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Hedjaz meteorite (Et-tlahi), Tabuk Region, Saudi Arabiai
Regional Level Types
Hedjaz meteorite (Et-tlahi)- not defined -
Tabuk RegionRegion
Saudi ArabiaCountry

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Latitude & Longitude (WGS84):
27° 36' North , 35° 40' East
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Duba22,000 (2016)27.7km
Mindat Locality ID:
266467
Long-form identifier:
mindat:1:2:266467:8
GUID (UUID V4):
0


Ordinary chondrite, unequilibrated & brecciated (L3.7-6, br.)
Fell, Autumn 1910; 6.1 kg, 4 stones

The oddities of the chondritic stone which fell during the night nearly a century ago have, so to speak, only slowly come to light. The primary constituents of the Hedjaz meteorite are normal ingredients of the L chondrites — the olivine and/or pyroxene-rich chondrules are prominent and usually distinct. And, within both chondrules and matrix are the usual ingredients — olivine, pyroxene, plagioclase, troilite, kamacite, and taenite — expected in any moderately large, unweathered chondrite fall. Small amounts of accessory chromite, merrillite, and ilmenite are present as well. The olivine is mostly equilibrated, but the pyroxene is much more variable and small amounts of glass are present. The latter features are those we find in unequilibrated chondrites. But Hedjaz is not a normal unequilibrated chondrite which has never experienced substantial metamorphism. Unincorporated, unequilibrated, even exotic inclusions are found — but next to the unmetamorphosed materials are equally prominent partially to fully equilibrated clasts with L4, L5, and L6 lithologies. Textures and variability of the Fe-Ni metal is equally prominent — kamacite and taenite occur separately, together, and occasionally with troilite. Dark veins and other shock features are striking. Being, perhaps, somewhat more precise than the usual standard terminology, we might say that Hedjaz is a brecciated mixture of unequilibrated, partially equilibrated, and equilibrated L chondrite chondrules and clasts.

Among the 44 witnessed unequilibrated ordinary chondrite falls, only Hedjaz is labelled specifically as an L3.7—6. Indeed, no other meteorite — fall or find — is classified as L3.7—6. Among the total 2508 recovered unequilibrated ordinary chondrites only Asuka 880956 — listed as an H3.7-6 — appears to have such a wide, but yet specifically limited range of the unequilibrated and the equilibrated.

The main Hedjaz mass has been at the Museum National d'Histoire Naturelle in Paris.

Nota bene: The geographical coordinates provided by the Meteoritical Bulletin Database are over the waters of the Red Sea.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


11 valid minerals.

Detailed Mineral List:

ⓘ Anorthite
Formula: Ca(Al2Si2O8)
Description: Most common plagioclase composition.
ⓘ Anorthite var. Bytownite
Formula: (Ca,Na)[Al(Al,Si)Si2O8]
Description: Most common plagioclase composition.
ⓘ Chromite
Formula: Fe2+Cr3+2O4
ⓘ 'Clinopyroxene Subgroup'
Description: Both Ca-poor clinopyroxene and diopside are present.
ⓘ Diopside
Formula: CaMgSi2O6
Description: As occasional rims on orthopyroxene.
ⓘ 'Fayalite-Forsterite Series'
ⓘ 'Glass'
ⓘ Graphite
Formula: C
Description: Rare.
ⓘ Ilmenite
Formula: Fe2+TiO3
ⓘ Merrillite
Formula: Ca9NaMg(PO4)7
ⓘ Native Iron
Formula: Fe
ⓘ Native Iron var. Kamacite
Formula: (Fe,Ni)
ⓘ 'Orthopyroxene Subgroup'
ⓘ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
Description: Occasional albite twinning plus rare instances of pericline twinning.
ⓘ Spinel
Formula: MgAl2O4
Description: Usually as Cr-rich spinel.
ⓘ Taenite
Formula: (Fe,Ni)
ⓘ Tridymite
Formula: SiO2
Description: In acicular pyroxene chondrules.
ⓘ Troilite
Formula: FeS

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘNative Iron1.AE.05Fe
ⓘvar. Kamacite1.AE.05(Fe,Ni)
ⓘTaenite1.AE.10(Fe,Ni)
ⓘGraphite1.CB.05aC
Group 2 - Sulphides and Sulfosalts
ⓘTroilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
ⓘChromite4.BB.05Fe2+Cr3+2O4
ⓘSpinel4.BB.05MgAl2O4
ⓘIlmenite4.CB.05Fe2+TiO3
ⓘTridymite4.DA.10SiO2
Group 8 - Phosphates, Arsenates and Vanadates
ⓘMerrillite8.AC.45Ca9NaMg(PO4)7
Group 9 - Silicates
ⓘDiopside9.DA.15CaMgSi2O6
ⓘAnorthite9.FA.35Ca(Al2Si2O8)
ⓘvar. Bytownite9.FA.35(Ca,Na)[Al(Al,Si)Si2O8]
Unclassified
ⓘ'Clinopyroxene Subgroup'-
ⓘ'Fayalite-Forsterite Series'-
ⓘ'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
ⓘ'Orthopyroxene Subgroup'-
ⓘ'Glass'-

List of minerals for each chemical element

CCarbon
Cⓘ GraphiteC
OOxygen
Oⓘ AnorthiteCa(Al2Si2O8)
Oⓘ Anorthite var. Bytownite(Ca,Na)[Al(Al,Si)Si2O8]
Oⓘ ChromiteFe2+Cr23+O4
Oⓘ DiopsideCaMgSi2O6
Oⓘ IlmeniteFe2+TiO3
Oⓘ SpinelMgAl2O4
Oⓘ TridymiteSiO2
Oⓘ MerrilliteCa9NaMg(PO4)7
Oⓘ Fayalite-Forsterite Series
Oⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
NaSodium
Naⓘ Anorthite var. Bytownite(Ca,Na)[Al(Al,Si)Si2O8]
Naⓘ MerrilliteCa9NaMg(PO4)7
Naⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgⓘ DiopsideCaMgSi2O6
Mgⓘ SpinelMgAl2O4
Mgⓘ MerrilliteCa9NaMg(PO4)7
Mgⓘ Fayalite-Forsterite Series
AlAluminium
Alⓘ AnorthiteCa(Al2Si2O8)
Alⓘ Anorthite var. Bytownite(Ca,Na)[Al(Al,Si)Si2O8]
Alⓘ SpinelMgAl2O4
Alⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Siⓘ AnorthiteCa(Al2Si2O8)
Siⓘ Anorthite var. Bytownite(Ca,Na)[Al(Al,Si)Si2O8]
Siⓘ DiopsideCaMgSi2O6
Siⓘ TridymiteSiO2
Siⓘ Fayalite-Forsterite Series
Siⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
PPhosphorus
Pⓘ MerrilliteCa9NaMg(PO4)7
SSulfur
Sⓘ TroiliteFeS
CaCalcium
Caⓘ AnorthiteCa(Al2Si2O8)
Caⓘ Anorthite var. Bytownite(Ca,Na)[Al(Al,Si)Si2O8]
Caⓘ DiopsideCaMgSi2O6
Caⓘ MerrilliteCa9NaMg(PO4)7
Caⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
TiTitanium
Tiⓘ IlmeniteFe2+TiO3
CrChromium
Crⓘ ChromiteFe2+Cr23+O4
FeIron
Feⓘ ChromiteFe2+Cr23+O4
Feⓘ IlmeniteFe2+TiO3
Feⓘ Native IronFe
Feⓘ Native Iron var. Kamacite(Fe,Ni)
Feⓘ Taenite(Fe,Ni)
Feⓘ TroiliteFeS
Feⓘ Fayalite-Forsterite Series
NiNickel
Niⓘ Native Iron var. Kamacite(Fe,Ni)
Niⓘ Taenite(Fe,Ni)

Other Regions, Features and Areas containing this locality

Arabian PlateTectonic Plate
AsiaContinent

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