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Itqiy meteorite, al-Saqiyah al-Hamra'a (Saguia el Hamra), Western Saharai
| Regional Level Types | |
|---|---|
| Itqiy meteorite | Meteorite Fall Location |
| al-Saqiyah al-Hamra'a (Saguia el Hamra) | Wadi |
| Western Sahara | Disputed Territory |
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Latitude & Longitude (WGS84):
26° 35' 26'' North , 12° 57' 7'' West
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Primitive Enstatite Achondrite [or Shock-melted Enstatite Chondrite]
1990 fall. 2 pieces, 410g and 4310g.
After a striking burst of light-and-sound, a 410 g stone was recovered by a nomad. A decade later a 4.31 kg stone was recovered — and the news of Itqiy spread.
The dominant constituent of Itqiy is enstatite accompanied by kamacite (~ 25 vol%) and tiny kamacite-sulfide intergrowths. The very reduced mineralogy, the oxygen isotopes, and the cosmic ray exposure age all indicate that Itqiy is a member of the Enstatite-rich meteorite clan, initially described as an Enstatite chondrite, but beyond that classification is elusive. The enstatite resembles that of EL chondrites, but the metal is closer in composition to that of EH chondrites. Furthermore, Itqiy lacks chondrules and chondrule relics. This may be entirely due to impact melting from pre-terrestrial shock, but that is a hypothesis — not a conclusion. To begin with, there is apparently no consensus on the level of shock.
The actual issues are deeper than that. Over two decades ago Klaus Keil (1989) argued that the Enstatite meteorites were derived from a minimum of four parent bodies (EH and EL chondrites, normal aubrites, and the Shallowater parent body). Recently, however, it has become increasingly difficult to accommodate several Enstatite meteorites into the four homeworld framework. Worlds that have been completely melted (e.g., Happy Canyon, Itqiy, NWA 2526) are especially difficult to understand. First, disentangling the effects of internally generated metamorphism from external shock(s) is difficult. Secondly, it is not clear whether all of the Enstatite-rich oddballs are derived from the four putative homeworlds. Recently, Keil and Bischoff (2008) have proposed that Itqiy and NWA 2526 may be derived from a fifth parent body.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
9 valid minerals.
Meteorite/Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Alabandite Formula: MnS |
| ⓘ Daubréelite Formula: Fe2+Cr3+2S4 |
| ⓘ Enstatite Formula: Mg2Si2O6 |
| ⓘ Native Iron Formula: Fe |
| ⓘ Native Iron var. Kamacite Formula: (Fe,Ni) |
| ⓘ Niningerite Formula: MgS |
| ⓘ Oldhamite Formula: CaS |
| ⓘ Perryite ? Formula: (Ni,Fe)5(Si,P)2 |
| ⓘ Schreibersite ? Formula: (Fe,Ni)3P |
| ⓘ Troilite Formula: FeS |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Iron | 1.AE.05 | Fe |
| ⓘ | var. Kamacite | 1.AE.05 | (Fe,Ni) |
| ⓘ | Perryite ? | 1.BB.10 | (Ni,Fe)5(Si,P)2 |
| ⓘ | Schreibersite ? | 1.BD.05 | (Fe,Ni)3P |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Troilite | 2.CC.10 | FeS |
| ⓘ | Alabandite | 2.CD.10 | MnS |
| ⓘ | Niningerite | 2.CD.10 | MgS |
| ⓘ | Oldhamite | 2.CD.10 | CaS |
| ⓘ | Daubréelite | 2.DA.05 | Fe2+Cr3+2S4 |
| Group 9 - Silicates | |||
| ⓘ | Enstatite | 9.DA.05 | Mg2Si2O6 |
List of minerals for each chemical element
| O | Oxygen | |
|---|---|---|
| O | ⓘ Enstatite | Mg2Si2O6 |
| Mg | Magnesium | |
| Mg | ⓘ Enstatite | Mg2Si2O6 |
| Mg | ⓘ Niningerite | MgS |
| Si | Silicon | |
| Si | ⓘ Enstatite | Mg2Si2O6 |
| Si | ⓘ Perryite | (Ni,Fe)5(Si,P)2 |
| P | Phosphorus | |
| P | ⓘ Perryite | (Ni,Fe)5(Si,P)2 |
| P | ⓘ Schreibersite | (Fe,Ni)3P |
| S | Sulfur | |
| S | ⓘ Alabandite | MnS |
| S | ⓘ Daubréelite | Fe2+Cr23+S4 |
| S | ⓘ Niningerite | MgS |
| S | ⓘ Oldhamite | CaS |
| S | ⓘ Troilite | FeS |
| Ca | Calcium | |
| Ca | ⓘ Oldhamite | CaS |
| Cr | Chromium | |
| Cr | ⓘ Daubréelite | Fe2+Cr23+S4 |
| Mn | Manganese | |
| Mn | ⓘ Alabandite | MnS |
| Fe | Iron | |
| Fe | ⓘ Daubréelite | Fe2+Cr23+S4 |
| Fe | ⓘ Native Iron | Fe |
| Fe | ⓘ Native Iron var. Kamacite | (Fe,Ni) |
| Fe | ⓘ Perryite | (Ni,Fe)5(Si,P)2 |
| Fe | ⓘ Schreibersite | (Fe,Ni)3P |
| Fe | ⓘ Troilite | FeS |
| Ni | Nickel | |
| Ni | ⓘ Native Iron var. Kamacite | (Fe,Ni) |
| Ni | ⓘ Perryite | (Ni,Fe)5(Si,P)2 |
| Ni | ⓘ Schreibersite | (Fe,Ni)3P |
Other Databases
| Wikipedia: | https://en.wikipedia.org/wiki/Itqiy_meteorite |
|---|---|
| Wikidata ID: | Q1449768 |
Other Regions, Features and Areas containing this locality
AfricaContinent
African PlateTectonic Plate
- Aaiun-Tarfaya basinBasin
- MauritanidesOrogenic Belt
North Africa
- Sahara DesertDesert
Northwest Africa MeteoritesGroup of Meteorite Fall Locations
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Itqiy meteorite, al-Saqiyah al-Hamra'a, Western Sahara