|Colongitude||235° at sunrise|
Tsiolkovskiy is a large lunar impact crater that is located on the far side of the Moon. Named for Russian scientist Konstantin Tsiolkovsky, it lies in the southern hemisphere, to the west of the large crater Gagarin, and northwest of Milne. Just to the south is Waterman, with Neujmin to the south-southwest. The crater protrudes into the neighbouring Fermi, an older crater of comparable size that does not have a lava-flooded floor.
Tsiolkovskiy is one of the most prominent features on the far side of the Moon. It possesses high, terraced inner walls and a well-formed central peak, which rises over 3200 m above the floor of the crater. The floor is unusual for a crater on the far side, as it is covered by the dark-hued mare that is characteristic of the maria found on the near side. The distribution of the mare material is not symmetrical across the floor, but is instead more heavily concentrated to the east and south. There is also a protruding bay of darker material that reaches the wall to the west-northwest. The remainder of the floor has the same albedo as the terrain surrounding the crater.
A row of small craters in Mendeleev crater far to the northeast are called Catena Mendeleev, and the row points directly at Tsiolkovsky. For this reason the craters are believed to be secondaries from the Tsiolkovsky impact.
Apollo 17 Astronaut Harrison "Jack" Schmitt and other scientists (Schmitt was the only trained scientist, a geologist, to walk on the Moon) strongly advocated Tsiolkovskiy as the landing site of Apollo 17, using small communications satellites deployed from the Command/Service Module for communication from the far side of the Moon. NASA vetoed the idea as too risky, and Apollo 17 instead landed in the Taurus–Littrow valley on December 11, 1972.
Lunar Orbiter 1 image
Apollo 8 image
Apollo 15 mapping camera image of the central peak
Oblique view from Apollo 17, facing south
Mosaic of Apollo 17 mapping camera images, while Tsiolkovskiy was at the terminator
By convention these features are identified on lunar maps by placing the letter on the side of the crater midpoint that is closest to Tsiolkovskiy.
- 1590 Tsiolkovskaja, asteroid
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|Wikimedia Commons has media related to Tsiolkovskiy (crater).|
- The following L&PI topographic maps show portions of the Tsiolkovskiy crater:
Northern half — LTO-101B2 Tsiolkovskij Borealis Southern half — LTO-101B3 Tsiolkovskij Australis Northeast — LTO-102A1 Patsaev Southeast — LTO-102A4 Fesnekov