File:Mare Orientale - C.jpg

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English: en:Mare Orientale straddles both the near and far side. The basin has the most nearly complete concentric ring structure of any basin in the west. The surrounding basin material is of the Lower Imbrian epoch, with the mare material being of the Upper Imbrian epoch. The outermost conspicuous ring is Cordillera, bounded inwardly by steep scarp or gentle lip and topped by some ridgelike massifs. The mare-like material to the northeast is Lacus Autumni. You can also make out the crater Maunder among the northern region of the mare. Off to the southeast of Maunder is Kopff. Montes Rooks lines the eastern edge of the mare.
来源 http://lunar.arc.nasa.gov/science/atlas/mare/morientale.htm (https://web.archive.org/web/20130221171721/http://lunar.arc.nasa.gov/science/atlas/mare/morientale.htm)
作者 NASA


Public domain 本文件完全由NASA创作,在美国属于公有领域。根据NASA的版权方针,NASA的材料除非另有声明否则不受版权保护。(参见Template:PD-USGov/zhNASA版权方针页面JPL图片使用方针。)
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当前2007年6月1日 (五) 01:072007年6月1日 (五) 01:07版本的缩略图350 × 382(20 KB)Bryan Derksen留言 | 贡献{{Information |Description={{en|en:Mare Orientale straddles both the near and far side. The basin has the most nearly complete concentric ring structure of any basin in the west.The surrounding basin material is of the Lower Imbrian epoch, with the

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