November 30, 2012
image by George Tarsoudis, Alexandroupolis, Greece
I was going to label this Golden Ash but then I thought that a lot is ejecta from Aristarchus. You can see the unambiguous ejecta splayed across Oceanus Procellarum to the bottom and the left. The ejecta are grayer than the ash, which was probably erupted from the Cobra Head vent of Schröter's Valley. The ash, normally called pyroclastics in more scientific descriptions, covers the Aristarchus Plateau (AP) and the high lands surrounding the Harbinger Mountains (HM) east of Prinz. The smooth, non-golden area between AP and HM is younger mare lava, erupted after the ash eruptions but before about 175 million years ago when Aristarchus formed, venering the lava with its pale ejecta. Notice the bipolar ejecta around the rim of Aristarchus - to the north it is dark, and to the south bright. Aristarchus formed on a boundary - the Plateau to the north and Procellarum to the south - and presumably the different colors of ejecta reflect differences in the composition of these materials - highlands vrs mare. Move away from the brilliant crater to the western edge of the Plateau. Gold coloration extends onto Procellarum lavas beyond the relatively straight edge of the raised Plateau - is that ejecta or ash? Splashes of brightness (secondary craters) on the lava demonstrate that at least some ejecta is there. Carefully calibrated multi-spectral images from the Clementine spacecraft nearly 20 years ago paint the ash as bright red, and the ejecta as brownish.The ash stops right at the straight western edge. It originally went further, but Procellarum lavas covered it, and later Aristarchus ejecta dusted it too.
Nov 26, 2012, 19:55-20:09 UT. Newtonian 10 inch @f/6.3, camera Unibrain fire-i 785, filters RGB, barlow 3X.
Rükl plate 18
21st Century Atlas chart 28.
Yesterday's LPOD: Bumps in the Night
Tomorrow's LPOD: Shadows Climbing Rims