Moon rock explained

Moon rock or lunar rock is rock originating from Earth's Moon. This includes lunar material collected during the course of human exploration of the Moon, and rock that has been ejected naturally from the Moon's surface and landed on Earth as meteorites.

Sources

Moon rocks on Earth come from four sources: those collected by six United States Apollo program crewed lunar landings from 1969 to 1972; those collected by three Soviet uncrewed Luna probes in the 1970s; those collected by the Chinese Lunar Exploration Program's uncrewed probes; and rocks that were ejected naturally from the lunar surface before falling to Earth as lunar meteorites.

Apollo program

Six Apollo missions collected 2,200 samples of material weighing 381kg (840lb), processed into more than 110,000 individually cataloged samples.[1]

MissionSiteSample mass
returned[2]
Year
Apollo 11Mare Tranquillitatis47.51order=flipNaNorder=flip1969
Apollo 12Ocean of Storms75.62order=flipNaNorder=flip1969
Apollo 14Fra Mauro formation94.35order=flipNaNorder=flip1971
Apollo 15Hadley-Apennine169.1order=flipNaNorder=flip1971
Apollo 16Descartes Highlands209.89order=flipNaNorder=flip1972
Apollo 17Taurus-Littrow243.4order=flipNaNorder=flip1972

Luna program

Three Luna spacecraft returned with 301g of samples.[3] [4] [5]

MissionSiteSample mass
returned
Year
Luna 16Mare Fecunditatis101g[6] 1970
Luna 20Mare Fecunditatis30g[7] 1972
Luna 24Mare Crisium170g[8] 1976

The Soviet Union abandoned its attempts at a crewed lunar program in the 1970s, but succeeded in landing three robotic Luna spacecraft with the capability to collect and return small samples to Earth. A combined total of less than half a kilogram of material was returned.

In 1993, three small rock fragments from Luna 16, weighing 200 mg, were sold for US$ 442,500 at Sotheby's .[9] In 2018, the same three Luna 16 rock fragments sold for US$ 855,000 at Sotheby's.[10]

Chang'e missions

See also: Changesite–(Y).

MissionSiteSample mass
returned
Year
Chang'e 5Mons Rümker1731abbr=onNaNabbr=on[11] 2020
Chang'e 6Southern Apollo crater1935.3abbr=onNaNabbr=on[12] [13] 2024

In 2020, Chang'e 5, the fifth lunar exploration mission of the Chinese Lunar Exploration Program, returned approximately of rocks and dust from the Oceanus Procellarum, (the Ocean of Storms), the largest dark region on the Moon, visible on the western edge.[14] The Chang'e-5 samples contain 'perplexing combination' of minerals and include the sixth new lunar mineral, named Changesite-(Y). This phosphate mineral characterized by colorless, transparent columnar crystals. Researchers estimated the peak pressure (11-40 GPa) and impact duration (0.1-1.0 second) of the collision that shaped the sample. Using shock wave models, they estimated the resulting crater to be between 3 to 32 kilometers wide, depending on the impact angle.[15]

The follow-up mission to Chang'e 5, Chang'e 6, reached the Moon on May 8, 2024, and entered lunar orbit for 20 days to find an appropriate landing site. On 1 June, 2024, the lander separated from the orbiter and landed on a mare unit at the southern part of the Apollo crater (36.1°S, 208.3°E).[16] The mission objective was to collect about 2 kg of material from the far side of the Moon and bring it back to Earth.

The Chang’e-6 probe withstood the high temperatures and collected the samples by drilling into the Moon’s surface and scooping soil and rocks with a mechanical arm, according to a statement from the China National Space Administration (CNSA). The collected rock was crushed, melted and drawn into filaments about one third of the diameter of a human hair, then spun into thread and woven into cloth. “The lunar surface is rich in basalt and since we’re building a lunar base in the future, we will most likely have to make basalt into fibers and use it as building materials," said engineer Zhou Changyi.[17]

The samples were placed in the ascent vehicle, which docked with the Chang'e 6 orbiter-return vehicle on June 6, 2024[18] China’s Chang’e-6 lunar probe, carrying the first lunar rocks ever collected from the far side of the Moon, landing in China’s Inner Mongolia region on June 25, 2024.

Lunar meteorites

More than 370 lunar meteorites have been collected on Earth,[19] representing more than 30 different meteorite finds (no falls), with a total mass of over 1090kg (2,400lb).[20] Some were discovered by scientific teams (such as ANSMET) searching for meteorites in Antarctica, with most of the remainder discovered by collectors in the desert regions of northern Africa and Oman. A Moon rock known as "NWA 12691", which weighs, was found in the Sahara Desert at the Algerian and Mauritanian borders in January 2017,[21] and went on sale for $2.5 million in 2020.[22]

Dating

Rocks from the Moon have been measured by radiometric dating techniques. They range in age from about 3.16 billion years old for the basaltic samples derived from the lunar maria, up to about 4.44 billion years old for rocks derived from the highlands.[23] Based on the age-dating technique of "crater counting," the youngest basaltic eruptions are believed to have occurred about 1.2 billion years ago,[24] but scientists do not possess samples of these lavas. In contrast, the oldest ages of rocks from the Earth are between 3.8 and 4.28 billion years.

Composition

See main article: Geology of the Moon.

Common lunar minerals
Mineral Elements Lunar rock appearance
Plagioclase feldsparCalcium (Ca)
Aluminium (Al)
Silicon (Si)
Oxygen (O)
White to transparent gray; usually as elongated grains.
PyroxeneIron (Fe),
Magnesium (Mg)
Calcium (Ca)
Silicon (Si)
Oxygen (O)
Maroon to black; the grains appear more elongated in the maria and more square in the highlands.
OlivineIron (Fe)
Magnesium (Mg)
Silicon (Si)
Oxygen (O)
Greenish color; generally, it appears in a rounded shape.
IlmeniteIron (Fe),
Titanium (Ti)
Oxygen (O)
Black, elongated square crystals.
Moon rocks fall into two main categories: those found in the lunar highlands (terrae), and those in the maria. The terrae consist dominantly of mafic plutonic rocks. Regolith breccias with similar protoliths are also common. Mare basalts come in three distinct series in direct relation to their titanium content: high-Ti basalts, low-Ti basalts, and Very Low-Ti (VLT) basalts.

Almost all lunar rocks are depleted in volatiles and are completely lacking in hydrated minerals common in Earth rocks. In some regards, lunar rocks are closely related to Earth's rocks in their isotopic composition of the element oxygen. The Apollo Moon rocks were collected using a variety of tools, including hammers, rakes, scoops, tongs, and core tubes. Most were photographed prior to collection to record the condition in which they were found. They were placed inside sample bags and then a Special Environmental Sample Container for return to the Earth to protect them from contamination. In contrast to the Earth, large portions of the lunar crust appear to be composed of rocks with high concentrations of the mineral anorthite. The mare basalts have relatively high iron values. Furthermore, some of the mare basalts have very high levels of titanium (in the form of ilmenite).[25]

Highlands rocks

Plagioclase! style="background:#E3E3DF"
PyroxeneOlivineIlmenite
90% 5% 5% 0%
60% 35% 5% 0%
60% 5% 35% 0%

Primary igneous rocks in the lunar highlands compose three distinct groups: the ferroan anorthosite suite, the magnesian suite, and the alkali suite.

Lunar breccias, formed largely by the immense basin-forming impacts, are dominantly composed of highland lithologies because most mare basalts post-date basin formation (and largely fill these impact basins).

Mare basalts

Plagioclase! style="background:#E3E3DF"
PyroxeneOlivineIlmenite
High titanium content 30% 54% 3% 18%
Low titanium content 30% 60% 5% 5%
Very low titanium content 35% 55% 8% 2%

Mare basalts are named as such because they frequently constitute large portions of the lunar maria. These typically contain 18–21 percent FeO by weight, and 1–13 percent TiO2. They are similar to terrestrial basalts, but have many important differences; for example, mare basalts show a large negative europium anomaly. The type location is Mare Crisium sampled by Luna 24.

Curation and availability

The main repository for the Apollo Moon rocks is the Lunar Sample Laboratory Facility at the Lyndon B. Johnson Space Center in Houston, Texas. For safekeeping, there is also a smaller collection stored at White Sands Test Facility in Las Cruces, New Mexico. Most of the rocks are stored in nitrogen to keep them free of moisture. They are handled only indirectly, using special tools.

Some Moon rocks from the Apollo missions are displayed in museums, and a few allow visitors to touch them. One of these, called the Touch Rock, is displayed in the Smithsonian National Air and Space Museum in Washington, D.C.[28] The idea of having touchable Moon rocks at a museum was suggested by Apollo scientist Farouk El-Baz, who was inspired by his childhood pilgrimage to Mecca where he touched the Black Stone (which in Islam is believed to be sent down from the heavens).[29]

Moon rocks collected during the course of lunar exploration are currently considered priceless. In 2002, a safe was stolen from the Lunar Sample Building that contained minute samples of lunar and Martian material. The samples were recovered, and NASA estimated their value during the ensuing court case at about $1 million for 10oz of material.

Naturally transported Moon rocks in the form of lunar meteorites are sold and traded among private collectors.

Goodwill Moon rocks

See main article: Lunar sample displays.

Apollo 17 astronauts Eugene Cernan and Harrison Schmitt picked up a rock "composed of many fragments, of many sizes, and many shapes, probably from all parts of the Moon". This rock was later labeled sample 70017.[30] President Nixon ordered that fragments of that rock should be distributed in 1973 to all 50 US states and 135 foreign heads of state. The fragments were presented encased in an acrylic sphere, mounted on a wood plaque which included the recipients' flag which had also flown aboard Apollo 17.[31] Many of the presentation Moon rocks are now unaccounted for, having been stolen or lost.

Discoveries

Three minerals were discovered from the Moon: armalcolite, tranquillityite, and pyroxferroite. Armalcolite was named for the three astronauts on the Apollo 11 mission: Armstrong, Aldrin and Collins.

Stolen and missing Moon rocks

See main article: Stolen and missing Moon rocks. Because of their rarity on Earth, and the difficulty of obtaining more, Moon rocks have been frequent targets of theft and vandalism, and many have gone missing or were stolen.

See also

References

General sources

External links

Notes and References

  1. Web site: NASA Lunar Sample Laboratory Facility . 1 September 2016 . NASA Curation Lunar . . 13 October 2018 . live . https://web.archive.org/web/20180825074518/https://curator.jsc.nasa.gov/lunar/lun-fac.cfm . 25 August 2018.
  2. Book: Orloff, Richard W. . Apollo by the Numbers: A Statistical Reference . Extravehicular Activity . https://history.nasa.gov/SP-4029/Apollo_18-30_Extravehicular_Activity.htm . August 1, 2013 . The NASA History Series . First published 2000 . September 2004 . NASA History Division, Office of Policy and Plans . Washington, D.C. . 978-0-16-050631-4 . 00061677 . NASA SP-2000-4029 . Orloff.
  3. Web site: Luna 16 . Ivankov . A. . . National Space Science Data Center Catalog . 13 October 2018 . The drill was deployed and penetrated to a depth of 35 cm before encountering hard rock or large fragments of rock. The column of regolith in the drill tube was then transferred to the soil sample container... the hermetically sealed soil sample container, lifted off from the Moon carrying 101 grams of collected material.
  4. Web site: Luna 20 . Ivankov . A. . . National Space Science Data Center Catalog . 13 October 2018 . Luna 20 was launched from the lunar surface on 22 February 1972 carrying 30 grams of collected lunar samples in a sealed capsule.
  5. Web site: Luna 24 . Ivankov . A. . . National Space Science Data Center Catalog . 13 October 2018 . the mission successfully collected 170.1 grams of lunar samples and deposited them into a collection capsule.
  6. Web site: NASA - NSSDC - Spacecraft - Details. nssdc.gsfc.nasa.gov. 2015-11-08.
  7. Web site: NASA - NSSDC - Spacecraft - Details. nssdc.gsfc.nasa.gov. 2015-11-08.
  8. Web site: NASA - NSSDC - Spacecraft - Details. nssdc.gsfc.nasa.gov. 2015-11-08.
  9. News: F.B.I. Revisits Earthly Theft of Moon Rock . Lawrence . Van Gelder . September 6, 2021 . The New York Times . 1995-12-02 .
  10. Web site: THE ONLY KNOWN DOCUMENTED SAMPLES OF THE MOON AVAILABLE FOR PRIVATE OWNERSHIP . Sothebys.com . 29 November 2018.
  11. Web site: 19 December 2020. China's Chang'e-5 retrieves 1,731 grams of moon samples. 19 December 2020. Xinhua News Agency. live. 20 December 2020. https://web.archive.org/web/20201220143345/http://www.xinhuanet.com/english/2020-12/19/c_139603150.htm.
  12. Web site: NASA - NSSDCA - Spacecraft - Details . 2024-06-21 . nssdc.gsfc.nasa.gov.
  13. Web site: 2024-06-28 . 新华社权威快报丨嫦娥六号带回世界首份月背样品1935.3克 . 2024-06-28 . 新华网 . zh-hans.
  14. Web site: Sharmila Kuthunur . 2024-02-08 . China's Chang'e-5 moon samples contain 'perplexing combination' of minerals . 2024-06-21 . Space.com . en.
  15. Web site: Nielsen . Marissa . 2024-02-06 . Understanding the Moon's History with Chang'e-5 Sample . 2024-06-21 . AIP Publishing LLC . en-US.
  16. Web site: First Look: Chang'e 6 . 2024-06-21 . www.lroc.asu.edu . en.
  17. Web site: McCarthy . Nectar Gan, Simone . 2024-06-04 . China's Chang'e-6 probe lifts off with samples from moon's far side in historic first . 2024-06-21 . CNN . en.
  18. Web site: NASA - NSSDCA - Spacecraft - Details . 2024-06-21 . nssdc.gsfc.nasa.gov.
  19. Web site: Meteoritical Bulletin Database — Lunar Meteorite search results . The Meteoritical Society . Meteoritical Bulletin Database . 10 July 2019 . 20 July 2019.
  20. Web site: List of Lunar Meteorites - Feldspathic to Basaltic Order . 11 September 2023 . meteorites.wustl.edu.
  21. Web site: Northwest Africa 12691. The Meteoritical Society.
  22. Web site: Super-Rare Moon Meteorite Found In Sahara Desert Goes On Sale For $2.5 Million. Forbes. 2 May 2020.
  23. James Papike . Grahm Ryder . Charles Shearer . amp . Lunar Samples . Reviews in Mineralogy and Geochemistry . 36 . 5.1–5.234 . 1998 .
  24. Ages and stratigraphy of mare basalts in Oceanus Procellarum, Mare Numbium, Mare Cognitum, and Mare Insularum . J. Geophys. Res. . 108. E7 . 2003 . 10.1029/2002JE001985 . 5065 . free . Hiesinger . H. . Head . J. W. . Wolf . U. . Jaumann . R. . Neukum . G. . 2003JGRE..108.5065H .
  25. News: Bhanoo . Sindya N. . New Type of Rock Is Discovered on Moon . 28 December 2015 . . 29 December 2015 .
  26. Wieczorek . Mark . Jolliff . Bradley . Khan . Amir . etal. The Constitution and Structure of the Lunar Interior . Reviews in Mineralogy and Geochemistry . 60 . 1 . 2006 . 221–364. 2006RvMG...60..221W . 10.2138/rmg.2006.60.3 .
  27. Lucey . Paul . Korotev . Randy . Taylor . Larry . etal. understanding the lunar surface and Space-Moon Interactions . Reviews in Mineralogy and Geochemistry . 60 . 1 . 2006 . 100. 2006RvMG...60...83L . 10.2138/rmg.2006.60.2 .
  28. Web site: How NASA has kept Apollo Moon rocks safe from contamination for 50 years. Grossman. Lisa. 2019-07-15. Science News. en. 2019-07-31.
  29. Web site: Reichhardt . Tony . Twenty People Who Made Apollo Happen . . . June 7, 2019 . 7 September 2019.
  30. Web site: Astromaterials Research . Exploration Science . amp . 70017 Ilmenite Basalt. NASA.
  31. Web site: Where are the Apollo 17 Goodwill Moon Rocks?. Collect Space.