{"product_id":"laayoune-002-lunar-meteorite-end-cut-feldspathic-breccia-116-40g-mirror-polished-moon-rock","title":"Laayoune 002 Lunar Meteorite End Cut, Feldspathic Breccia, 116.40g, Mirror Polished Moon Rock","description":"\u003ch2\u003eAbout this specimen\u003c\/h2\u003e\n\n\u003cp\u003eThis is a 116.40 g end cut of Laayoune 002, a lunar feldspathic breccia recovered in Western Sahara. The Meteoritical Bulletin Database records the recommended classification as Lunar (feldsp. breccia), the find as January 2022, and the country as Western Sahara. The name was approved on 19 March 2022 and the meteorite was published in Meteoritical Bulletin 111.\u003c\/p\u003e\n\n\u003cp\u003eThe form matters here as much as the mass. An end cut of this weight presents a single large polished face rather than the same material divided across several thin slices. On a breccia, that face is the specimen: everything worth looking at is the clast population exposed by the cut.\u003c\/p\u003e\n\n\u003ch2\u003eStructure and features\u003c\/h2\u003e\n\n\u003cp\u003eThe cut face is mirror polished and carries a lot going on. The groundmass runs warm, through browns, tans and olive tones into gray blue, and it is crossed throughout by a dense network of pale veining that branches across the whole face. Angular clasts sit in that network at every scale, from pieces large enough to read individually down to fragments that only resolve under magnification, and they range from near white through buff and orange brown to dark inclusions that read almost black against the surrounding rock. The macro photographs above are of this specimen and show that texture at working distance.\u003c\/p\u003e\n\n\u003cp\u003eThe Bulletin writeup describes both recovered stones as lacking fusion crust, with an overall gray color and whitish clasts visible. That describes the outside of the stones. The interior exposed by this cut is considerably more varied than the exterior suggests, which is the usual reason for cutting a breccia in the first place.\u003c\/p\u003e\n\n\u003cp\u003eThe reverse of the specimen is left uncut and retains the natural exterior surface of the stone, so the piece shows both the polished interior and the original outer face.\u003c\/p\u003e\n\n\u003cp\u003eThe published petrography, carried out by A. Irving at the University of Washington and P. Carpenter at Washington University in St. Louis, records a breccia composed of mineral clasts of anorthite, olivine, orthopyroxene, pigeonite and augite, with accessory ilmenite and chromite of variable titanium content and minor secondary barite. The anorthite is highly calcic at An96.1 to An97.7.\u003c\/p\u003e\n\n\u003cp\u003eThe Bulletin records the shock stage as low and the weathering grade as low. For desert-recovered lunar material that combination is worth noting, because it is what keeps the clast boundaries legible rather than blurred by terrestrial alteration.\u003c\/p\u003e\n\n\u003ch2\u003eDiscovery and provenance\u003c\/h2\u003e\n\n\u003cp\u003eThe Bulletin writeup records that the meteorite was found near Laayoune in January 2022 and purchased from the finder by Aziz Habibi. Two stones were recovered, of 3,680 g and 1,468 g, for a total known weight of 5.15 kg. Recorded coordinates are 27.070 degrees N, 13.202 degrees W, in Saguia el Hamra, Western Sahara. The place of purchase is recorded as Agadir and the work name as AH 709, submitted by A. Irving.\u003c\/p\u003e\n\n\u003cp\u003eThe type specimen is a 20.7 g polished end cut held at the University of Washington, Burke Museum of Natural History and Culture. The Bulletin records the main mass as held by A. Habibi.\u003c\/p\u003e\n\n\u003cp\u003eThis specimen was acquired by Treasure Coast Meteorite Co. and prepared as a mirror polished end cut. It carries serial TC-00040 and a permanent specimen record page.\u003c\/p\u003e\n\n\u003ch2\u003eScientific context\u003c\/h2\u003e\n\n\u003cp\u003eFeldspathic breccias sample the lunar highlands, the light colored anorthositic crust that covers most of the Moon and forms the pale regions visible from Earth without a telescope. That crust is understood to have formed by the flotation of plagioclase in a global magma ocean early in lunar history. The very calcic anorthite recorded in this meteorite, at An96.1 to An97.7, is the signature of that process.\u003c\/p\u003e\n\n\u003cp\u003eA breccia is rock assembled from fragments of older rock, welded together by impact. Every clast on this face is a separate piece of lunar crust that existed before the impact that bound them, so the specimen is a sample of several lunar rocks at once rather than one. That is why the exposed area of a cut matters on this material in a way it does not on a homogeneous stone.\u003c\/p\u003e\n\n\u003cp\u003eFeldspathic breccias are the most common lunar meteorite type, accounting for a large share of all lunar entries in the Bulletin database. Background on how this material leaves the Moon and reaches Earth is set out in \u003ca href=\"\/de\/pages\/what-is-a-lunar-meteorite\"\u003ewhat is a lunar meteorite\u003c\/a\u003e, and the shape of the wider lunar population is covered in \u003ca href=\"\/de\/pages\/the-largest-lunar-meteorites\"\u003ethe largest lunar meteorites\u003c\/a\u003e.\u003c\/p\u003e\n\n\u003ch2\u003eFrequently asked questions\u003c\/h2\u003e\n\n\u003cp\u003e\u003cstrong\u003eIs this actually material from the Moon?\u003c\/strong\u003e\u003cbr\u003e\nYes. Laayoune 002 is a formally classified lunar meteorite with an entry in the Meteoritical Bulletin Database, published in Meteoritical Bulletin 111 and classified by A. Irving and P. Carpenter. Lunar identification rests on mineral chemistry and oxygen isotopes rather than on appearance.\u003c\/p\u003e\n\n\u003cp\u003e\u003cstrong\u003eWhy is there no fusion crust?\u003c\/strong\u003e\u003cbr\u003e\nThe Bulletin writeup records that both recovered stones lack fusion crust. Crust is thin and is among the first features lost to terrestrial weathering and to the abrasion of a desert surface. Its absence says nothing about authenticity, which rests on the laboratory classification.\u003c\/p\u003e\n\n\u003cp\u003e\u003cstrong\u003eWhat are the whitish clasts?\u003c\/strong\u003e\u003cbr\u003e\nFragments of lunar highlands rock. The published petrography records mineral clasts of anorthite, olivine, orthopyroxene, pigeonite and augite. The pale material is dominated by calcic anorthite, the plagioclase feldspar that makes up the bright highlands crust.\u003c\/p\u003e\n\n\u003cp\u003e\u003cstrong\u003eIs it legal to own a piece of the Moon?\u003c\/strong\u003e\u003cbr\u003e\nYes. Lunar meteorites arrived on Earth naturally and can be bought and sold where the source country permits export. Material returned by the Apollo missions is United States government property and cannot be privately owned. This is covered in \u003ca href=\"\/de\/pages\/can-you-legally-buy-a-moon-rock\"\u003ecan you legally buy a moon rock\u003c\/a\u003e.\u003c\/p\u003e\n\n\u003cp\u003e\u003cstrong\u003eWas Laayoune 002 seen to fall?\u003c\/strong\u003e\u003cbr\u003e\nNo. The Bulletin database records it as a find, with a find date of January 2022.\u003c\/p\u003e\n\n\u003cp\u003e\u003cstrong\u003eWhat documentation comes with it?\u003c\/strong\u003e\u003cbr\u003e\nA certificate card bearing serial TC-00040, and a permanent specimen record page on this site giving the identification and classification data, the recorded weight, and photographs of this specimen.\u003c\/p\u003e\n\n\u003ch2\u003eCollector significance\u003c\/h2\u003e\n\n\u003cp\u003eMost lunar material offered to collectors is measured in single grams or fractions of a gram. At 116.40 g this is a substantially larger holding, and the end cut form concentrates that mass into one continuous polished face rather than dividing it.\u003c\/p\u003e\n\n\u003cp\u003eThe material also carries a full published record. The classification, the petrography, the mineral chemistry, the find coordinates, the two recovered masses and the location of the type specimen are all in the Bulletin and can be checked against this listing line by line. That is the difference between a specimen described in adjectives and one measured against the published record.\u003c\/p\u003e\n\n\u003cp\u003eThis specimen is offered through white glove service. Offered by Treasure Coast Meteorite Co., IMCA Member #3323, Hobe Sound, Florida. Further lunar material is listed in the \u003ca href=\"\/de\/collections\/lunar-meteorites\"\u003elunar meteorite collection\u003c\/a\u003e. Classification data on this page is reproduced from the \u003ca href=\"https:\/\/www.lpi.usra.edu\/meteor\/metbull.cfm?code=77253\" rel=\"noopener\" target=\"_blank\"\u003eMeteoritical Bulletin Database entry for Laayoune 002\u003c\/a\u003e and from Meteoritical Bulletin 111, \u003ca href=\"https:\/\/doi.org\/10.1111\/maps.13995\" rel=\"noopener\" target=\"_blank\"\u003edoi:10.1111\/maps.13995\u003c\/a\u003e, maintained by the Nomenclature Committee of the \u003ca href=\"https:\/\/meteoritical.org\/\" rel=\"noopener\" target=\"_blank\"\u003eMeteoritical Society\u003c\/a\u003e and hosted by the \u003ca href=\"https:\/\/www.lpi.usra.edu\/\" rel=\"noopener\" target=\"_blank\"\u003eLunar and Planetary Institute\u003c\/a\u003e. How that database works is explained in \u003ca href=\"\/de\/pages\/meteoritical-bulletin-explained\"\u003eunderstanding the Meteoritical Bulletin\u003c\/a\u003e.\u003c\/p\u003e","brand":"Treasure Coast Meteorite Co.","offers":[{"title":"Default Title","offer_id":46126165229615,"sku":"LAAYOUNE-002-116.40G-ENDCUT","price":8148.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0726\/9724\/9839\/files\/laayoune-002-lunar-feldspathic-breccia-116.40g-polished-face-lightbox.jpg?v=1788534084","url":"https:\/\/www.tcmeteorites.com\/de\/products\/laayoune-002-lunar-meteorite-end-cut-feldspathic-breccia-116-40g-mirror-polished-moon-rock","provider":"Treasure Coast Meteorite Co.","version":"1.0","type":"link"}