The Moon is Earth's only natural satellite, orbiting at an average distance of 384,399 km. It's tidally locked to Earth, resulting in synchronous rotation, where its rotation and orbital periods are identical, keeping the same side facing Earth. The Moon's gravity is the primary cause of Earth's tides.
From 1920 to the 1940s, comparative studies were conducted on lunar craters, leading to the development of lunar stratigraphy.
Following the first spaceflight of Sputnik 1 in 1957 during International Geophysical Year, the spacecraft of the Soviet Union's Luna program were the first to accomplish a number of goals in lunar exploration.
In 1958, the Soviet Union's Luna program experienced three unnamed failed missions before successfully reaching the moon.
In 1959, the Soviet Union's Luna program achieved multiple milestones, including Luna 1 escaping Earth's gravity and passing near the Moon, Luna 2 reaching the Moon's surface by intentionally impacting, and Luna 3 taking the first photographs of the far side of the Moon.
In 1959, the first human-made objects were sent to the Moon, starting with the flyby of the Soviet Union's Luna 1 and the intentional impact of Luna 2.
In 1961, President John F. Kennedy committed the United States to a crewed Moon landing before the end of the decade, leading to NASA's lunar exploration programs.
In 1966, Luna 9 performed the first successful lunar soft landing, and Luna 10 became the first vehicle to orbit the Moon.
In 1966, the first soft landing on the moon was achieved by Luna 9, and the first orbital insertion was achieved by Luna 10.
In 1968, Apollo 8 made the first human mission to lunar orbit, which took place after the Soviet Union's Zond 5 carried the first Earthlings (tortoises) around the Moon three months earlier.
On July 20, 1969, humans first stepped on an extraterrestrial body, landing on the Moon at Mare Tranquillitatis with the lander Eagle of the United States' Apollo 11 mission.
On July 21, 1969 (02:56 UTC), Neil Armstrong, commander of the Apollo 11 mission, became the first person to set foot on the Moon. The Apollo TV camera transmitted this event, and an estimated 500 million people worldwide watched the live broadcast. At the same time the Soviet Union's Luna 15 was in orbit around the Moon.
The analysis revealed that scientists have confirmed the presence of a cave on the Moon near the Sea of Tranquillity, not far from the 1969 Apollo 11 landing site.
The existence of moonquakes was an unexpected discovery from seismometers placed on the Moon by Apollo astronauts from 1969 through 1972.
From 1969 through 1972, seismometers were placed on the Moon by Apollo astronauts, leading to the discovery of moonquakes.
In 1972, the Apollo 17 mission collected the high-titanium "orange glass soil" of volcanic origin, which later was found to contain 615-1410 ppm water in melt inclusions in May 2011.
In 1972, the Apollo 17 mission marked the last crewed mission to the Moon, during which 380.05 kilograms of lunar rock and soil were collected.
In 1973, Explorer 49 was the last dedicated U.S. probe to the Moon until the 1990s.
In late 1977, direct transmission of data from the scientific instrument packages installed on the lunar surface during the Apollo landings concluded due to budgetary considerations.
In 1994, the bistatic radar experiment located on the Clementine spacecraft, indicated the existence of small, frozen pockets of water close to the surface of the moon.
In 1998, the NASA Lunar Prospector mission collected data, which planetary scientists later used in 2016 to find two hydrogen-rich areas (most likely former water ice) on opposite sides of the Moon.
In 2006, a study of Ina, a tiny depression in Lacus Felicitatis, found jagged, relatively dust-free features that, because of the lack of erosion by infalling debris, appeared to be only 2 million years old.
Models from 2007 and later suggest a larger fraction of the Moon derived from the proto-Earth.
In 2008, the Chandrayaan-1 spacecraft confirmed the existence of surface water ice, using the on-board Moon Mineralogy Mapper. The spectrometer observed absorption lines common to hydroxyl, in reflected sunlight, providing evidence of large quantities of water ice, on the lunar surface.
In 2009, the Lunar Crater Observation and Sensing Satellite (LCROSS) sent a 2,300 kg impactor into a permanently shadowed polar crater, and detected at least 100 kg of water in a plume of ejected material.
In 2010, photos taken by NASA's Lunar Reconnaissance Orbiter were used to analyze and confirm the existence of a cave on the moon. The cave is identified as an entry point to a collapsed lava tube and is roughly 45 meters wide and up to 80 m long.
In May 2011, 615–1410 ppm water in melt inclusions in lunar sample 74220 was reported, the famous high-titanium "orange glass soil" of volcanic origin collected during the Apollo 17 mission in 1972.
In 2016, planetary scientists using data collected on the 1998–99 NASA Lunar Prospector mission found two hydrogen-rich areas (most likely former water ice) on opposite sides of the Moon.
In August 2018, analysis of the findings of the Moon Mineralogy Mapper (M3) revealed for the first time "definitive evidence" for water-ice on the lunar surface. The data revealed the distinct reflective signatures of water-ice, as opposed to dust and other reflective substances. The ice deposits were found on the North and South poles.
In 2018, using the Moon Mineralogy Mapper's reflectance spectra, indirect lighting of areas in shadow confirmed water ice within 20° latitude of both poles.
In October 2020, astronomers reported detecting molecular water on the sunlit surface of the Moon by several independent spacecraft, including the Stratospheric Observatory for Infrared Astronomy (SOFIA).
A study published in 2022 using high-resolution simulations found that giant impacts can immediately place a satellite with similar mass and iron content to the Moon into orbit far outside Earth's Roche limit.
On November 1, 2023, scientists reported that, according to computer simulations, remnants of Theia could still be present inside the Earth.
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