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Geological studies of the Moon are based on a combination of Earth-based telescope observations, measurements from orbiting spacecraft, lunar samples, and geophysical data. . Six locations were sampled directly during the crewed Apollo program landings from 1969 to 1972, which returned 382 kilograms (842 lb) of lunar rock and lunar soil to Earth [8] In addition, three robotic Soviet Luna ...
They do not contain any water, but are believed to have been formed from molten rock from the Moon's mantle coming out onto the surface of the Moon. This list also includes the one oceanus and the features known by the names lacus, palus and sinus. The modern system of lunar nomenclature was introduced in 1651 by Riccioli. [1]
The Descartes Highlands is an area of lunar highlands located on the near side that served as the landing site of the American Apollo 16 mission in early 1972. The Descartes Highlands is located in the area surrounding Descartes crater, after which the feature received its name.
NASA Image Lunar Ferroan Anorthosite #60025 (Plagioclase Feldspar). Collected by Apollo 16 from the Lunar Highlands near Descartes. This sample is currently on display at the National Museum of Natural History in Washington, DC. Descartes is a heavily worn lunar impact crater that is located in the rugged south-central highlands of the Moon.
Tycho (/ ˈ t aɪ k oʊ /) is a prominent lunar impact crater located in the southern lunar highlands, named after the Danish astronomer Tycho Brahe (1546–1601). [2] It is estimated to be 108 million years old. [3] To the south of Tycho is the crater Street, to the east is Pictet, and to the north-northeast is Sasserides. The surface around ...
Oblique view of Fra Mauro taken from lunar orbit on the Apollo 12 mission. The Fra Mauro formation (or Fra Mauro Highlands) is a formation on the near side of Earth's Moon that served as the landing site for the American Apollo 14 mission in 1971. It is named after the 80-kilometer-diameter crater Fra Mauro, located within it.
The Apollo 16 mission lands in the Descartes Highlands region near the lunar equator in April 1972. - NASA ... All the minerals and rocks on the moon have a story to tell about lunar history ...
Mountains on the Moon have heights and elevations/altitudes defined relative to various vertical datums (referring to the lunoid), each in turn defined relative to the center of mass (CoM) of the Moon. c. 1960 — the U.S. Army Mapping Service datum was established 1,737,988 meters from the CoM.