What's Happening at Aestuum?
Explanation:
East of Copernicus there is a cluster of 200-250 km wide roughly
circular mare patches (Vaporum, Medii, and Aestuum) that presumably occupy degraded
basins or craters. Mare Vaporum
has the strongest hints of circular structure, but the east side of Sinus Aestuum
(Bay of Billows, whatever that means) includes an arcuate series of mare ridges that
is also suggestive of a possible inner ring. The area inside the braided mare ridge
seems lower than the area outside it; perhaps the ridge traces a fault and the inner
part of the Sinus has subsided. The area inside is also rougher, with many apparent
small hills. But if you look at a higher res (but lower Sun) Lunar
Orbiter IV view, you'll see that the "hills" are really small craters. Many of
these craters are Copernicus secondaries, which are younger than any of the Aestuum
lavas, but the impression is that the lava within the mare ridges might be older
than that in the surrounding moat. Getting back to the braided ridge - it contains
at least two circular depressions that may simply be accidents of lighting and shallow
topography, but suggest collapse pits, which are rare on mare ridges.
—
Chuck
Wood
Technical Details:
Nov 20,2004. 250 mm f/6 Newtonian + 5X Barlow + Phillips Toucam Pro; 23 stacked frames.
Related Links:
Rukl Sheet 32