
Ever since I first saw ‘Friends‘ back in the mid-1990s CE, I’ve wondered about the choice the writers made with Phœbe’s name. Is it connected with the moon’s name or not? If it is, it must be an extremely obscure in-joke because I imagine that most people had no idea what Phœbe was at the time, and of course the name is originally from Greek mythology, which raises the question of whether there was something about the titan herself which brought eccentricity or oddness to mind. Because Phœbe the moon is odd. It orbits the opposite way round to the majority of other moons in the Solar System, which is expressed in the stats as having a high orbital tilt, and Phœbe the ‘Friends’ character kind of does the same thing. She’s the odd one out and in the model of ‘Friends’ characters which approximates each to a personality disorder, she’s the schizotypal one. Not that I agree with that particular approach to personality disorders because they may be better characterised as combinations of unusually pronounced traits (which means that on the OCEAN model there could be thirty-two of them), but it’s been said a lot recently that there are various ways in which the sitcom has not aged well.
As is often so, Greek myths include several figures named Phœbe, but the moon is unequivocally named after the titan because it’s a satellite of Saturn and that’s how the naming scheme there went. That Phœbe is the grandmother of Artemis and Apollo, this last also known as “Phœbus” in Latinised form, who are respectively deities associated respectively with the lesser and greater luminaries. Hence it’s possible that naming a child Phœbe associates her with shining beauty, perhaps even a woman “with hair brighter than the Sun”. Phœbe’s daughter is Leto, alias Latona, goddess of night, chiefly known for being in labour for nine days owing to Hera keeping the midwife goddess Ilythia away from her when she birthed Apollo.
The question therefore arises as to why Phœbe the moon’s name was arbitrary beyond the order of its discovery leading to the need to seek decreasingly significant titans. This in itself raises an interesting question: does this mean that smaller Saturnian moons are more likely to have feminine names? If so, does that reflect a bias in classical times or more recently? This moon is the first to be discovered through photography alone, the second-largest retrograde satellite and as such is bumped down the scale of discovery, being likelier to be found later. It was first confirmed on photographic plates on 18th March 1899, the plates having been taken on the sixteenth of August the previous year. I find it a little surprising that it only took one night of plates to detect the moon’s movement and presume that it must’ve been quite far from maximum elongation at the time.
Just to return once more to the cultural aspects of this body, Phœbe is difficult to type on a computer. Although English, French and Latin all use the “œ” digraph, the letter isn’t present on the French AZERTY layout so far as I can tell, so on a typewriter it would have to be double-struck, and English lacks it entirely. I think of it as a letter in the French version of the Latin alphabet and it’s also used in the International Phonetic Alphabet with its French value. In Latin, the diphthong it represented shifted before the classical period into the sound /e/, and combined with our own vowel shift we now pronounce the moon’s name as “FEE-bee”, which incidentally also means we’ve conceded the shift from /ph/ to /f/, even though in classical Latin it would’ve been pronounced in the former way, at least for a while. In fact the only sound which has stayed the same in the name is /b/. I am, in any case, acutely aware of the fiddliness of typing the name as I’m writing this post
When I first heard about Phœbe in I think 1973, more than two decades before ‘Friends’ but millennia after the end of Dodekatheism, all that I and presumably most other people knew about it was that it was a small irregular moon, the outermost of Saturn’s, orbiting backwards compared to the other known moons, and was considered to be a captured asteroid. This last bit puzzled me because the asteroid belt is something like 750 million kilometres from Saturn. In the next few years, Chiron was discovered, and for a while this puzzled astronomers because it appeared to be an out-of-place asteroid. I will be talking about Chiron in a future post. Chiron, being named after a centaur, was just the first discovered minor planet of the “centaur” class, which I will eventually mention. There’s also Hidalgo, which is odd in that its aphelion is almost as far out as Saturn and its perihelion not so far from Mars’s, so it’s almost as if it belongs to both asteroid belts, as it were. But I’m getting ahead of myself.
Although Chiron was the first centaur to be discovered, in about 1977 I think, Phœbe seems to be a former centaur. This wasn’t picked up for getting on for a century since its discovery because they were otherwise unknown, but some of the characteristics of its orbit are highly compatible with this designation. Before I go any further, just as a centaur is a half-equine, half-human creature, astronomically centaurs are intermediate between comets and asteroids, which is also what Phœbe seems to be. The moon has an eccentricity of almost sixteen percent and averages almost thirteen million kilometres from Saturn. Since Saturn itself has an aphelion of 10.1238 AU, this means Phœbe reaches out to 10.2238 AU from the Sun. Chiron’s perihelion is actually inside Saturn’s orbit, so it’s entirely feasible to imagine Phœbe as a centaur.
While I’m at it, I may as well mention the other features of its orbit. It’s inclined to Saturn’s equatorial plane by 151° 47′, which actually just means it orbits backwards at a tilt of around thirty degrees, taking a year and a half to go all the way round. This distance also means it approaches Sinope, Jupiter’s outermost moon, to within about three and a half AU, which sounds like a lot, being slightly greater than the diameter of the orbit of Mars, but this is the outer Solar System where distances are increasingly larger than the inner. It’s about half a light hour. This is not a hugely consequential fact unless there were perhaps some kind of “moon-hopping” means of transport for getting between systems. There is of course The Solar Mass Transit System I mentioned a while back, but the gravity involved is insignificant. Nonetheless, out there somewhere is a neutral gravity point between the two, much closer to Sinope than Phœbe. That moon would also feel Jupiter’s magnetosphere most strongly out of any of the moon
I ask myself, is Phœbe genuinely the most distant of Saturn’s moons? Are there any bits and pieces in beyond it which still orbit it? Saturn’s Hill Sphere is bigger than Jupiter’s because it’s further from the Sun even though it’s also less massive, at sixty-one million kilometres in radius, which is almost five times the radius of Phœbe’s orbit. Nevertheless, matter is sparser out there than further in. And in fact there are fifty-five further moons, though some are extremely small. Some are only fourteen metres across, and it seems both hardly fair to include them as moons and also quite amazing that they’ve been detected at all. However, even the outermost moon is only half way to the surface of the Hill sphere, so it seems possible there will be even more. It’s thirty-four metres across and has no official name.
The moon is the largest of the so-called “Norse Group” of irregular satellites with retrograde motion. It’s over a thousand times the volume, ten times the diameter, of the next largest such moon, Ymir. Since it was discovered before the invention of this grouping, Phœbe has a Greco-Latin rather than a Norse name, Ymir being the frost giant nourished by the milk of the primordial cow and from whom the world was made in Norse mythology, thereby providing a possible link with Hinduism. There are probably a number of subgroups among the Norse moons. Among all of them, however, Phœbe is in a league of its own in terms of size, averaging about two hundred kilometres across, and as can be seen from the image at the top of this post, it somewhat approximates sphericality, more so in fact than the rather larger Hyperion. Other comparisons with Hyperion are worthwhile too. For instance, Phœbe lacks Hyperion’s spongy appearance and looks to me more like Deimos or a small asteroid. It’s also more massive than Hyperion, which is in fact connected to the appearance as it’s less porous too, and therefore denser. Phœbe is also as black as soot, reflecting only six percent of the light falling on it, which is darker than any other of Saturn’s largish or large moons. This would make it warmer than most of the other small moons which don’t experience substantial tidal forces, and certainly warmer than Hyperion, which is quite a bit paler and reflects a lot of light and therefore heat, being five times brighter than this moon.
Although there are maps of the place, it kind of makes more sense to label the “globe” because it’s too irregular to map without considerable distortion compared to a spheroidal object:

The craters are named after the story of ‘Jason And The Argonauts’, hence the very large crater called Jason at top left of this panel. This is more than eighty kilometres across and has walls sixteen kilometres high.
This moon is an exception to the exploration of the satellites undertaken by the Voyager probes. This is the best image taken at the time:
Hence research on the moon is rather behind that on the others. One thing which is noticeable about it is that it’s higher in dry ice than the others, which is one reason why it’s thought to be a centaur. It’s also the only such object which has been imaged as more than a dot, even by the Hubble Space Telescope. No space probe has been anywhere near any of the others, which basically means Chiron. It’s difficult, really, to talk about it without talking about the other, proper centaurs, which I want to leave until I get to Chiron.
Phœbe is unusual in having its own rotation period. Unlike Hyperion, whose rotation is chaotic, it does have a proper axis and takes nine and a quarter hours to rotate on it. This makes it the only sizeable moon of Saturn which has a proper day of its own, and Saturn will rise and set in its sky. Saturn is also usually in a position where its rings are fully visible, but unfortunately the planet is also very small and far-away.
Phœbe also has a ring, although unlike Rhea’s possible rings and the remnants of the one around Iapetus, if that’s what that is, it doesn’t encircle the moon but its orbit, through which the moon travels. It’s one of those irritating technical truths, like the fact that Alaska is the easternmost state in the US because of the Aleutian Islands crossing into the Eastern Hemisphere, that Saturn’s biggest ring is actually this one, which is so sparse as to be practically non-existent. It’s technically 23 million kilometres across, and may be the cause of the dark hemisphere on Iapetus, due to dark material leaving Phœbe’s surface and spreading inward as far as the two-faced moon. It’s probably caused by meteorites hitting Phœbe’s surface and the moon’s gravity not being strong enough to pull them back. It is, however, entirely within the moon’s orbit, suggesting that like the inner moonlets near Saturn’s more substantial and visible rings most of the way in, it also acts as a ring shepherd, although a particularly large one with a particularly diaphanous though large ring. Some of the larger impacts may also have caused bigger fragments to escape the moon’s pull and become other Norse moons in their own right, some of which have similar orbital characteristics.
That, then, is not only it for Phœbe but for the entire Saturnian system. Although most of the moons haven’t even been mentioned, these are all the moons discovered before the twentieth century. My impression of Saturn’s system is that it’s characterised by clutter. It has the rings, numerous small moons orbiting in unexpected places and a fair bit of matter exchange. It’s also quite light and of low density, with the exception of Titan. Due to being both quite massive, even given its low density, and far out in the system, it has a large sphere of influence and has managed to retain quite a lot of matter.
The next post on the Solar System will be about the initially mysterious and surprising object Chiron, discovered in 1977, and its “relatives”, the centaurs. These form a kind of second, outer asteroid belt. More on them in a couple of days.

