[HN Gopher] Differences between Moon's near and far sides linked...
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       Differences between Moon's near and far sides linked to colossal
       ancient impact
        
       Author : wglb
       Score  : 70 points
       Date   : 2022-04-11 14:31 UTC (1 days ago)
        
 (HTM) web link (www.brown.edu)
 (TXT) w3m dump (www.brown.edu)
        
       | prewett wrote:
       | The article doesn't seem to answer the question of why the heat
       | plume distributed stuff on the nearside rather than evenly, or on
       | the top side. If the south pole was hit, it seems like the heat
       | should flow evenly on both sides, and if anything case the
       | deposition to happen towards the north pole, rather than the near
       | side.
        
         | andrewflnr wrote:
         | Reading the linked paper and Wikipedia, it looks like the
         | center of the KREEP concentration is roughly antipodal to the
         | impact crater, which itself is not exactly on the south pole.
         | So at least the symmetry side of things is in order. But yeah,
         | this PR article is exceptionally bad at taking a long time to
         | say almost nothing of interest.
         | 
         | [0] https://www.science.org/doi/10.1126/sciadv.abm8475 [1]
         | https://en.wikipedia.org/wiki/South_Pole%E2%80%93Aitken_basi...
        
         | waynecochran wrote:
         | Yes -- that is what I was wondering. The following statement is
         | given with no explanation -- was Earth's gravity involved?
         | As the heat plume spread beneath the Moon's crust, that
         | material was eventually delivered en masse to the nearside.
        
       | akomtu wrote:
       | A wild speculation: perhaps Moon is the huge asteroid that hit
       | and liquefied the planet that was there before Earth, so some of
       | its material sticked to that asteroid and formed Moon, while the
       | rest formed Earth. In this case, the two sides of Moon show the
       | direction of the impact.
        
         | Sharlin wrote:
         | I mean, the prevailing theory _is_ that the Moon formed in the
         | aftermath of the Theia-proto-Earth collision. Indeed the
         | existence of the Moon is why the Theia hypothesis was proposed
         | in the first place. But the bulk of Theia's mass (which would
         | have been ~10% of Earth's mass) is thought to have mixed with
         | Earth's and sunk into the core /mantle, while most of the Moon
         | is made of same material as the modern Earth's crust.
         | 
         | However, the differentiation of the Moon's near and far sides
         | must have happened later, presumably during what's called the
         | late heavy bombardment ("late" is relative here; we're still
         | talking ~4 Ga ago). Although I believe some recent research has
         | cast doubt on whether the LHB actually happened at all.
        
       | JKCalhoun wrote:
       | I recently took an old-school "voxel" algorithm and munged some
       | NASA moon terrain data to try to create a game.
       | 
       | I really have enjoyed learning about the Moon's geography just
       | from flying around the terrain, picking locations for "lunar
       | bases" and such. Fascinating cracks and valleys, grooves, a
       | straight mountain range -- in general things I was not expecting
       | on a planetoid without water/erosion.
       | 
       | It really is stark how different the far side of the Moon is from
       | the near side. Insanely pock-marked with so many craters.... I
       | assumed there was an Earth component to that in the same way the
       | Earth has locked the Moon into an orbit/rotation that is always
       | facing us.
       | 
       | I'm become very keen to learn more about the Moon now.
        
         | Teever wrote:
         | Can you talk more about the moon data munging?
         | 
         | I just started some Blender tutorials and the first thing I
         | want to try once I get some tutorials under my belt import dats
         | from the Moon/Mars.
        
           | JKCalhoun wrote:
           | Sure.
           | 
           | For the Moon the (images) data seems to be bucketed with
           | regard to pixels-per-degree (PPD), the more coarse data set
           | being 64ppd data (finer resolution for the Moon goes at least
           | as high as 512ppd that I have found). Sadly, my workflow
           | (image editors, and Blender as you mentioned) are already
           | straining with the 64ppd data-set so I did not try to go
           | higher resolution. It means though that my Moon is wildly
           | small -- the lunar bases that seem to be a paltry 7x7 or 9x9
           | voxels are in fact the size of a small town.
           | 
           | I began with NASA's "CGI Moon Kit" [1] which, as I say, is
           | 64ppd. There is both a "color data" image and an "elevation
           | data" image (where the greyscale value of the image
           | represents elevation). Polar data was garbage (and would look
           | wildly distorted in my tile-based voxel algorithm so I
           | confess that I tossed it -- cropped everything outside
           | 60-degrees latitude basically - I just limit fuel in the game
           | to keep pesky kids from trying to get too deep into the polar
           | regions).
           | 
           | Even at 64ppd and poles cropped, I still ended up with two
           | images that were 23040 x 11264 pixels in size. This turned
           | out to be a challenge for most of the image editing apps I
           | have. Blender handled it (but barely).
           | 
           | With both color + elevation images I followed an online
           | tutorial [2] meant for cartographers wanting to use Blender
           | for relief shading. NASA's moon map had no shadows (probably
           | a good thing). I was not going to try to real-time
           | shade/light the voxel terrain so I settled on "burning in"
           | the shadows with Blender. While my MacBook ran some 8 hours
           | or so (over night) to generate the relief-shaded lunar map,
           | the result was quite nice. As a result, it is near sunset
           | everywhere on my Moon, ha ha.
           | 
           | With a relief-shaded image representing the color and a same-
           | sized image representing the elevation, I wrote a custom app
           | to read both files into memory and then generate the correct
           | number of 512 x 512 tiles that contain both the elevation
           | data and RGB data in a single raw file. Now I have 45 x 22
           | raw tiles covering the entire 64ppd Moon. The voxel algorithm
           | uses simple math to figure out which tile a given voxel is to
           | be found, reads the elevation/color data.
           | 
           | In hindsight, I could have output PNG files or something with
           | alpha channel (where alpha would be interpreted as
           | elevation). As it turned out, the Moon color was so close to
           | greyscale that I ended up treating it as such and used only
           | the green channel when creating my Moon tiles (so the tile
           | data has only a single 8-bit value for elevation and a single
           | 8-bit value for "color" per voxel -- cut the raw tile size in
           | half).
           | 
           | Still wrapping up the game [3]. I'll put the sources up on
           | Github end of the month, I think.
           | 
           | [1] https://svs.gsfc.nasa.gov/4720
           | 
           | [2] https://somethingaboutmaps.wordpress.com/blender-relief-
           | tuto...
           | 
           | [2] https://mooncraft2000.com
        
             | 127 wrote:
             | I did some cropping of the LOLA dataset to a .raw that
             | Unity3D could understand as terrain input:
             | https://github.com/amb/SplitTIFF ... a couple of years ago
             | 
             | Happy to hear any better alternatives for the task.
        
               | JKCalhoun wrote:
               | That is very cool. I starred your repo, if I try to up
               | the PPD I'll have a closer look.
        
             | bdefore wrote:
             | Fascinating. Are there upcoming plans from any space agency
             | to improve that 64PPD with upcoming or existing satellites
             | or Earth-based capture of moon topography?
        
               | JKCalhoun wrote:
               | There are 512ppd data sets [1] already. As I say, I found
               | them unwieldy with my workflow. A new workflow would be
               | required to process these into "game tiles".
               | 
               | [1] https://astrogeology.usgs.gov/search/map/Moon/LRO/LOL
               | A/Lunar...
        
               | bdefore wrote:
               | Whoops. I missed that you mentioned higher PPD is
               | available. If your workflow was improved to accommodate
               | it, I presume it would produce more, for lack of a better
               | phrase, life-like terrain? Would a much higher PPD be
               | required to reach a threshold to improve the experience.
               | And are there plans coming to get finer detail than
               | 512PPD?
        
               | JKCalhoun wrote:
               | It occurred to me that, beyond 512ppd, you could
               | "synthesize" higher-res detail. I don't know how much of
               | a cop-out that is though.
               | 
               | There may be >512ppd data though. IANAS (I am not a
               | selenologist).
        
         | gehwartzen wrote:
         | Becouse of the orbital lock it's interesting to think of it
         | like a shield for earth. I imagine a lot of those craters were
         | by asteroids that would have hit earth, esp the perfectly round
         | ones in the center. The oblong ones or ones towards the edges
         | might have come at an angle that wouldn't have hit earth. Seems
         | like a fascinating way to study earths impact history if we end
         | up exploring the dark side of the moon in more detail.
        
           | bdefore wrote:
           | I believe consensus is that the moon will eventually drift
           | away from the Earth. Do such impacts, predominantly on the
           | far side of the moon, apply enough force to change that
           | prediction? Are such projections of whether the moon leaves
           | Earth orbit (or instead collides with Earth) accounting for
           | this?
        
             | throwanem wrote:
             | The moon _is_ drifting away from Earth at a rate of about
             | four centimeters per year [1]. Inbound impacts on the far
             | side won 't significantly affect this because of the way
             | orbital mechanics works. To lower an orbital altitude, you
             | need thrust opposing the orbital vector. (This is why
             | spacecraft orient the way they do, with engines pointing in
             | the direction of travel, for retrofire.) Thrusting toward
             | or away from the orbital center of gravity (in this case
             | Earth) can affect the circularity of the orbit, but that's
             | all. In the case of the moon intercepting an impactor
             | that'd otherwise strike Earth, the thrust vector is
             | necessarily toward Earth, so the effect would be to render
             | the moon's orbit infinitesimally more elliptical, with the
             | increase along the major axis balanced by an equally
             | minimal decrease along the minor axis. (To the extent the
             | force vector of the impact is displaced from the axis
             | through the moon's own center of gravity, that will affect
             | the spin of the moon, but not its orbit.)
             | 
             | According to the linked article, it will take about fifteen
             | billion years for the moon to escape Earth orbit entirely.
             | I haven't checked, but I believe that's considerably longer
             | than it is expected to take for the Sun to expand as a red
             | giant and render Earth uninhabitable. Certainly more
             | wondrous than either event would be for anything then
             | living to remember having once had distant ancestors who
             | called themselves "human"...
             | 
             | [1] https://www.google.com/amp/s/public.nrao.edu/ask/what-
             | happen...
        
               | bdefore wrote:
               | It's compelling to me that the Earth and its moon are so
               | tightly linked that their relationship is projected to
               | outlast a life-providing sun. I believe this is moreso
               | than any other moon-planet pairing in the solar system?
               | Given what we know of incoming asteroids and comets, the
               | probability of their impacts hitting with enough force at
               | a trajectory you describe with enough significance to
               | change the moon's orbit is expected to be low . And we're
               | relatively confident of that?
        
               | throwanem wrote:
               | I don't have numbers or references here, but my intuition
               | from a lifetime of space nerding is that, if the moon
               | were struck with enough retrograde force to materially
               | lower its orbit, in the _best_ case that impact would
               | liberate debris of mass and vector such that our first
               | concern would be planetwide disaster response. (In the
               | worst case, it might shatter the moon entirely and
               | distribute a significant fraction of its total mass
               | across Earth 's surface; in such a scenario, the survival
               | of eukaryotic life anywhere on Earth qualifies as a
               | million-to-one-shot win.)
               | 
               | But the odds of such a collision I suspect are
               | significantly lower even than of a similarly sized
               | impactor striking Earth. Granted that the moon helps a
               | great deal in sweeping space near Earth of objects that
               | might otherwise enter our atmosphere, but something with
               | the kind of kinetic energy it would take to produce these
               | outcomes isn't going to spend long enough within the
               | gravitational influence of the Earth-Moon system to be
               | significantly affected before impact. It'd be like trying
               | to swerve an ICBM warhead by blowing really hard on it,
               | and I choose that simile with care - if this ever _does_
               | happen, I think it might constitute a clear indication
               | that someone somewhere in the universe really hates us!
        
           | JKCalhoun wrote:
           | I also am fascinated by the idea of Nemesis [1] -- an
           | infrequent event that causes mass-impact throughout our solar
           | system.
           | 
           | [1] https://en.wikipedia.org/wiki/Nemesis_(hypothetical_star)
        
           | bdefore wrote:
           | Do we have an idea of what percentage of impacts were
           | prevented this way? What likelihood is there that the moon
           | saved humanity (more than once?) since the time that we
           | descended from the trees?
        
             | gehwartzen wrote:
             | I imagine once you figure out which craters correspond to
             | ones that came in at an angle which would have hit earth
             | and compare that to all the impacts you have had on earth
             | one could figure it out.
             | 
             | The thing is that on the moon the craters remain visible
             | for a much longer period of time while on earth they get
             | covered up by plate shifts, erosion, ocean impacts, etc. So
             | instead it might be a way to calculate how many asteroids
             | likely have hit earth in general throughout history whether
             | we have found the craters on earth or not. Then you could
             | calculate based on the size of the craters on the moon
             | which ones would have been earth catastrophic events
             | (taking into account any diminishing impact energy due to
             | our atmosphere). Which would tell us how many the moon
             | saved the earth from. In terms of how many since human
             | ancestors were evolving we would have to then date earth
             | catastrophic craters on the moon. I'm not sure if this can
             | be done through photographs or if we would have to get
             | surface samples.
             | 
             | Then comparing that number to the fraction of earth
             | covered/protected by the moon to the total area on earth we
             | would have a decent idea of how many of these events
             | happened one earth even if we haven't discovered the
             | evidence for them on earth.
        
       | getpolarized wrote:
       | There's a MASSIVE impact crater on the far side of the moon which
       | we never see.
       | 
       | Imagine if it was inverted. It would look like a MASSIVE eyeball
       | staring at us during our evolution.
       | 
       | Imagine how that would have impacted religion!
        
         | [deleted]
        
       | mageofpanthera wrote:
        
         | wishawa wrote:
         | This comment sounds AI-generated. If you're a real person can
         | you explain the point you were trying to deliver and why you
         | chose to write this way?
        
           | mageofpanthera wrote:
           | Machines do not have narrative-interpretation bugs associated
           | with Superiority Complex, humans do, Arthur.
        
           | klyrs wrote:
           | I've met some old-school hippies who actually talk like that,
           | and appear to completely believe the pseudoscience.
        
             | xen2xen1 wrote:
             | You mean self importance?
        
             | mageofpanthera wrote:
             | Oh, I remember that word now: "pseudoscience"; it used to
             | be regurgitated everytime someone stepped into a pool of
             | reality-altering facts. They never manage to pin down the
             | 'pseudo' or the 'science', or contribute (like old-school
             | hippies) anything to the collective.
        
               | klyrs wrote:
               | Yeah, but sell a finger for the price of a lid, and your
               | hippie suddenly believes in concrete facts, scientific
               | measurements and capitalism...
        
           | bdefore wrote:
           | Is that what happened here? My head went in a few orbits over
           | this comment.
        
             | [deleted]
        
       | h2odragon wrote:
       | > The nearside is home to a compositional anomaly known as the
       | Procellarum KREEP terrane (PKT) -- a concentration of potassium
       | (K), rare earth elements (REE), phosphorus (P), along with heat-
       | producing elements like thorium. KREEP seems to be concentrated
       | in and around Oceanus Procellarum, the largest of the nearside
       | volcanic plains, but is sparse elsewhere on the Moon.
       | 
       | Bait. Big pile of things we want, placed where we can see them
       | but not easily reach...
        
         | sfblah wrote:
         | I thought Kazakhstan produced the best potassium.
        
         | JKCalhoun wrote:
         | Indeed, the Moon is a harsh mistress.
        
       | rhplus wrote:
       | _Why the two sides are so different is one of the Moon's most
       | enduring mysteries._
       | 
       | How much can be explained by the earth shielding the moon from
       | impacts to its near-side?
        
         | spaetzleesser wrote:
         | That's what I was thinking. Or that the earth gravity would
         | cause tidal forces.
        
         | vikingerik wrote:
         | Not much. The Earth subtends a width of only 2deg in the Moon's
         | sky - it covers only about 1/10000 of the possible approach
         | vectors to the Moon.
         | 
         | Think about a lunar eclipse for comparison: the Earth
         | intercepts the Sun-Moon vector for a couple hours every few
         | months, roughly 1/10000 of the time.
         | 
         | The Moon is a smaller target (1/4 the diameter, 1/16 the cross
         | section, also 1/81 the mass and gravity), so it gets hit less
         | because of that, but not because of Earth shielding it.
        
           | cperciva wrote:
           | I don't think that calculation is quite right. An asteroid on
           | a collision course with the moon doesn't need to _hit_ the
           | Earth in order to avoid hitting the moon -- simply coming
           | close to the Earth will alter its course.
        
       | uncertainquark wrote:
       | This is yet another (most welcome) hypothesis in explaining the
       | sheer differences in our Moon's nearside and farside. Just last
       | month I wrote a feature article explaining the other leading
       | theories for what caused these nearside-farside differences if
       | anyone's interested: https://blog.jatan.space/p/the-two-faced-
       | moon
       | 
       | The Moon is so much more interesting than most people think.
        
         | frankohn wrote:
         | I was wondering if a possible explanation is that, due to the
         | gravity attraction of the earth, the hot, heavy, inner part of
         | the moon, which is richer in heavy elements, I guess, like iron
         | is closer to the near-side surface. Since in the far-side the
         | hot, heavy part is too far from the surface the eruption
         | activity is small or non-existing.
         | 
         | Because the moon is tidally locked to the earth the pull always
         | act in the same direction.
         | 
         | I was imagining the moon as a drop of liquid in the vacuum
         | space with a denser core at the center. The heavier core would
         | be at the center because of the moon's own gravity. In the
         | presence of the earth's gravity the denser part of the "liquid
         | drop" will be centered more closely to one side and so the
         | volcanic activity would be strongly biased.
        
           | OscarCunningham wrote:
           | For the same reason there are two tides, you would expect the
           | drop to be pulled towards Earth, but also thrown out away
           | from Earth.
           | 
           | https://en.wikipedia.org/wiki/Tidal_force
        
             | frankohn wrote:
             | No, because the moon is tidal-locked to the earth so the
             | pull is always in the same direction. Tidal-locked means
             | the moon always show the same face to the earth.
        
               | CorrectHorseBat wrote:
               | Won't there be centrifugal pull (push?) on the other
               | side? Just like there is tide on the moon side and on the
               | other side
        
               | false-mirror wrote:
               | You're referring to the fictitious centrifugal force [0]
               | which is actually a minor change in inertia--very much
               | out shined by the centripetal force of gravity. For
               | example, on earth if you weigh 200 lbs on the North Pole,
               | you'd weigh about 199lbs on the equator. On the moon,
               | this tiny effect would be wiped out by gravity.
               | 
               | [0]:https://en.wikipedia.org/wiki/Centrifugal_force
        
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