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The pit is located at 8.3355°N, 33.222°E on the moon's surface. Radar imaging indicated that the pit's funnel is roughly 20 meters deep, while the inner pit has a depth of approximately 105 meters. The diameter of the pit's funnel was between 140 and 146 meters long while the diameter of the inner pit is 88–100 meters long.
The Mare Tranquillitatis pit has been associated with a lava tube. Lunar lava tubes are lava tubes on the Moon formed during the eruption of basaltic lava flows. When the surface of a lava flow cools, it hardens and the lava can channel beneath the surface in a tube-shaped passage. Once the flow of lava diminishes, the tube may drain, forming a ...
Mare Tranquillitatis was the landing site for the first crewed landing on the Moon on July 20, 1969, at 20:18 UTC. After astronauts Neil Armstrong and Buzz Aldrin made a soft landing in the Apollo 11 Lunar Module Eagle , Armstrong told flight controllers on Earth, "Houston, Tranquility Base here.
Vega is an eroded lunar impact crater that is located in the southeastern part of the Moon. ... 63.5° E 30 km C 45.2° S 64.8° E 21 km D 44.7° S 64.3° E 25 km G
The Marius Hills region was at one time considered a possible landing site for a lunar landing mission during the American Apollo program (eventually becoming the alternative site for Apollo 15), with the possibility of gaining insight about the volcanic history of the Moon from domes in the area. [11]
According to David H. Levy, Shoemaker "saw the craters on the Moon as logical impact sites that were formed not gradually, in eons, but explosively, in seconds." [ 3 ] Lunar craters as captured through the backyard telescope of an amateur astronomer, partially illuminated by the sun on a waning crescent moon.
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Plato is a lava-filled lunar impact crater on the Moon.Its diameter is 101 km. It was named after ancient Greek philosopher Plato. [1] It is located on the northeastern shore of the Mare Imbrium, at the western extremity of the Montes Alpes mountain range.