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Apollo Crater
Apollo, also called the Apollo basin, is a large impact crater located on the far side of the Moon, in the southern hemisphere. It was previously known as Basin XVI; in 1970 it was officially named after the Apollo missions by the International Astronomical Union. The Chang'e 6 spacecraft landed within Apollo basin in 2024, collected samples of the surface, then brought them to Earth for analysis. Geology Apollo is a double-ringed walled plain (or basin) whose inner ring is roughly half the diameter of the outer wall. Both the outer wall and the interior have been heavily worn and eroded by subsequent impacts, so that significant parts of the outer and inner walls now consist of irregular and incised sections of mountainous arcs. The interior floor is covered in a multitude of craters of various sizes, some of which have been named for people associated with the Apollo program or other NASA projects. Sections of Apollo's interior have been resurfaced with lava, leaving pat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lunar Orbiter 5
Lunar Orbiter 5, the last of the "Lunar Orbiter series", was designed to take additional Project Apollo, Apollo and Surveyor program, Surveyor landing site photography and to take broad survey images of unphotographed parts of the Moon's far side. It was also equipped to collect selenodetic, radiation intensity, and micrometeoroid impact data and was used to evaluate the Manned Space Flight Network tracking stations and Apollo Orbit Determination Program. Mission summary The spacecraft was placed in a cislunar trajectory and on August 5, 1967 was injected into an elliptical near polar lunar orbit with an inclination of 85 degrees and a period of 8 hours 30 minutes. On August 7 the perilune was lowered to , and on August 9 the orbit was lowered to a , 3 hour 11 minute period. The spacecraft acquired photographic data from August 6 to 18, 1967, and readout occurred until August 27, 1967. A total of 633 high resolution and 211 medium resolution frames at resolution down to were ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Borman (crater)
Borman is a lunar impact crater that is located in the southern hemisphere on the far side of the Moon. It lies across the southeast section of the mountainous inner ring, within the walled basin named Apollo. The rim of Borman remains sharp-edged, although a smaller crater lies across its northwestern rim. The interior is rough but relatively flat. Borman L is an older and much more worn crater that is attached to the southern rim of Borman. Borman crater is named after the American astronaut Frank Borman. In 1968, Borman and his Apollo 8 crewmates became the first humans to orbit the Moon. Two nearby craters are named after the other crew members, William Anders ( Anders crater) and Jim Lovell ( Lovell crater). 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 Borman. The following craters have been renamed by the IAU. * Borman A — ''See'' McNair (crater). * Borman ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Smith (lunar Crater)
Smith is a lunar impact crater that is located within the huge walled plain Apollo, on the far side of the Moon. This crater is attached to the west-southwestern outer rim of Scobee and it overlies the northern edge of the inner mountain ring within Apollo Apollo is one of the Twelve Olympians, Olympian deities in Ancient Greek religion, ancient Greek and Ancient Roman religion, Roman religion and Greek mythology, Greek and Roman mythology. Apollo has been recognized as a god of archery, mu .... To the north lies Barringer. This crater is roughly circular and bowl-shaped, with a mildly worn outer rim. Some piles of scree lie along the base of the inner wall in the northern part of the crater. The interior floor is relatively featureless, with a small hill at the midpoint of the crater. References * * * * * * * * * * * * {{refend Impact craters on the Moon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
McNair (crater)
McNair is a small lunar impact crater on the far side of the Moon. It lies within the double-ringed Apollo basin, inside the eastern part of the interior ring. It has partly merged with the crater Jarvis, and the two share a common rim. To the south of McNair lies Borman. This is a bowl-shaped feature with a somewhat worn outer rim. There are some tiny craterlets along the southern rim, and a narrow cut through the edge to the south-southwest. The interior floor is relatively featureless. The crater name was approved by the IAU The International Astronomical Union (IAU; , UAI) is an international non-governmental organization (INGO) with the objective of advancing astronomy in all aspects, including promoting astronomical research, outreach, education, and developmen ... in 1988 in honor of Ronald McNair, killed in the Space Shuttle ''Challenger'' disaster on January 28, 1986. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jarvis (crater)
Jarvis is a Impact crater, crater that lies on the Far side (Moon), far side of the Moon. It is located within the walled plain Apollo (crater), Apollo, and lies in the eastern half of this basin within the interior ring. Jarvis has a low, somewhat worn outer rim that is generally circular. There is a wide break in the south-southeastern portion of the rim where is it partly overlain by the crater McNair (crater), McNair. The latter is younger than Jarvis, since its rim still survives where it intersects the interior of Jarvis. The interior of the crater is otherwise undistinguished, being marked only by tiny craters and some low ridges along the ramparts of McNair. The crater name was approved by the International Astronomical Union, IAU in 1988 in honor of Gregory Jarvis, killed in the Space Shuttle Challenger disaster, Space Shuttle ''Challenger'' disaster on January 28, 1986. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
