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Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!


Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!
Meteorite**Tarda, C2-Ung.**0.193 gram, NEW FALL MOROCCO 08/25/2020; Ultra Rare!!


$39.99 Buy It Now or Best Offer
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Seller Store matt992011
(3558) 100.0%,

Location: Riverside, California
Ships to: US,
Item: 267024374213

All returns accepted:ReturnsNotAccepted
Country/Region of Manufacture:Morocco

Tarda Meteorite: A Unique Treasure for Collectors The Tarda meteorite, a striking example of the cosmos, hails from Morocco and is an exceptional find for any collector of unique and fascinating items. This ultra-rare meteorite, weighing a mere 0.193 grams, provides a glimpse into the universe’s secrets while also being a remarkable aesthetic piece for display. **Classification and Composition** The Tarda meteorite is classified as a C2-Ungrouped carbonaceous chondrite, making it a distinct and significant specimen within the meteorite community. Carbonaceous chondrites are among the most primitive types of meteorites, believed to contain organic compounds and water, offering insights into the early solar system’s formation and the building blocks of life. The “C2” classification pertains to its chemical composition and mineralogy, highlighting its carbon content, while “Ungrouped” denotes its unique characteristics that do not fit into established classification groups. This makes Tarda particularly valuable to researchers and enthusiasts alike, as it represents a rare opportunity to study a type of meteorite that is not often obtained. **Historical Context** The Tarda meteorite fell on August 25th, 2020, a testament to its recent arrival from the vastness of space. Freshly fallen specimens like Tarda are invaluable for scientific analysis, as they have not undergone extensive terrestrial weathering, allowing for a more accurate study of their original properties. **Aesthetic Appeal** One of the standout features of the Tarda meteorite is its exquisite fresh black fusion crust. This crust is formed when a meteorite enters the Earths atmosphere at high speeds, causing the exterior to melt and subsequently solidify upon cooling. The striking appearance of Tarda, with its glossy black surface, makes it not only a scientific treasure but also an eye-catching display piece. **Included Documentation and Display** To enhance its value, the Tarda meteorite comes with a Certificate of Authenticity (COA) card, ensuring its legitimacy and providing provenance. Additionally, it is accompanied by a display case, allowing collectors to showcase this extraordinary specimen with pride. For collectors and enthusiasts, the Tarda meteorite is more than just a specimen; it is a rare artifact from the cosmos with a fascinating story. Its designation as a C2-Ungrouped carbonaceous chondrite elevates its status within the community, making it a coveted piece for anyone passionate about outer space and the mysteries it holds. Don’t miss the opportunity to own this ultra-rare meteorite; Tarda is truly a must-have for any serious collection. Name: Tarda This is an OFFICIAL meteorite name. Abbreviation: There is no official abbreviation for this meteorite. Observed fall: Yes, confirmed fall Year fell: 2020 Country: Morocco Mass: 4 kg Tarda Basic informationName: Tarda This is an OFFICIAL meteorite name. Abbreviation: There is no official abbreviation for this meteorite. Observed fall: Yes, confirmed fall Year fell: 2020 Country: Morocco Mass:help 4 kg Classification history: Meteoritical Bulletin: MB 109 (2020) C2-ung Recommended: C2-ung This is 1 of 27 approved meteorites classified as C2-ung. Search for other: Carbonaceous chondrites, Carbonaceous chondrites (type 2), and Ungrouped chondrites Comments:Approved 14 Oct 2020 Writeuphelp Writeup from MB 109: Tarda 31 49′ 35″N, 4 40′ 46″W Morocco Confirmed fall: 2020 Classification: Carbonaceous chondrite (C2, ungrouped) History: (H. Chennaoui Aoudjehane, FSAC, ATTARIK Foundation: A. Aaronson) On Tuesday, 25 August 2020, around 2:30 pm Moroccan time (GMT+1) a fireball was widely witnessed by people in southern Morocco from Alnif, Zagora, Tazarine, and Rich. The fireball trajectory was from the SW to NE. A search was immediately undertaken by local residents and meteorite hunters between Goulmima and Errachidia. Hundreds of people began searching on the same day, and the first piece was found the following day by Alalou Youssef close to his village of Tarda. The fall location is crossed by the national road linking Ouarzazate to Errachidia, and because of the easy access thousands of people soon traveled to the area. National TV channels Al Oula and 2M recorded the activity. A field mission was organized to the fall site on 27 and 28 August 2020, with Dr Mohamed Aoudjehane, Prof. Faouziya Haissen and Prof. Hasnaa Chennaoui (members of the board of directors of ATTARIK Foundation), with the support of Prof. Hicham Si Mhamdi (Faculty of Sciences, Errachidia), Adam Aaronson and members of the Moroccan Association of Meteorites (Ahmed Bouferra, Mohamed and Zaid El Guireh). Several eyewitnesses from areas up to 150 km away were interviewed, and reported three ” of a bright yellow, barrel-sized fireball with green edges. The meteor was followed by a thick trail of white smoke that remained suspended for several seconds. The fireball was reported to release little pieces around its edges, witnesses said the fireball was accompanied by a whistle, followed by multiple detonations. One eyewitness reported an almost vertical trajectory. Thousands of small, mostly complete stones were collected ranging from only a few milligrams to 99 g. Many pieces were recovered by hunters using magnets. The strewn field is about 3 km long and situated ~10 km east of Tarda centered at 31.8265N, 4.6794W. Physical characteristics: Hundreds of small to medium-sized fusion crusted stones ranging from 0.1 g to 99 g. The majority of the fusion-crusted stones are <1 g. Some flight-oriented stones show a blue iridescence on their trailing edge, similar to that observed with Aguas Zarcas. Many stones shattered upon impact with the ground. The stones have low density, are somewhat friable, and are particularly susceptible to moisture, and rapidly slake in contact with water or alcohol. Freshly picked up stones were said to have a charcoal-like odor. Small fragments crushed in water emit a powerful tar-like odor. The interiors of the stones are dull black with dispersed white or light-colored grains or clasts (up to ~1 mm in size). Magnetic susceptibility log ( 10-9 m3/kg) = 4.99, 4.83, 5.03 (A. Irving, UWS), 4.80 (H. Chennaoui Aoudjehane, FSAC), 4.96 (D. Sheikh, FSU); average 4.920.10, n=5. Petrography: (A. Irving, UWS; P. Carpenter, WUSL; L. Garvie, ASU; D. Sheikh, FSU) Optical and electron microprobe observations of three fragments in polished thin sections reveal a matrix-rich breccia containing small chondrules (granular, BO) and chondrule fragments, very fine grained AOA, grains of forsterite (exhibiting slight undulose extinction) and other clasts set in a dominant fine-grained matrix (~80 vol.%, opaque in thin section). Chondrule sizes measured in two thin sections: 310150 m, n=10; 450200 m, n=5. No CAIs were identified. The dominant chondrule phase is forsterite (but spinel is present in two examples), and some are mantled by forsterite dust or exhibit partial replacement by Fe-Mn-dolomite, siderite or phyllosilicate material. A single igneous achondrite clast with subophitic texture was observed, and consists predominantly (~75 vol.%) of laths of twinned anorthite with subordinate forsterite, enstatite and minor diopside. Electron microprobe surveys of thin sections and powder X-ray diffraction studies of several ~20 mg fragments show that the matrix is dominated by phyllosilicates, with lesser magnetite, pyrrhotite, pentlandite, troilite, carbonates (Fe-Mn-dolomite, Mg-rich siderite and siderite), and olivine. The phyllosilicates show broad basal reflections at 14.7 and 7.4 , consistent with smectite and serpentine or interstratified serpentine/smectite, respectively. No reflections for sulfates were recognized. Magnetite (<20 m) is scattered throughout the sample in the form of framboids, platelets, and individual spherules; other accessory phases identified in the matrix by EPMA are troilite, Ni-bearing pyrrhotite, chromite and very rare kamacite. Classification: (C. Agee, UNM; K. Ziegler, UNM; A. Irving, UWS; L. Garvie, ASU; D. Sheikh, FSU; P. Carpenter, WUSL; H. Chennaoui Aoudjehane, FSAC; M. Zolensky, JSC; P. Schmitt-Kopplin, HZM) Carbonaceous chondrite (C2-ungrouped). The bulk mineralogy is consistent with a petrologic grade 2, based on the predominance of smectite and serpentine together with the presence of anhydrous mafic silicates, AOA, and chondrules. The oxygen isotopes give a bimodal distribution of the 18O-values, with one group having values somewhat like those of the CI chondrites, and the other group like values for the Yamato-type (CY) carbonaceous chondrites (King et al., 2019). However, 17O values are lower than those for CI and CY chondrites, and plot below the TFL. These isotopic values do not overlap with those of any established carbonaceous chondrite group, hence the ungrouped designation.

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