July 23, 2019
Guess what the 'greenish-yellow' stuff is.
A: Impact related lava flows in Lunar Craters?
B: Sand dunes in windswept craters on Mars?
C: Stromatolite colonies in brine pools in Australia?
It's even better than pancakes!
The pictures of the Mercurian arctic were taken by N.A.S.A's Messenger spacecraft before its demise. According to the phys-org article there was initially some considerable skepticism that they were what they appeared to be. However, Arecibo Observatory has now confirmed that these are big piles of ice; actual glaciers. There's no mention in the article what phases the ice is (presumably 1-4).
The sheer scale of the ice deposits is remarkable The big, half filled crater in the foreground, Prokofiev, is 69 miles across. Just eyeballing it, the nearly full craters, behind it, Kandinsky, Tolkien, Tryggvadottir, and Chesterton, are about 20 to 40 miles across. If Tolkien has a radius of 15 miles, then Ï€â€‰r2 gives us a bit less than 707 square miles of ice for that smallish crater alone. How many cubic miles depends , of course, on the thickness, but that's a hell of a lot of ice. and remember, that's just one crater, and that's just the glacier, not the buried frozen mud and such.
What's remarkable is how far from the north pole the ice deposits seem to extend. They seem to exist south of the arctic circle. Presumably these are DEEP craters.
Now, one might ask, if Mercury (which is right next to the fricking sun and is hot enough to melt lead in its tropics) has actual glaciers, why doesn't the moon, which is much farther away have such spectacular ice deposits?
A trio of researchers at the University of California has found evidence that suggests there is far more ice on the surface of the moon than has been thought. In their paper published in the journal Nature Geoscience, Lior Rubanenko, Jaahnavee Venkatraman and David Paige describe their study of similarities between ice on Mercury and shadowed regions on the moon and what they found.
Indications of water had been detected in craters on the Moon, and Scientists have long suspected that there are ice deposits in the shadowed craters of The Moon and Mercury, which have almost no axial tilt. Those polar craters, being in permanent shadow, are invisible from the ground here on Earth. However, while satellites passing over the lunar poles have detected indications of ice, they haven't actually looked down into the craters on the moon with the same instrument that Messenger used to get these pictures of Mercury. So they didn't confirm what form the ice is in. It was always assumed to be something akin to permafrost with a few frozen puddles and some ice sheets. . However, all the other data from the lunar craters is consistent with what's been seen on Mercury, so it looks like there's probably a similar situation there, meaning much more ice than previously thought, and possibly in glacial form. Heretofore, studies have focused on ways to "cook" water out of the regolith.Well, having GLACIERS would rather simplify matters.
This means we need to get one of those particular cameras into lunar polar orbit to confirm this, and if this is true it has immense potential to facilitate lunar settlements.
Of course this also means that not only The Moon, but Mercury (of all places) are potentially much easier to settle. Mining in space to bring things to Earth does not make any economic sense normally, but Mercury is a likely mother load of heavy elements like tungsten, gold, platinum group metals, and radioactives. The PGMs in particular could potentially make mining operations on Mercury worthwhile in a few decades.
All that aside, I just find it transcendentally cool that there are actual glaciers on planet Mercury.
UPDATE: Antarctic too!
These results support the observation that Mercuryâ€™s south pole has a substantially higher volume of frozen water ice and other volatiles than Mercuryâ€™s north pole
Note though, that this is not a direct radar photo like the one above; just an indication that there is ice and other radar reflective substances present. It's not clear what form they're in and it is certainly not a given that these deposits are the same sort of hectometer thick ice sheets seen in the above pictures of the northern glaciers, though it would seem likely that at least some are.
Posted by: Pixy Misa at Tue Jul 23 21:33:05 2019 (PiXy!)
Posted by: Mauser at Tue Jul 23 21:48:27 2019 (Ix1l6)
Posted by: MadRocketSci at Tue Jul 23 21:56:42 2019 (K+Kza)
Posted by: MadRocketSci at Tue Jul 23 21:58:04 2019 (K+Kza)
Posted by: MadRocketSci at Tue Jul 23 22:20:47 2019 (K+Kza)
Posted by: Pixy Misa at Tue Jul 23 22:26:34 2019 (PiXy!)
Posted by: David at Wed Jul 24 01:20:14 2019 (7VRIY)
Mercury is surprisingly hard to get to...
Indeed. However, once one is there it is easier to get back from than one would assume of something so far down the sun's gravity well. You see, its orbit is so fast that it acts like an additional rocket stage, so theoretically, mass drivers on Mercury could sent a constant stream of metals earthward without too much cost or difficulty once sufficient infrastructure had been built up.
Posted by: The Brickmuppet at Wed Jul 24 06:14:30 2019 (YUAc9)
So these are all at the north pole
Posted by: The Brickmuppet at Thu Jul 25 05:35:11 2019 (YUAc9)
Posted by: Pixy Misa at Thu Jul 25 22:57:14 2019 (PiXy!)
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