

It looks alot like an excavator, or some watermill wheel.
Originally posted by Rilence
Now, what exactly caused those particular shapes to form, I have no idea at all, other than what I said in that they dont seem to be "natural"
Anything else you want me to take a look at ?![]()
Originally posted by johnlearAren't those ejecta rays a flat feature? The idea I have of it is that they are like a splash of mud, painting the ground with a layer of the material ejected from the impact.
Where did the rays go?
To add to the mystery in the Apollo 8 photo you can clearly see the city and the spaceport and all of the tubular structures.I can not see any "spaceport" or "city", but I think that the features you identified as "city" and "spaceport" are there, in the same place as they were in the other photo, just not that visible.

Originally posted by johnlearThey're probably full-time airbrushers with NASA.
Originally posted by SpaceBits
Hi, I'm new to this site,
This parking lot idea just doesnt seem to fit, prehistoric-phosile-fuled vehicles on the moon? The stucture resembles more to be some type of proccessing plant or maybe a geo-thermal plant... for what you might ask?
well the obvious of course which is WATER or H2O. the one substance not easily obtained in space.
originally by John Lear:
All of the evidence leads to greatlakes and Rilance being professionally sponsored.
but Rilence is as well! Cool, I never knew, hey what kind of salary does a disinfo agent get anyways these
days. Oh wait, according to John Lear and zorgon, I'm one, I should know!
hey rilence do you have those secret docs or do I?
quote: Originally posted by johnlear
We accept differing viewpoints on this thread as long as they agree with ours.
quote: Originally posted by johnlear
So here is the deal. If you would like to conduct a critical thinking class here on ATS you have every right to do so. But I respectfully request that you do not hijack this thread with pictures of milk drops telling us that that is what Aristarchus is. Thanks.

The Aristarchus plateau is a rectangular, elevated crustal block about 200 km across, surrounded by the vast mare lava plains of Oceanus Procellarum.
Clementine altimetry shows that the plateau is a tilted slab sloping down to the northwest, that rises more than 2 km above Oceanus Procellarum on its southeastern margin. The plateau was probably uplifted, tilted, and fractured by the Imbrium basin impact, which also deposited hummocky ejecta on the plateau surface. The plateau has experienced intense volcanic activity, both effusive and explosive.
It includes the densest concentration of lunar sinuous rilles, including the largest known, Vallis Schroteri, which is about 160 km long, up to 11 km wide, and 1 km deep. The rilles in this area begin at 'cobra-head' craters, which are the apparent vents for low-viscosity lavas that formed vents for 'dark mantling' deposit covering the plateau and nearby areas to the north and east. This dark mantling deposit probably consists primarily of iron-rich glass spheres (pyroclastics or cinders), and has a deep red color on this image.
). The Aristarchus impact occurred relatively recently in geologic time, after the Copernicus impact but before the Tycho impact. The 42 km diameter crater and its ejecta are especially interesting because of its location on the uplifted southeastern corner of the Aristarchus plateau. As a result, the crater ejecta reveal two different stratigraphic sequences: that of the plateau to the northwest, and that of the portion of Oceanus Procellarum to the southwest.
The infrared spectral properties measured by Clementine are consistent with a composition of almost pure anorthosite, the primitive rock type produced by the lunar magma ocean. This is the first discovery of a major exposure of anorthosite in this region of the Moon, well within the boundary of the hypothetical Procellarum basin.