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Originally posted by Bob Down Under
I can clearly see gigantic purple unicorns. They are so obvious to me, I have no idea why all these skeptics are missing it. I guess if you cannot see the unicorns, then saddly there is nothing to be done for you. Denying they are there is silly. Instead, try to explain what we might be seeing.
Let me say that that anomaly is NOT something on the surface of the moon. It is nothing real there on the moon.
lack of information = easy to imagine everything. (pareidolia)
The Hubble Space Telescope was used to gather high resolution multi spectral data of the moon's Aristarchus Crater in order to investigate the possibility of potential oxygen producing minerals on the surface. Identifying such minerals could aid in planning future sustained human missions on the moon. Initial analysis of the data indicate the likely presence of titanium and iron oxides. Both these minerals could be used as oxygen sources essential for human exploration.
This visualization starts with a view of the moon as seen from Earth using a USGS Apollo derived artist rendered texture (airbrushed). The camera then zooms into the Aristarchus Crater region. Simulated topography derived from Clementine data is used for relief and high resolution HST data is used for the area of interest. After investigating Aristarchus Crater, the camera then moves over to Schroter's Valley for a brief investigation.
Originally posted by easynow
Originally posted by easynow
just because you drew some lines on the picture doesn't prove there is nothing there. you also can't prove that it's an image artifact. your opinion does not make it a factoid.
Originally posted by easynow
look i already know the Anomaly does not appear in the other photos.
but that does not mean the Anomaly is an image artifact. you cannot prove it.
can i demosntrate there is 100% processing artifact? Never.
I don't understand why defend this picture, allegedly beeing something in the surface of the moon, without any serious reason.
Originally posted by Nohup
If you can't prove to me that aliens built these domes, then I'll have to go back to my first assumption, which is that they were built by leprechauns to mine their gold. Prove me wrong.
The Clementine 'natural' color composite mosaic (5 UVVIS bands available) is presented here for browsing by utilizing three of the five UVVIS multispectral bands, combined in red, green and blue channels of a color image (see table below). (Note: The composite image is not truly "natural color," but mimics natural color to the human eye.) This multispectral lunar mosaic is a radiometrically and geometrically controlled, photometrically modeled global image mosaic compiled using more than 400,000 images from multiple filter observations of the Ultraviolet/Visible (UVVIS) camera onboard the Clementine Spacecraft (Eliason et al., 1999).
Channel | Band | Description
Red | 1000 nm | Near Infrared
Green | 900 nm | Near Infrared
Blue | 415 nm | Ultraviolet
This '3-band' view is presented for browsing purposes. All five bands of the Clementine global mosaic are available when ordering data downloads of the UVVIS 'Natural Color' product.
The Clementine UVVIS Ratio ("false color") views of the Moon are created by creating ratio images using 3 of the 5 Clementine UVVIS camera bands and combining these into the red, green, and blue channels of a color image:
Channel | Ratio (band/band)
Red | 750 nm/415 nm
Green | 750 nm/950 nm
Blue | 414 nm/750 nm
The color ratio image product serves to cancel out the dominant brightness variations of the scene (controlled by albedo variations and topographic shading) and enhances color differences related to soil mineralogy and maturity. The lunar highlands, mostly old (~4.5 billion years) gabbroic anorthosite rocks, are depicted in shades of red (old) and blue (younger). The lunar maria (~3.9 to ~1 billion years), mostly iron-rich basaltic materials of variable titanium contents, are portrayed in shades of yellow/orange (iron-rich, lower titanium) and blue (iron-rich, higher titanium). Superimposed on and intermingled with these basic units are materials from basins and craters of various ages, ranging from the dark reds and blues of ancient basins to the bright blue crater rays of younger craters (e.g., Mcewen et al., 1999; Pieters et al., 1999).