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Vallis Palitzsch
The Vallis Palitzsch is a geological structure of the surface of the Moon. The name of the valley was given in 1964 by the International Astronomical Union and comes from the adjacent crater, which in turn was named after the German astronomer Johann Georg Palitzsch (1723–1788). References Valleys on the Moon {{Valleys on the Moon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
:en:Palitzsch (crater)
Palitzsch is a lunar impact crater that is located in the southeast part of the Moon, near the southeast rim of the crater Petavius. Just to the southwest of Palitzsch is Hase, while to the east-southeast is Legendre. The northeast rim of Palitzsch forms the southern end of Vallis Palitzsch, a lunar valley that follows the eastern rim of Petavius for a distance of about 110 kilometers. The crater rim is relatively low and inconspicuous, while the floor forms a depression in the surface that follows the contours of the neighboring valley. Satellite craters By convention these features are identified on lunar maps by placing the letter on the side of the crater midpoint that is closest to Palitzsch. Due to its rays, Palitzsch B is mapped as part of the Copernican System.The geologic history of the Moon, 1987, Wilhelms, Don E.; with sections by McCauley, John F.; Trask, Newell J. USGS The United States Geological Survey (USGS), formerly simply known as the Geological ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
:en:Petavius (crater)
Petavius is a large lunar impact crater located to the southeast of the Mare Fecunditatis, near the southeastern lunar limb. Attached to the northwest rim is the smaller crater Wrottesley. To the southeast are Palitzsch, Vallis Palitzsch, and Hase. Farther to the north is the large crater Vendelinus. Petavius appears oblong when viewed from the Earth due to foreshortening. Petavius is Imbrian in age. The outer wall of Petavius is unusually wide in proportion to the diameter, and displays a double rim along the south and west sides. The height of the rim varies by as much as 50% from the lowest point, and a number of ridges radiate outwards from the rim. The convex crater floor has been resurfaced by lava flow, and displays a rille system named the Rimae Petavius. The large central mountains are a prominent formation with multiple peaks, climbing 1.7 kilometers above the floor. A deep fracture runs from the peaks toward the southwest rim of the crater. Rev. T. W. Webb desc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
