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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


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.
Reference: Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).
Anorthite var. Bytownite
Formula: (Ca,Na)[Al(Al,Si)Si2O8]
Description: Most common plagioclase composition.
Reference: Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).
Chromite
Formula: Fe2+Cr3+2O4
Reference: Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).
'Clinopyroxene Subgroup'
Description: Both Ca-poor clinopyroxene and diopside are present.
Reference: Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).
Diopside
Formula: CaMgSi2O6
Description: As occasional rims on orthopyroxene.
Reference: Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).
'Fayalite-Forsterite Series'
Reference: Kraut, F. & Fredriksson, K. (1971) Hedjaz, an L-3, L-4, L-5 and L-6 chondrite. Meteoritics 6: p. 284.; Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).; Misawa, K. & Nakamura, N. (1987) The Hedjaz Meteorite: REE Abundances in Chondrules and Lithic Fragments: Abstracts of the Lunar and Planetary Science Conference, volume 18, page 645.
'Glass'
Reference: Kraut, F. & Fredriksson, K. (1971) Hedjaz, an L-3, L-4, L-5 and L-6 chondrite. Meteoritics 6: p. 284.; Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).
Graphite
Formula: C
Description: Rare.
Reference: Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).
Ilmenite
Formula: Fe2+TiO3
Reference: Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).
Iron
Formula: Fe
Reference: Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).
Iron var. Kamacite
Formula: (Fe,Ni)
Reference: Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).
Merrillite
Formula: Ca9NaMg(PO4)7
Reference: Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).; Misawa, K. & Nakamura, N. (1987) The Hedjaz Meteorite: REE Abundances in Chondrules and Lithic Fragments: Abstracts of the Lunar and Planetary Science Conference, volume 18, page 645.
'Orthopyroxene Subgroup'
Reference: Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).
'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
Description: Occasional albite twinning plus rare instances of pericline twinning.
Reference: Kraut, F. & Fredriksson, K. (1971) Hedjaz, an L-3, L-4, L-5 and L-6 chondrite. Meteoritics 6: p. 284.; Misawa, K. & Nakamura, N. (1987) The Hedjaz Meteorite: REE Abundances in Chondrules and Lithic Fragments: Abstracts of the Lunar and Planetary Science Conference, volume 18, page 645.
Spinel
Formula: MgAl2O4
Description: Usually as Cr-rich spinel.
Reference: Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).
Taenite
Formula: (Fe,Ni)
Reference: Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).
Tridymite
Formula: SiO2
Description: In acicular pyroxene chondrules.
Reference: Kraut, F. & Fredriksson, K. (1971) Hedjaz, an L-3, L-4, L-5 and L-6 chondrite. Meteoritics 6: p. 284.; Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).
Troilite
Formula: FeS
Reference: Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986).

Gallery:

List of minerals arranged by Strunz 10th Edition classification

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

List of minerals for each chemical element

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

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Mason, B.H. (1963) Olivine composition in chondrites. Geochimica et Cosmochimica Acta 27, 1011-1023.
Kraut, F. & Fredriksson, K. (1971) Hedjaz, an L-3, L-4, L-5 and L-6 chondrite. Meteoritics 6: p. 284.
Fredriksson, K., Fredriksson, B. J. & Kraut, F. (1986) The Hedjaz meteorite: Meteoritics 21(2): 159-168. (June 1986)
Misawa, K. & Nakamura, N. (1987) The Hedjaz Meteorite: REE Abundances in Chondrules and Lithic Fragments: Abstracts of the Lunar and Planetary Science Conference, volume 18, page 645.
Mittlefehldt, D.W. & 3 others (1998) Non-Chondritic Meteorites from Asteroidal Bodies. In: Planetary Materials (Papike, JJ - Ed.), Chapter 3: 1-398: Mineralogical Society of America, Washington, DC, USA.
Grady, M.M. (2000). Catalogue of Meteorites (5/e). Cambridge University Press: Cambridge; New York; Oakleigh; Madrid; Cape Town. 689 pages.

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