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Originally posted by arianna
reply to post by wmd_2008
Yes, all in good time.
With respect wmd_2008, why do you have to make snide comments instead of commenting on the subject matter. Your pompus attitude towards me in this thread and other threads is not helpful.
Originally posted by wildespace
Aha! The best image yet, M140237118RC (0.489 m/p resolution)
Sun is overhead, so almost no shadow, but the great resolution shows it to be nothing but a big rock.
Originally posted by SayonaraJupiter
Order in the Thread.
How did these rocks come to be located in the precise locations?
Originally posted by wmd_2008
Well since we have a resolution for the picture and using G.I.M.P or Photoshop image software guess what we can measure the ROCK its around 26 pixels at the widest point so that works out at around 12.7 mtr not as big as some would claim on here and certainly not a building.
Originally posted by arianna
The animation provided below is a closer view and I have arrowed some of the objects that are clearly recognizable as possible built structures. If you consider the features I have arrowed could not possibly be structures then what other explanation could there possibly be for these particular shapes?
Originally posted by arianna
reply to post by eriktheawful
Well erik, you provide the terrestrial image with reference information and I will apply the process.
BTW, could you possibly point out where the false data is in the animation or the enhanced image I posted as the enhacement is showing a much clearer view of the surface features which can be observed and verified in the contrast-adjusted original?
For purposes of this thread I would like it if we ALL could stick with original images that have been enhanced only by adjustments to brightness, contrast, and they may be cropped or enlarged. I hope you ALL will understand that ATS values the opinions of ALL it's memberships.
Hansteen rocks are different than most normal basaltic moon rocks. Check out: Hawke et al., JGR 108 (2003), E7,5069. www.spudislunarresources.com...
This region has rocks that are unusual in that they are made of dacite, which is much more silica-rich lava than basalt. Dacite is a superfine-grained form of granodiorite. Since there is less manganese and iron in the chemical makeup of silica-rich lavas, the silicate-molecule tetrahedrons aren't as bound up by metal ions, so the silica units cling to each other more. (At least that is the simple explanation I have in my head). As a result, the silica-rich lavas are lumpy and flow like toothpaste. The more basaltic lavas are more runny and flow like maple syrup. Dacite and the even more silica-rich rhyolite (superfine-grained granite) form steep-sided plug domes. The plug dome in Mt. St. Helens formed in the 1980's was dacite.
Other good candidates for silica-rich volcanic constructs on the Moon are : Marian domes, Oceanus Procellarum [41.4 N, 48 E]; Hansteen alpha, Oceanus Procellarum [12.3 S, 51 W]; Mons Gruithuisenen, Mare Imbrium [36.3 N, 40 W], and Compton-Belcovich Farside [61 N, 99.5 E].
If you poke around those areas, you'll also find some features that look like lumpy big-bouldered plug domes remnants. There is a great example of a big boulder pile just S of Beta dome in the Compton-Belkovic complex.