fortunate in outline," she explained. "One of the four pixels sits almost entirely in the bright region, and one in the dark region. So these represent the first resolved spectra of Iapetus."
Getting resolved spectra of Iapetus' bright material and dark material means that it's possible for a spectroscopist like Buratti to tell the difference in composition between the light stuff and the dark stuff, and begin to answer the question of how and why Iapetus can have two such different surfaces. The results surprised Buratti. "I may have to eat a lot of stuff that I've published in the past," she said. Looking at infrared wavelengths, she found carbon dioxide bound up in the dark material, just as was seen at Phoebe. This falls in line with the preexisting theory that the dark stuff on Iapetus could have come from Phoebe. But that's not the whole story.
"Phoebe and Iapetus are very different in the visible [wavelengths]," Buratti said. In those wavelengths, Iapetus' dark material looks more like D-type asteroids, which are reddish in color, "like Hyperion." Phoebe, by contrast, most closely resembles a more primitive C-type asteroid. Buratti tried to explain how these differences could arise within the Saturn system. "Exogenic small outer satellites," that is, small bodies that formed outside of the Saturn system and were later captured into distant orbits, "could provide additional material that's reddish in visible wavelengths," which would explain the D-type appearance of Iapetus. This hypothesis is reasonable, Buratti said, because "the small outer satellites do have reddish colors in the visible [wavelengths]." But she can't explain why the reddish coloration doesn't also show up on Phoebe.
http://www.planetary.org/news/2004/cassini_iapetus_1209.html
Help!!!!
I've been trying to view Iapetus from Cassini using this Webpage http://samadhi.jpl.nasa.gov/ Nothing I do makes this Webpage work?!?!
Everyone else seems to have no problem with it?!
What can I be doing wrong?
This is what I get.... http://space.jpl.nasa.gov/cgi-bin/wspace?tbody=806&vbody=-90&month=8&day=29¢ury=20&decade=0&year=4&hour=00&minute=0&rfov=30&fovmul=-1&bfov=30
Double post.
Strange, it works for cassini up to July 2, 2004 then I get your error message. I can see Iapetus from Dione after that. Maybe they didn't know its path after orbital insertion when they wrote the software?
New PICS!!
And this was from Dec 18! Man I can't wait!!!
http://saturn1.jpl.nasa.gov/multimedia/images/raw/casJPGFullS07/N25973.jpg
http://saturn1.jpl.nasa.gov/multimedia/images/raw/casJPGFullS07/N00025977.jpg
Wow!
Looks like only the dark side will be sunlit at closest approach. i guess we'll have to wait for the close up of the monolith
Looking at this map does anyone know what side will be imaged in Light and what side will be in the Dark?
http://www.monde.de/saturn-iapetus11b.jpg
I can't get JPL's solar sysyem simulator to work for Cassini after July 2 so I found another way to simulate the view. View from sun gives sunlit side
http://space.jpl.nasa.gov/cgi-bin/wspace?tbody=806&vbody=0&month=1&day=1¢ury=20&decade=0&year=5&hour=02&minute=45&rfov=30&fovmul=-1&bfov=30
view from saturn gives phase angle of 110 degrees.
http://space.jpl.nasa.gov/cgi-bin/wspace?tbody=806&vbody=6&month=1&day=1¢ury=20&decade=0&year=5&hour=02&minute=45&rfov=30&fovmul=-1&bfov=30
110-90=20 which should be longitude where terminator crosses equator on your map (sunlit to left)
View from Titan has phase angle of 95 degrees which is close to phase angle at closest approach (94 degrees) So the view from Titan should be close to what Cassini will see at closest approach.
http://space.jpl.nasa.gov/cgi-bin/wspace?tbody=806&vbody=606&month=1&day=1¢ury=20&decade=0&year=5&hour=02&minute=45&rfov=30&fovmul=-1&bfov=30
Would be simpler if they updated the simulato so you could use Cassini as the viewpoint after July
Actually the view from Titan is significantly different from Cassini's view since Cassini will be viewing the northern hemisphere. Page 1 in this thread has some renders I did showing Cassini's viewing geometry.
Beautiful work Bjorn. I guess this isn't very useful then
http://ringmaster.arc.nasa.gov/tools/viewer2_sat.html
should have noticed: last updated July 14, 2003
I had the terminator in the right place at least
Wow !
http://saturn.jpl.nasa.gov/multimedia/images/raw/raw-images-details.cfm?feiImageID=29377
The highest resolution image ever obtained of Iapetus...
There's a small bump on the limb just past the 3 o'clock position in that image of Iapetus - could that be one of the giant mountains we've heard about?
Upsidedown?
Three impact basins? On stretched image I see at 12 o'clock, one at 9 o'clock, is other at 3 o'clock? The mountain appears to be part of rim of impact basin at 9 o'clock.
Will Cassini get close enough to determine whether Iapetus has an asymmetric mass distribution?
I thought this moon was werid before, now its just flat out CRAZY!
I'm loving it! This moon looks like Rocky eye in Rocky!
Check this link out for some refreshed Voyager Maps using cassini data.
http://laps.fsl.noaa.gov/albers/sos/sos.html
Titan WOW!
Tethys
Iapetus
Also Europa was very nicly done!
Jason's stretched image makes it clear that Iapetus' irregular limb -- whioch ahs always intrigued me -- is due to the simple fact, that, for whatever reason, this moon has had the living hell bashed out of it. That largest impact basin looks like the hugely oversized craters that NEAR photographed on the asteroid Mathilde. Is it possible that -- as an abstract I recently saw suggests -- Iapetus is a captured moon, like Phoebe (and Triton)? This could explain its moderately tilted orbit.
Crazy idea: Iapetus was a larger differentiated object: dark outside, light inside; which was shattered by an impact. A large fragment, about one third of the original, was folded together by gravity into a spherical shape with the result looking similar to a baseball. This was later captured by Saturn.
Anyone try using an unsharp mask on the images of Iapetus?
Wish I had Photoshop. Looking on the web I see the term unsharp masking used two different ways. This is what I was referreing to.
http://voltaire.csun.edu/masking.htm
^ I wish I understood the question, I'm not that great at adobey.
What will that do to the image?
If it is done like in the link I referred to it will reduce the brightness range between the light and dark areas while keeping most of the details. It should make the features in the dark area easier to see. I don't have the software so I don't know if it will work in this case.
Iapetus with its three impacts looms larger and larger each day:
http://saturn.jpl.nasa.gov/multimedia/images/raw/raw-images-details.cfm?feiImageID=29430
Robert Schulz
nice. Looks likes the raw images page is about a day behind us. Tomorrow, there is a color sequence at 4.2 km/pixel.
My try at it..
Where did you get the tri-color data? Or did you just colorize the monochrome data?
I colorize the monochrome data.
As said before the Image is very compressed.
I would prefer a Tiff to play with.
Odd, there is very little approach images of Iapetus.
Why the wait for Raw Images?
2 Images in a week!?
Sorry Had to Vent.
I know.... as soon as yesterday's opnavs show up in the raw image page, I will post my color composites
I know.... as soon as yesterday's opnavs show up in the raw image page, I will post my color composites
They're up
http://saturn.jpl.nasa.gov/multimedia/images/raw/raw-images-list.cfm?browseLatest=0&cacheQ=0&storedQ=0
I've been seeing a faint linear feature along the equator on the raw images of Iapetus. I thought my imaginations was lining up random noise at first but this is the third day I've seen it. I wonder what it is. The large impact basin near the terminator looks like a multi-ring structure, it reminds me of Mare Orientlale.
Wow, and this is three or four days before closest approach! What is the highest resolution imaging Cassini will attain (on this flyby)? It has been said before, but with all the changes made, I am a bit confused.
So... what's going on? Is this a world-spanning ridge of giant equatorial cryovolcanoes that spew dark material onto the ice?
heres the fault in an earlier image look how high it is
http://saturn.jpl.nasa.gov/multimedia/images/raw/casJPGFullS04/N00022208.jpg
Operating on the 'see what sticks' principle-
Could the light material be some kind of polar deposit? The non-polar distribution could be related to historical changes in Iapetan obliquity.
Where is Iapetus equator in that image volcanopele?
I'm trying to get a bearing as where this is on the Voyager Global Maps.
How about this: Iapetus is hit head on by a centaur, that huge impact basin near the terminator looks like a likely spot. Some of the debris from the centaur ends up in a retrgrade orbit and lands on Iapetus's leading side.
Decepticon, I think the dark area is is centered on the equator, light areas in the latest images are on the poles.
Or maybe not
Volcanopele responded while I was typing
A giant grabbed hold of it and twisted it until it cracked and the insides leaked out of it. those aren't impact basis, they are his fingerprints.
This looks similar to the crater at the top center of the dark region
http://photojournal.jpl.nasa.gov/catalog/PIA01054
Cassini Page Update! Video Flyby.
Description of Iapetus flyby
http://www.planetary.org/news/2004/cassini_iapetus_plan_1229.html
From the Cassini website?
_____________________
Target: Iapetus - December 29, 2004
Next up for Cassini is a flyby of Saturn's icy moon Iapetus on Dec. 31. Iapetus is Saturn's two-faced moon -- one side is very bright, and the other is very dark. The spacecraft will pass about 65,600 kilometers (40,800 miles) of the frigid moon.
___________________
Has this not been updated to reflect the change in trajectory or has there been some other development that I have somehow missed?
Even at the current distance the Images must me Mouth Watering.
I just can't wait to see these Images!
My father says Iapetus looks like a walnut in yesterdays images.
(1) Ah. So, judging from the Planetary Society's description, radar scatterometry of Iapetus WILL be obtained during this flyby. (By the way, Jason, you never did confirm for us that Cassini missed some of its planned measurements -- including the radar -- during its recent Dione flyby, or explain what caused the problem.)
(2) It turns out that some researchers have been WAY ahead of us in noting both Iapetus' nonspherical, lumpy shape and the apparent implication that this moon has had the very devil knocked out of it at some point -- and that its whole developmental history has been radically different from that of Saturn's inner moons:
http://protostar.aas.org/publications/baas/v32n3/dps2000/329.htm
http://www.lpi.usra.edu/meetings/lpsc2000/pdf/1596.pdf
http://www.lpi.usra.edu/meetings/lpsc2000/pdf/1660.pdf
I remember going to the library to scope out every newspaper I could that might, just might have Neptune coverage. Then I would keep checking Science News. Then, at last, Sky and Telescope and Astronomy would have the latest. I am still an S&T subscriber. But I think it is an old habit - I haven't taken it out of the plastic-wrap in months!
Before the Internet Space News was very hard to get your Hands on.
When it did come out it was amazing stuff.
When Voyager passed Neptune PBS did a Live broadcast from JPL.
I was so excited.
I remember "Neptune All Night." I was 10 in 1989, and my parents made me stop watching a little past midnight to go to bed.
I was 14 years old during the neptune flyby. Triton was a gem of a moon.
To bad this encounter is not live.
At least we have the Huygens landing.
I'm looking forward to seeing the first Europa Subs with my son in the future. (I belive 100% of subsurface Oceans
)
I noticed something odd about the latest images of Iapetus: the shadows are wrong. The insides of the craters are dark on the sides closest to the poles and brighter on the sides closest to the equator when it should be the other way around. Is this caused by impacts redistrubing the light and dark material? How old would the dark material have to be to show this effect?
Mapping Coverage...
http://saturn.jpl.nasa.gov/multimedia/images/image-details.cfm?imageID=1265
http://www.jpl.nasa.gov/news/news.cfm?release=2004-300
Jet Propulsion Laboratory
December 30, 2004
I've noticed some interesting features near the poles I'd like a closer look at. Any chance of getting one before Monday?
If you look just at the rims of the craters the dark material continues almost to the poles.
Anyone else see a huge impact basin here? Or am I just imagining things in the noise?
http://s02.imagehost.org/view.php?image=/1148/impact_basin.jpg
it appears to be split apart by a rift
original image is here
http://www.nasa.gov/mission_pages/cassini/multimedia/pia06146.html
If it is, that is 1 HUGE Impact.
I'm having some doubts about it now. I don't see it in any of the Voyager images.
First set of Iapetus images are down. That is a HUGE ridge
Bright-dark dichonomy:
http://saturn.jpl.nasa.gov/multimedia/images/raw/raw-images-details.cfm?feiImageID=29520
OMG
I'm in shock! Amazing!
My first try at stiching. What you think?!
A colour try. Remember I'm new at this...
Decepticon, part of the dark area is gray rather than brown. Why?
http://img126.exs.cx/my.php?loc=img126&image=iapetus4ve.jpg
I love it when PTGui says the control points are "too good to be true"
Dark material looks like dust to me. Is it just me or does the edge of the light terran look polished to anyone else?
I was thinking looks like wind blown streaks must be dust. How do you get something that looks llike wind blown streaks with no atmosphere
Another theory:1)Iapetus had a subsurface ocean like Europa. 2) The equatoral ridge was present before the largest impact basin. 3)The impact compressed the other side of Iapetus driving the liquid out of the fissure at enough pressure for it reach escape velocity. The liquid freezes and darkens and is swept up by Iapetus.
Alan is thinking along lines roughly similar to mine. My own version: This utterly gigantic and incredible ridge seems to run smack through the middle of the dark region, and it looks like an enormous version of the double ridges crisscrossing Europa. Could it possibly be a gash out of which methane from Iapetus' interior gushed as gas before freezing back down onto the surface as methane frost -- which was then gradually darkened into dark organics by solar UV and Saturn's radiation (as is hypothesized to see the very dark patches we can already see on Pluto)? And could the few bright patches that seem to be sprinkled along the length of the gash ( http://saturn.jpl.nasa.gov/multimedia/images/raw/casJPGFullS04/N00022208.jpg ) be the few regions where water was extruded out of the gash and refroze AFTER the gash had stopped emitting methane?
Second wild speculation: that famous huge "dark ring" first seen by Voyager and now more clearly seen by Cassini ( http://www.nasa.gov/mission_pages/cassini/multimedia/pia06146.html ) turns out to just contact the outer corner of the main dark region -- and, as Alan said earlier, it looks like the lower outer floor perimeter of a gigantic crater with a raised hummock in the middle (like the Callisto crater at http://photojournal.jpl.nasa.gov/catalog/PIA01054 ). Could it be that, since this was where the methane cloud gushed from the ridge was just approaching its limits, the gas was able to flow along the surface in the depressed ring without coating the surface at the higher central hummock, so that it formed a methane frost layer which later became radiation-darkened in the "moat" around the central hummock?
What would happen to liquid (water, methane, ammonia) if was exposed on the surface of Iapetus? Would it vaporize explosively creating something like a pyroclastic flow? (cryoclastic?) Would this create steep sided mountains like Mt. St. Helens?
I looked at the images from the 27th again. What appeared to be wind blown streaks is probably a group of parallel ridges with dark material on one side.
"What would happen to liquid (water, methane, ammonia) if it was exposed on the surface of Iapetus? Would it vaporize explosively creating something like a pyroclastic flow? (cryoclastic?) Would this create steep sided mountains like Mt. St. Helens?"
Methane would, I think -- the moons of Saturn are still above its vacuum vaporization temperature. Water and ammonia almost certainly would not. What I'm thinking about that ridge is that -- as hypothesized for Europa's ridges -- it may be a region in which liquid water-ammonia mixture oozed upwards to the surface and then froze, later being pushed up by more liquid coming up from benetath it -- and that methane mixed with this, when it reached the vacuum at the surface, exploded outwards as gas. (It might indeed have contributed to pyroclastic phenomena around the immediate vicinity of the ridge -- or not, depending on forceful its release was. Alternatively, it might have vented outwards relatively gently.)
The ridge may have formed as the last remnants of a subsurface ocean frove. As the outsides of a pocket of water froze it would compress what remained in the center. It would squeeze out at a weak spot like a crack that already present.
The second batch is http://saturn.jpl.nasa.gov/multimedia/images/raw/raw-images-list.cfm?browseLatest=0&cacheQ=0&storedQ=0
^ Oddly I don't see them?!
Link?
You need to do a Ctrl-Refresh if using IE.
Oddly, the distances in the image 'captions' are incorrect, they seem to refer to the old trajectory which had a closest appoach of roughly 60,000 km. However, the closest approach was about 120,000 km. It's extremely frustrating that the exact image times are not given; in that case I could calculate the correct distance myself.
Thanks!
The might side Images are amazing!
This will help alot to map this moon out.
Bjorn have you been working on a global map for this moon?
Wow, I see five craters in the graylight images where the crust has sunk creating basins rather than rims.
http://saturn.jpl.nasa.gov/multimedia/images/raw/casJPGFullS07/N00026380.jpg
The "moat" and the curves leading from it were probably created by a broken object like Comet Shoemaker-Levy 9.
Look at those star trails. Excellent job tracking on those long exposures.
And another mountain at the edge of the dark terrain. I think there is a fault continuing from it into the light terrain. How far does that equatorial ring go?
A very quick-and-dirty Iapetus mosaic:
http://paranoid.dechengst.nl/saturn/Iapetus1.jpg
And yes it's dirty. One part has duplicate craters
Looks nice! I've been trying to do that all morning and I failed.
Every time I look at the dark side of Iapetus it gets even more bizarre. What I thought was a crater chain before now appears to be the end of a narrow wedged shaped sunken area. I see at least two other "craters" that have the same sunken area leading from them and a number of large cliffs.
Some the collaped areas have deposits of dark material just outside the top of the cliffs. I think the dark material was vented when they collaped.
I see lots of sunken areas, uplifted areas, fractures and cliffs on Iapetus except near the ridge. I think a subsurface ocean expanded as it froze causing the crust to stretch forming horst and graben in many areas. This didn't happen around the ridge because the slushy material was squeezed out through the fault releasing the pressure.
color images
http://www.planetary.org/news/2005/cassini_iapetus_firstimages_0101.html
Maybe this is superficial, but Iapetus is starting to remind me of the Uranian moon Umbriel. Particularly with the bright crater rim and whisps Umbriel has (and considering our coverage is limited to the southern hemisphere of Umbriel, there could be more elsewere). Of course, this could just be superficial.
I see some color variations in the large vrater on the left in this image. Are they real? If so are they different materials or just different lighting?
http://www.planetary.org/news/2005/images/iapetus1_lg.jpg
Some of the small craters in the light material on the trailing side have dark floors, the large ones do not, i see one midsized crater with a dark ring and light center. There could be a thin layer of dark material under the bright material on the trailing side.
I am favoring an endogenic process right now. I have never liked exogenic theories but when images showing an ancient dark terrain started showing up, I thought I was going to have to eat my hat. But all this discussion has reminded me that endogenic processes don't necessarily mean lava flows but could just mean pyroclastic deposits.
I wonder how tall that Crater wall is.
http://saturn1.jpl.nasa.gov/multimedia/images/raw/casJPGFullS07/N00026298.jpg
I hope Cassini gets some super High Res of that.
Also Can we expect more Images or thats it for the sweet stuff.
I found a diffuse patch in the nightside images. Could it be an active vent
or just an area sloped away from the light source.
http://s02.imagehost.org/view.php?image=/1157/diffuse_patch.jpg
I may have posted this before. It describes ice volcanos along the shore of Lake Superior
http://mivo-sys.tripod.com/cryo.html
I think I have a way to darken material on the sides of craters closest to the poles while leaving the opposite side bright. If it darkened by exposure to sunlight the sides that are shaded or are sloped away would be exposed to less and would remain bright. Another way to darken it may be exposure to the solar wind. Is Iapetus outside of saturn's magnetic field? Of course this doesn't exlain why its on the leading side only. It would be easier if the ridge ran all way along the equator on the leading side. Perhaps it is buried under debris from the large impact basin.
Redid the first mosaic and made a new one:
http://paranoid.dechengst.nl/saturn/Iapetus1.jpg
http://paranoid.dechengst.nl/saturn/Iapetus2.jpg
I read that Titans orbits is near the edge of Saturn's magnetophere so Iapetus should be outside ot it. I wonder what effect passing through the magnetotail would have.
Alan's latst theory, alas, will not work at all. First, both sides of Iapetus are exposed to sunlight equally often.
As for possible darkening by Saturn's radiation belts: this might be a conceivable explanation if Iapetus were within them -- although it would actually have to be LIGHTENING of the material on Iapetus' trailing side instead, since Saturn rotates faster than Iapetus revolves around Saturn, and so the charged particles dragged along by its magnetic field would be smacking into Iapetus' light-colored trailing side. Such radiation-induced color changes are, in fact, noted on the trailing sides of Jupiter's Galilean satellites, although they're very mild by comparison (they're due mostly to sulfur atoms that are expelled by Io, ionized and then dragged around Jupiter by its rotating magnetic field, smacking into the trailing sides of the three big icy moons). Nitrogen ions from Titan are likely to get rammed into the trailing sides of the inner icy moons of Saturn in the same way, although any color changes this produces are subtle. (I believe that Pioneer 11, by sheer chance, actually flew close enough to Epimetheus to detect the low-radiation wake which that moon, like all of Saturn's inner moons, plows in Saturn's radiation belts on its leading side.)
But Iapetus is actually far outside Saturn's radiation belts (indeed, Titan is only within them part of the time) -- and so this explanation won't fly either; just as both sides of Iapetus are equally exposed to sunlight, they're equally exposed to the solar wind. Whatever has colored one side of Iapetus, it's more than radiation exposure that has produced it -- although this still leaves the possibility that the dark material is methane frost on one side of it that has been darkened by exposure to solar UV and/or charged particles in the solar wind and in Saturn's long trailing nightside "magnetotail". This, as I said, is one of the leading explanations for the dark patches that are so dramatically evident on Pluto that we can see them even from here.
Bruce, I was using the varied exposure to sun light as an alternate theory to explain the brightness variations with latitude and in particular the brightness variation of the crater rims at highter latitudes which would naturally occur if Iapetus was orbiting through debris. I did mention that it didn't explain why it is on the leading side only.
Something I just thought about, if orbiting through debris would result it the craters near the poles having one dark rim and one light rim then the craters near the east and west edges should show the same effect but with the the variation being east/west rather than north/south. I don't see this is the night side images.
Made this using alans great stich job and Bjorn Lat/Log Map.
Looks like the guy who posts the raw images has sunday off. Anyone know if they have a press conference scheduled next week.
I zoomed one of the images of the leading side to look at the cliff. I noticed something odd: near the top there is a darker layer, yes darker than the rest of the dark terrain.
http://saturn.jpl.nasa.gov/multimedia/images/raw/casJPGFullS07/N00026259.jpg
Michael E. Adams of the Jupiter List has stitched together an absolutely superb mosaic of Cassini's Iapetus pictures: http://www.meawebdesign.com/space/iapetus_mosaic_bw.jpg . Unfortunately, when you magnify those craters on it, the resolution of the photos is not just not quite high enough to determine whether we're looking at central pits or at central peaks that have had the dark material slide down their outside slopes to expose light ice underneath. I'll have to review the craters seen on various other icy moons to determine whether any of them show central pits instead of peaks.
What we do see is unmistakable streaking of the dark material at the dark region's edges -- which really does look more like the pattern from ejecta than from methane gas, which I'd think would spread out more evenly. But the gigantic ridge does indeed run smack through the midline of the dark Cassini Regio -- so is this pure coincidence, or was the dark material indeed expelled from Iapetus' interior through the ridge? At any rate, we have here still further confirmation that the Solar System is dead set on continuing to surprise us.
I thought this crater looked strange. Seemed too unlikely that three imacts each smaller than the previous would hit the same spot.
http://s05.imagehost.org/view.php?image=/0624/iapetus_v2_81a.jpg
http://s05.imagehost.org/view.php?image=/0624/iapetus-v2-81b.jpg
Never mind about the geyser/volcanos I got confused by the bright sides of the large craters and forgot which direction the light was from.
It's rather easy to do that with this particular world I suppose tomorrow we'll all know a great deal more.
Was this area melted?
http://s04.imagehost.org/view.php?image=/1468/N00026259a.jpg
Looks kind of fishy to me
With Michael Adams' new stitch, turned in a different orientation than the ones we've been looking at, suddenly I find myself wondering if the dark stuff wasn't there first and the light material came in later! I can almost convince myself that at the interface area between the dark and light portions, the light stuff seems streaked into the dark areas. And many of the craters near the boundary have light material on the crater walls facing the light side of the moon. So couldn't that argue for the light material coming afterward??
Of course, that doesn't explain the ridge. That part of Iapetus looks like an almond shell or the seam on a (american) football!
More images have come up...
Some Great night side Images!
http://saturn1.jpl.nasa.gov/multimedia/images/raw/raw-images-list.cfm?browseLatest=0&cacheQ=0&storedQ=0
Here is a mosaic of the new crescent imagery. This is one amazing flyby! This was a fun one to assemble, though the large depression on the limb confused me for a while.
Give this a try: increase the brightness on one of the nightside images then rotate it 90 degrees. I can see lots of fractures running parallel to the equator when I do this. So many that I'm wondering if speculating that the entire dark side being an impact basin wasn't so crazy after all.
^ I tried but don't see it alan.
Got a example?
Try it with this one
http://saturn.jpl.nasa.gov/multimedia/images/raw/casJPGFullS07/N00026439.jpg
It needs to be brightened a lot before you can see anything. Look for the dark lines running sideways near the southern (curved) horizon, helps if that is at the top. They look like the tops of uplifted blocks to me.
Somethings weird is going on here
http://s05.imagehost.org/view.php?image=/0631/N00026245odd.jpg
Alan,
I'm a newbie here. What exactly is weird?
Chris
Its not just the "wind streaks" the craters looks odd. The have rings of light and dark material inside of them and the ejecta looks "wet" like the they formed in slushy material. One group of them is in a lobe of bright material. Some of the larger craters look like one of the rims is sliding downhill.
A couple of notes:
1) RADAR detected Iapetus. According to Arecibo results, the dark material and the bright material are indistinguishable, suggesting that the dark material is less than a radar wavelength deep (3 m or 13 m, not sure which Arecibo used). Should be interesting to see what Cassini RADAR found.
2) There is a press "activity" on Friday. Some good mosaics should be presetned then.
I think the outer rim of the largest impact basin is where the crust cracked and settled rather the rim of the crater. A couple of craters along the rim look like they are split or shifted as it settled.
http://s04.imagehost.org/view.php?image=/1485/N00026263Ro.jpg
What would happen if methane calthrate was erupted onto the surface? Would it be stable? I'm thinking if there were patches of it on the surface the methane could be released by impacts. This would settle in any holes that had formed in the dark blanket and darken with exposure to sunlight. I see this as a way to create fresh dark material after Iapetus cooled too much to drive volcanism.
A mosiac of sunlit cresent and the night side was posted here
http://www.markcarey.com/cgi-bin/mt/mt-view.cgi/18/entry/21706/discussion_page?start=41&show=20
I don't mean to be rude, but the new release http://photojournal.jpl.nasa.gov/catalog/PIA06166
is the worst version of that mosaic I have seen anywhere - the limb is entirely washed out. And several other images seem like very compressed jpegs compared to amateur versions, even though the versions I downloaded were .tiff files. I can understand a motive for releasing limited imagery in terms of not wanting to be beaten to scientific results by those not on the team. But with the images in the "raw" section being much better than the public release quality this time around, it seems to have little point. I fear the Cassini team is failing to understand the importance of "instant science in creating public interest in the mission.
I didn't mean to offend anyone. I just couldn't understand why the jpeg compression was there. Good to here it was just a mistake.
Ted
One complaint I have is the way the unsharp mask was done. I usually a smaller boxfilter size, usually less than 1 pixel. This greatly reduces edge effects.
Please tell me that JPL will use exposure times imaging on other moon flybys!?
This adds to images during each moon encounters.
Iapetus global maps will benefit a great deal using this method.
What do you mean by that? Are you referring to the images taken of the part of Iapetus in Saturnshine? Such imaging might be possible, but the spacecraft, at aphelion, was not moving very fast. For the other moons, this might prove difficult or impossible.
Ted
In addition to being more difficult because of spacecraft motion, Cassini will have many more non-targeted opportunities often not listed in lists of non-targeted flybys (100,000 - 250,000 km) to do gapfill on the moons inside Titan's orbit. The next closest Iapetus flyby other than the targeted flyby in 2007 will be this fall at ~415,000 km(Better than the nearly full view used in Jason's little icon (~700,000 km) but not nearly as good as this flyby. I wish I had a list of the flyby distances for major moons for all orbits, like we did with Galileo. But I guess that was a lot easier when we were only dealing with four major moons at Jupiter. Also, without Galileo's bottleneck, the Cassini people probably have a lot more observations to plan.
You would think this info would come out before each encounter!
Sadly its not.
VIMS and CIRS data for Iapetus has been released. Check out photojournal.jpl.nasa.gov
Jason, any word on the Dione VIMS data?
Ted
I find it interesting that the CO2 peaks at mid latitudes and has holes in it. Perhaps there is more than one type of dark material: a thick layer containing minerals from inside Iapetus concentrated near the equator, and a thin layer containing the CO2 from the outer moons like Phoebe that is more widely distributed.
I noticed Ted Stryk's excellent 12/2004 image in this post that I'll link here:
http://www.unmannedspaceflight.com/index.php?showtopic=4561&st=690&p=101828&#entry101828
I was wondering which PDS or raw images this was made from. Ted's processed image may be worth substituting over certain areas in my map if that's OK, or I could go to the original images. Is this from about 700000km out on approach? I'd be interested in any background info on this. For some reason these aren't showing up when I do simple searches on the PDS or the raw images page.
Might be fun to help complete this dormant thread. This is the approach image I'm http://laps.noaa.gov/albers/sos/saturn/iapetus/gridded/ortho15_gridded.jpg in the map. Is Ted's image a sharpened version of the one I'm using?
Thanks,
The images you probably want were taken on 2004-12-27, target is listed as UNK, not IAPETUS. Here's my quick take on the IR3/GRN/UV3 shot, desaturated to approximate natural colors and contrast-reduced to bring out CR:
http://i108.photobucket.com/albums/n15/ugordan/2004-12-27near-true.png
Yes. Same dataset. I applied a variant of Tim Parker's super-resolution technique to the images and made a color overlay.
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