翻訳と辞書
Words near each other
・ Clavilux
・ Clavinet
・ Clavinova
・ Claviola
・ Clavioline
・ Claviorganum
・ Clavipalpa
・ Clavipalpula
・ Clavipalpula aurariae
・ Clavipectoral
・ Clavipectoral fascia
・ Clavipectoral triangle
・ Clavis
・ Clavis Patrum Graecorum
・ Clavisybra strandiella
Clavius (crater)
・ Clavius Base
・ Clavivox
・ Clavières
・ Clavocerithium
・ Clavocerithium taeniatum
・ Clavogaster
・ Clavomphalia
・ Clavoserixia bifasciata
・ Clavosurcula
・ Clavosurcula schepmani
・ Clavosurcula sibogae
・ Clavulanic acid
・ Clavularia
・ Clavularia crassa


Dictionary Lists
翻訳と辞書 辞書検索 [ 開発暫定版 ]
スポンサード リンク

Clavius (crater) : ウィキペディア英語版
Clavius (crater)

Clavius is one of the largest crater formations on the Moon, and it is the third largest crater on the visible near side. It is located in the rugged southern highlands of the Moon, to the south of the prominent ray crater Tycho. The crater is named for the Jesuit priest Christopher Clavius, a 16th-century German mathematician and astronomer.
== Description ==

Due to the location of the crater toward the southern limb, the crater appears oblong due to foreshortening. Because of its great size, Clavius can be detected with the unaided eye. It appears as a prominent notch in the terminator about 1–2 days after the Moon reaches first quarter. The crater is one of the older formations on the lunar surface and was likely formed during the Nectarian period about 4 billion years ago. Despite its age, however, the crater is relatively well-preserved. It has a relatively low outer wall in comparison to its size, and it is heavily worn and pock-marked by craterlets. The rim does not significantly overlook the surrounding terrain, making this a "walled depression". The inner surface of the rim is hilly, notched, and varies in width, with the steepest portion in the south end. Overall the rim has been observed to have a somewhat polygonal outline.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Clavius (crater)」の詳細全文を読む



スポンサード リンク
翻訳と辞書 : 翻訳のためのインターネットリソース

Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.