File:Mare Orientale - C.jpg

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描述
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.
來源 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 本作品由NASA創作,屬於公有領域。根據NASA的版權政策:“NASA的創作除非另有聲明否則不受版權保護。”(參見:Template:PD-USGov/zhNASA版權政策JPL圖像使用政策
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目前2007年6月1日 (五) 01:07於 2007年6月1日 (五) 01:07 版本的縮圖350 × 382(20 KB)Bryan Derksen{{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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