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Apollo used the Saturn family of rockets as launch vehicles, which were also used for an Apollo Applications Program, which consisted of Skylab, a space station that supported three crewed missions in 1973–1974, and the Apollo–Soyuz Test Project, a joint United States-Soviet Union low Earth orbit mission in 1975.
Once complete, it obviated the need for the E-type objective of a medium Earth orbital test. The D-type mission was instead performed by Apollo 9; the F-type mission, Apollo 10, flew the CSM/LM spacecraft to the Moon for final testing, without landing. The G-type mission, Apollo 11, performed the first lunar landing, the central goal of the ...
The PSEP was placed 16.8 meters (55 ft) from the Apollo 11 Lunar Module at Tranquility Base on July 21, 1969. [1] A set of 15 different commands could be sent to the experiment package from mission control on Earth to direct the instrument's levelling and calibration motors. [1]
Launched in June 2015, the project - named for the Apollo Program, which brought together thousands of scientists and engineers to put mankind on the moon - calls for developed nations to commit to spending 0.02% of their GDP, for 10 years, to fund co-ordinated research to solve the challenge. This equates to $150 billion over a decade, roughly ...
Orbital photo of the Hadley-Apennine site; Apollo 15 landing site is marked with a circle. Hadley–Apennine is a region on the near side of Earth's Moon that served as the landing site for the American Apollo 15 mission, the fourth crewed landing on the Moon and the first of the "J-missions", in July 1971.
The facility is the chief repository of the samples returned by the Apollo program. [5] The Apollo missions to the lunar surface (Apollo 11, Apollo 12, Apollo 14, Apollo 15, Apollo 16, and Apollo 17) returned a total of 382 kilograms (842 pounds) of lunar rocks, core samples, pebbles, sand and lunar surface dust, comprising 2200 individual ...
Lunokhod 2 's array continues to return signals to Earth. [11] The Lunokhod arrays suffer from decreased performance in direct sunlight—a factor considered in reflector placement during the Apollo missions. [12] The Apollo 15 array is three times the size of the arrays left by the two earlier Apollo missions.
The Solar Wind Composition Experiment (SWC) was an experiment deployed on the Moon during the Apollo program (Apollo 11, 12, 14, 15 and 16). The aim was to measure and sample the solar wind outside the Earth's magnetosphere. It was the first definitive isotopic measurements of solar material. [2]