Moon rock or lunar rock is rock that is found on the Earth's moon including lunar material collected during the course of human exploration of the Moon, or rock that has been ejected naturally from the Moon's surface (and which has then landed on the Earth as meteorites).
Moon rocks on Earth come from three sources: those collected by the United States Apollo program manned lunar landings from 1969 to 1972; samples returned by three Soviet Luna programme unmanned probes in the 1970s; and rocks that were ejected naturally from the lunar surface. The Apollo missions collected 2,200 samples weighing 382 kilograms (842 lb). Three Luna spacecraft returned with 301 grams (10.6 oz) of samples. More than 300 lunar meteorites have been collected on Earth, representing more than 30 different meteorite fall events (none witnessed), with a total mass of over 190 kilograms (420 lb). 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.
Luna mission sample returns
The Soviet Union attempted, but failed to make manned lunar landings in the 1970s, due to failure to develop their N1 rocket, but they succeeded in landing three robotic Luna spacecraft with the capability to collect and return small samples to Earth. A combined total of less than one kilogram of material was returned.
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. Based on the age-dating technique of "crater counting," the youngest basaltic eruptions are believed to have occurred about 1.2 billion years ago, 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 old.
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).
|High titanium content||30%||54%||3%||18%|
|Low titanium content||30%||60%||5%||5%|
|Very low titanium content||35%||55%||8%||2%|
|Mineral||Elements||Lunar rock appearance|
|Plagioclase feldspar||Calcium (Ca)
|White to transparent gray; usually as elongated grains.|
|Maroon to black; the grains appear more elongated in the maria and more square in the highlands.|
|Greenish color; generally, it appears in a rounded shape.|
|Black, elongated square crystals.|
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).
The ferroan anorthosite suite consists almost exclusively of the rock anorthosite (>90% calcic plagioclase) with less common anorthositic gabbro (70-80% calcic plagioclase, with minor pyroxene). The ferroan anorthosite suite is the most common group in the highlands, and is inferred to represent plagioclase flotation cumulates of the lunar magma ocean, with interstitial mafic phases formed from trapped interstitial melt or rafted upwards with the more abundant plagioclase framework. The plagioclase is extremely calcic by terrestrial standards, with molar anorthite contents of 94-96% (An94-96). This reflects the extreme depletion of the bulk moon in alkalis (Na, K) as well as water and other volatile elements. In contrast, the mafic minerals in this suite have low Mg/Fe ratios that are inconsistent with calcic plagioclase compositions. Ferroan anorthosites have been dated using the internal isochron method at "circa" 4.4 Ga.
The magnesian suite (or "mg suite") consists of dunites (>90% olivine), troctolites (olivine-plagioclase), and gabbros (plagioclase-pyroxene) with relatively high Mg/Fe ratios in the mafic minerals and a range of plagioclase compositions that are still generally calcic (An86-93). These rocks represent later intrusions into the highlands crust (ferroan anorthosite) at round 4.3-4.1 Ga. An interesting aspect of this suite is that analysis of the trace element content of plagioclase and pyroxene require equilibrium with a KREEP-rich magma, despite the refractory major element contents.
The alkali suite is so-called because of its high alkali content—for moon rocks. The alkali suite consists of alkali anorthosites with relatively sodic plagioclase (An70-85), norites (plagioclase-orthopyroxene), and gabbronorites (plagioclase-clinopyroxene-orthopyroxene) with similar plagioclase compositions and mafic minerals more iron-rich than the magnesian suite. The trace element contents of these minerals also indicates a KREEP-rich parent magma. The alkali suite spans an age range similar to the magnesian suite.
Lunar granites are relatively rare rocks that include diorites, monzodiorites, and granophyres. They consist of quartz, plagioclase, orthoclase or alkali feldspar, rare mafics (pyroxene), and rare zircon. The alkali feldspar may have unusual compositions unlike any terrestrial feldspar, and they are often Ba-rich. These rocks apparently form by the extreme fractional crystallization of magnesian suite or alkali suite magmas, although liquid immiscibility may also play a role. U-Pb date of zircons from these rocks and from lunar soils have ages of 4.1-4.4 Ga, more or less the same as the magnesian suite and alkali suite rocks. In the 1960s, NASA researcher John A. O'Keefe and others linked lunar granites with tektites found on Earth although many researchers refuted these claims. According to one study, a portion of lunar sample 12013 has a chemistry that closely resembles javanite tektites found on Earth.
Lunar breccias range from glassy vitrophyre melt rocks, to glass-rich breccia, to regolith breccias. The vitrophyres are dominantly glassy rocks that represent impact melt sheets that fill large impact structures. They contain few clasts of the target lithology, which is largely melted by the impact. Glassy breccias form from impact melt that exit the crater and entrain large volumes of crushed (but not melted) ejecta. It may contain abundant clasts that reflect the range of lithologies in the target region, sitting in a matrix of mineral fragments plus glass that welds it all together. Some of the clasts in these breccias are pieces of older breccias, documenting a repeated history of impact brecciation, cooling, and impact. Regolith breccias resemble the glassy breccias but have little or no glass (melt) to weld them together. As noted above, the basin-forming impacts responsible for these breccias pre-date almost all mare basalt volcanism, so clasts of mare basalt are very rare. When found, these clasts represent the earliest phase of mare basalt volcanism preserved.
Mare basalts are named as such because they frequently constitute large portions of the lunar maria. They are similar to terrestrial basalts, but have many important differences; for example, mare basalts show a large negative europium anomaly. Certain mare basalts (the so-called VHK (Very High K) basalts) have extraordinary potassium content.
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 safe keeping, 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.
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 10 oz. (285 g) of material.
Naturally transported Moon rocks in the form of lunar meteorites are sold and traded among private collectors.
Goodwill Moon rocks
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. 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. Many of the presentation Moon rocks are now unaccounted for, having been stolen or lost.
Three minerals were discovered from the Moon. These include 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
Samples in Lunar Sample Building at JSC
Moon rock on display for visitors to touch at the Apollo/Saturn V Center
Cut fragment of Apollo 17 sample 76015, an impact melt breccia
Sample 15016, the Seatbelt basalt
Sample 61016, better known as Big Muley, the largest sample collected during the Apollo program
- "NASA Lunar Sample Laboratory Facility". NASA Curation Lunar. NASA. 1 September 2016. Archived from the original on 25 August 2018. Retrieved 13 October 2018.
A total of 382 kilograms of lunar material, comprising 2200 individual specimens returned from the Moon, has been processed to meet scientific requirements into more than 110,000 individually cataloged samples.
- Ivankov, A. "Luna 16". National Space Science Data Center Catalog. NASA. Retrieved 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
- Ivankov, A. "Luna 20". National Space Science Data Center Catalog. NASA. Retrieved 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
- Ivankov, A. "Luna 24". National Space Science Data Center Catalog. NASA. Retrieved 13 October 2018.
the mission successfully collected 170.1 grams of lunar samples and deposited them into a collection capsule
- "Meteoritical Bulletin Database — Lunar Meteorite search results". Meteoritical Bulletin Database. The Meteoritical Society. 15 August 2017. Retrieved 17 August 2017.
- "List of Lunar Meteorites - Feldspathic to Basaltic Order". meteorites.wustl.edu. Retrieved 30 March 2018.
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- "NASA - NSSDC - Spacecraft - Details". nssdc.gsfc.nasa.gov. Archived from the original on 2012-09-28. Retrieved 2015-11-08.
- James Papike; Grahm Ryder & Charles Shearer (1998). "Lunar Samples". Reviews in Mineralogy and Geochemistry. 36: 5.1–5.234.
- H. Hiesinger, J. W. Head, U. Wolf, R. Jaumann, and G. Neukum, H. (2003). "Ages and stratigraphy of mare basalts in Oceanus Procellarum, Mare Numbium, Mare Cognitum, and Mare Insularum". J. Geophys. Res. 108: 5065. Bibcode:2003JGRE..108.5065H. doi:10.1029/2002JE001985.
- Bhanoo, Sindya N. (28 December 2015). "New Type of Rock Is Discovered on Moon". New York Times. Retrieved 29 December 2015.
- "Exploring the Moon -- A Teacher's Guide with Activities, NASA EG-1997-10-116 - Rock ABCs Fact Sheet" (PDF). NASA. November 1997. Retrieved 19 January 2014.
- Orloff, Richard W. (September 2004) [First published 2000]. "Extravehicular Activity". Apollo by the Numbers: A Statistical Reference. NASA History Division, Office of Policy and Plans. The NASA History Series. Washington, D.C.: NASA. ISBN 0-16-050631-X. LCCN 00061677. NASA SP-2000-4029. Retrieved August 1, 2013.
- Astromaterials Research & Exploration Science. "70017 Ilmenite Basalt" (PDF). NASA.
- "Where are the Apollo 17 Goodwill Moon Rocks?". Collect Space.
|Wikimedia Commons has media related to Lunar samples.|
- Rocks & Soils from the Moon — Johnson Space Center
- Apollo Geology Tool Catalog
- Lunar meteorites — Washington University, Department of Earth and Planetary Sciences
- Lunar Samples Lunar and Planetary Institute
- Articles about Moon rocks in Planetary Science Research Discoveries educational journal
- Where Today are the Apollo 11 Lunar Sample Displays? collectSPACE
- Where Today are the Apollo 17 Goodwill Moon Rocks? collectSPACE
- Kentucky's lunar sample displays in the Kentucky Historical Society objects catalog: Apollo 11, Apollo 17