Log In
Ergheo meteorite, Lower Shabelle Region, Somaliai
| Regional Level Types | |
|---|---|
| Ergheo meteorite | Meteorite Fall Location |
| Lower Shabelle Region | Region |
| Somalia | Country |
This page is currently not sponsored. Click here to sponsor this page.
Latitude & Longitude (WGS84):
1° 10' 22'' North , 44° 5' 35'' East
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Name(s) in local language(s):
, Soomaaliya (الصومال; aṣ-Ṣūmāl)
Ordinary chondrite, veined (L5)
Fell, July 1889; 20.375 kg.
Baldanza described the location of the find as "Ergheo, Brava, Somaliland".
The port town of Brava is now also known as Barawa (Baraawe).
A single stone fell and was left where it lay for several years. The moderately equilibrated interior is characterized by indistinct chondrules with small metal grains. Widespread wavy extinction is present within mineral grains and interstitial maskelynite is ubiquitous. Olivine (Fa~24) and orthopyroxene (Fs~21) compositions are characteristic of the L-chondrite geochemical group. Mineralogically the meteorite is dominated by silicates [>90 vol%] (primarily olivine and pyroxene) accompanied by minor troilite (~6 vol%), and Fe-Ni (~2 vol%) metal. Accessory chromite and other minor silicates and oxides are also reported. Shock indicators include prominent veining, fractured crystals, irregular aggregates of polyhedral chondrules, maskelynite, and plessite. Not surprisingly, significant weathering is often apparent.
K-Ar and Pb,Th:He gas retention ages of 1.023 Ga & 0.61 Ga, respectively, as well as a cosmic-ray exposure (CRE) age of ~24 Ma have been reported. Helium and Argon release ages often reflecting major collisional events, while the CRE age often reflects the meteoroid's final period before earth-encounter.
The L-group of ordinary chondrites (relatively low in total iron) is the largest group of classified witnessed meteorite falls and account for ~45% of the well-classified meteorite falls. The small L5 petrologic type subgroup accounts for ~ 20% of the group. 82 meteorite falls had been classified exactly as L5 chondrites by early June 2017.
The Ergheo mass was well distributed with masses of ~ 1 kg still held by the United States National Museum (Washington) and the British Natural History Museum (NHM) in London. Consequently, it has been been a minor part of a number of studies. Much of the mineralogical and petrographic work was consolidated in the article by Baldanza & Levi-Donati (1971).
Nota bene: The coordinates provided by both the Catalogue of Meteorites (5/e) and the Meteoritical Bulletin Database (June 2017) would place the fall site in the ocean east of Somalia.
Coordinates are approximate only.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
6 valid minerals.
Meteorite/Rock Types Recorded
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Chromite Formula: Fe2+Cr3+2O4 |
| ⓘ 'Fayalite-Forsterite Series' Description: Olivine composition — (Fa25), Mason 1963, (Fa23.7), Keil & Fredriksson 1964 — typical L-group ordinary chondrites References: Mason, Brian (1963) Olivine composition in chondrites. Geochimica et Cosmochimica Acta, 27 (10) 1011-1023 doi:10.1016/0016-7037(63)90062-0 |
| ⓘ 'Feldspar Group' |
| ⓘ 'Glass' Description: Dark brown glass in veins as well as transparent interstitial maskelynite. |
| ⓘ Ilmenite Formula: Fe2+TiO3 Description: Peculiar tri-planar twinning in magnetite. |
| ⓘ 'Limonite' |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 |
| ⓘ 'Maskelynite' References: |
| ⓘ Native Iron Formula: Fe |
| ⓘ Native Iron var. Kamacite Formula: (Fe,Ni) |
| ⓘ 'Orthopyroxene Subgroup' Description: Orthopyroxene composition (Fs2o.5), typical of L-group ordinary chondrites. References: |
| ⓘ 'Plessite' |
| ⓘ Taenite Formula: (Ni,Fe) |
| ⓘ Troilite Formula: FeS Description: Often in recrystallized polycrystalline masses. |
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) |
| ⓘ | Taenite | 1.AE.10 | (Ni,Fe) |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Troilite | 2.CC.10 | FeS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Chromite | 4.BB.05 | Fe2+Cr3+2O4 |
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| Unclassified | |||
| ⓘ | 'Feldspar Group' | - | |
| ⓘ | 'Limonite' | - | |
| ⓘ | 'Maskelynite' | - | |
| ⓘ | 'Fayalite-Forsterite Series' | - | |
| ⓘ | 'Plessite' | - | |
| ⓘ | 'Orthopyroxene Subgroup' | - | |
| ⓘ | 'Glass' | - | |
List of minerals for each chemical element
| O | Oxygen | |
|---|---|---|
| O | ⓘ Chromite | Fe2+Cr23+O4 |
| O | ⓘ Ilmenite | Fe2+TiO3 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Fayalite-Forsterite Series | |
| Mg | Magnesium | |
| Mg | ⓘ Fayalite-Forsterite Series | |
| Si | Silicon | |
| Si | ⓘ Fayalite-Forsterite Series | |
| S | Sulfur | |
| S | ⓘ Troilite | FeS |
| Ti | Titanium | |
| Ti | ⓘ Ilmenite | Fe2+TiO3 |
| Cr | Chromium | |
| Cr | ⓘ Chromite | Fe2+Cr23+O4 |
| Fe | Iron | |
| Fe | ⓘ Chromite | Fe2+Cr23+O4 |
| Fe | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | ⓘ Native Iron | Fe |
| Fe | ⓘ Native Iron var. Kamacite | (Fe,Ni) |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Taenite | (Ni,Fe) |
| Fe | ⓘ Troilite | FeS |
| Fe | ⓘ Fayalite-Forsterite Series | |
| Ni | Nickel | |
| Ni | ⓘ Native Iron var. Kamacite | (Fe,Ni) |
| Ni | ⓘ Taenite | (Ni,Fe) |
Other Regions, Features and Areas containing this locality
This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to
visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders
for access and that you are aware of all safety precautions necessary.
References
Mason, Brian (1963) Olivine composition in chondrites. Geochimica et Cosmochimica Acta, 27 (10) 1011-1023 doi:10.1016/0016-7037(63)90062-0
Keil, Klaus, Fredriksson, Kurt (1964) The iron, magnesium, and calcium distribution in coexisting olivines and rhombic pyroxenes of chondrites. Journal of Geophysical Research, 69 (16) 3487-3515 doi:10.1029/jz069i016p03487
Bunch, T.E., Keil, Klaus, Snetsinger, K.G. (1967) Chromite composition in relation to chemistry and texture of ordinary chondrites. Geochimica et Cosmochimica Acta, 31 (10). 1569-1582 doi:10.1016/0016-7037(67)90105-6
[1]Baldanza, B., Levi-Donati, G. R. (1971) Evidence of shock-metamorphic effects in the Ergheo meteorite. Mineralogical Magazine, 38 (294) 197-204 doi:10.1180/minmag.1971.038.294.09
Wasson, John T., Wang, Sichao (1991) The histories of ordinary chondrite parent bodies: U,Th-He age distributions. Meteoritics, 26 (2) 161-167 doi:10.1111/j.1945-5100.1991.tb01033.x

Ergheo meteorite, Lower Shabelle Region, Somalia