Mare Moscoviense
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| Ciało niebieskie | Księżyc | |
| Średnica krateru | 420 km | |
| Głębokość krateru | 5,25 - 5,96 km | |
| Źródło nazwy | Wielkie Księstwo Moskiewskie | |
Położenie na mapie Księżyca  | ||
 27°18′N 147°54′E/27,300000 147,900000 | ||
Mare Moscoviense (łac. Morze Moskwy) – morze księżycowe położone po niewidocznej stronie Księżyca, w centralnej części dużego basenu uderzeniowego. Średnica morza równa jest 277 km, jest to jedno z niewielu mórz znajdujących się na odwróconej od Ziemi stronie Księżyca. Morze Moskwy zostało rozpoznane na zdjęciach sondy Łuna 3, która w 1959 r. jako pierwsza sfotografowała tę część Srebrnego Globu[1].
Przypisy
- ↑ Akademia Nauk ZSRR: Atlas odwrotnej strony Księżyca. Tłum. Andrzej Kajetan Wróblewski. Warszawa: Państwowe Wydawnictwo Naukowe, 1961.
Media użyte na tej stronie
Nuvola apps kmoon left.png
Autor:
Icon from Nuvola icon theme for KDE 3.x.
Autor:
- Nuvola_apps_kmoon.png: David Vignoni / derivative work: Lady Whistler (talk)
Icon from Nuvola icon theme for KDE 3.x.
Moonmap from clementine data.png
cylindrical map projection of the Moon. The Moon's whole surface was mapped by the Clementine spacecraft in 1994, here North is at the top. The dark floor of crater Plato is at the middle top above Mare Imbrium, while the bright floor and rays of crater Tycho is near the middle bottom below Mare Imbrium. Mare Procellarum is at the near left, and Mare Tranquillitatis is just right of centre and Mare Crisium is at the near right. The far left and far right show the contrast of the mostly cratered farside with small isolated mare.
cylindrical map projection of the Moon. The Moon's whole surface was mapped by the Clementine spacecraft in 1994, here North is at the top. The dark floor of crater Plato is at the middle top above Mare Imbrium, while the bright floor and rays of crater Tycho is near the middle bottom below Mare Imbrium. Mare Procellarum is at the near left, and Mare Tranquillitatis is just right of centre and Mare Crisium is at the near right. The far left and far right show the contrast of the mostly cratered farside with small isolated mare.
Steel pog.svg
Shiny LightSteelBlue button/marker widget. Used to mark the location of something such as a tourist attraction.
Shiny LightSteelBlue button/marker widget. Used to mark the location of something such as a tourist attraction.
Full Moon Luc Viatour.jpg
(c) Luc Viatour, CC-BY-SA-3.0
Nearly Full Moon view from earth In Belgium (Hamois).
(c) Luc Viatour, CC-BY-SA-3.0
Nearly Full Moon view from earth In Belgium (Hamois).
Mare Moscoviense - Clementine.jpg
en:Mare Moscoviense sits in the Moscoviense basin.Like Mare Marginis, this mare appears to be fairly thin. However, it is clearly centered within a large impact basin. It is also much lower than either the outer basin floor or the farside highlands. The great depth of this mare beneath the nearby highlands probably explains why mare units are so rare on the lunar farside. Very few basins on the farside were deep enough to allow mare volcanism. Thus, while large impact basins are found on both the nearside and farside, large mare are mostly found on the nearside. Mare lavas apparently could reach the surface more often and more easily there. The basin material is of the Nectarian epoch, while the mare material is of the Upper Imbrian epoch. The crater Komarov is seen to the southeast of the mare. You can just make out the crater Titov in the northern regin of the mare.
en:Mare Moscoviense sits in the Moscoviense basin.Like Mare Marginis, this mare appears to be fairly thin. However, it is clearly centered within a large impact basin. It is also much lower than either the outer basin floor or the farside highlands. The great depth of this mare beneath the nearby highlands probably explains why mare units are so rare on the lunar farside. Very few basins on the farside were deep enough to allow mare volcanism. Thus, while large impact basins are found on both the nearside and farside, large mare are mostly found on the nearside. Mare lavas apparently could reach the surface more often and more easily there. The basin material is of the Nectarian epoch, while the mare material is of the Upper Imbrian epoch. The crater Komarov is seen to the southeast of the mare. You can just make out the crater Titov in the northern regin of the mare.