Olivenza meteorite, Olivenza, Badajoz, Extremadura, Spaini
| Regional Level Types | |
|---|---|
| Olivenza meteorite | Meteorite Fall Location |
| Olivenza | Town |
| Badajoz | Province |
| Extremadura | Autonomous Community |
| Spain | Country |
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Latitude & Longitude (WGS84):
38° 43' North , 7° 4' West
Latitude & Longitude (decimal):
Locality type:
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Valverde de Leganés | 3,876 (2012) | 9.1km |
| Badajoz | 148,334 (2018) | 19.8km |
| Elvas | 9,904 (2018) | 20.1km |
| La Albuera | 1,796 (2012) | 21.1km |
| Táliga | 705 (2012) | 21.3km |
Name(s) in local language(s):
, Extremadura, España
Ordinary chondrite, fragmental breccia (LL5, S3, W0)
Fell, 19 June 1924; 150 kg
After the appearance of a moving white cloud, detonations were heard and 5 stones fell and broke into several pieces. Observations reveal poorly defined chondrules and chondrule fragments which merge with the fine-grained matrix. Relict chondrules are both olivine and pyroxene rich (BO, RP, POP) with Fe-Ni metal and troilite as blebs within the matrix and and interstitial patches between the relic chondrules. Olivine (Fa30) and orthopyroxene (Fa24.5) compositions and total iron (Fe 18.9 wt%) indicate an LL chondrite classification; textures provide the petrologic type; the presence of plessite and undulose extinction in olivine reflect moderate preterrestrial shock (level S3). A number of minor minerals have been observed with phosphates receiving special attention as hosts of radioactive isotopes. The reported presence of three different iron sulfides is more likely reflective of the observing skills of Paul Ramdohr than to any special features of Olivenza sulfides. Rb-Sr dating provides an ancient formational age (~4.6 Ga) for a putative original parent body. A cosmic ray exposure age of ~ 8.4 Ma — somewhat on the low end for LL chondrites — has been reported.
Olivenza is Spain's only LL5 meteorite and is its most massive recorded meteorite fall. 87 confirmed LL meteorite falls, including 19 LL5 meteorites, are currently listed as LL chondrites (very low in total Fe) with the Meteoritical Bulletin Database (January 2016). The LL chondrites are the smallest defined group of ordinary chondrites and represent ~10% of all meteorite falls.
The largest portion of the mass has been kept at the Spanish National Science Museum in Madrid (Museo Nacional de Ciencias Naturales) [50 kg in 2000]. Several other moderate-sized masses have been distributed elsewhere.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
12 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:
| ⓘ Chlorapatite Formula: Ca5(PO4)3Cl Reference: Mold, P., Bull, R.K. & Durrani, S.A. (1982) Plutonium-244 concentrations in chondritic phosphates and their significance in fission-tracks dating of meteorites. IN: Solid State Nuclear Track Detectors: Proceedings of the 11 International Conference Bristol (Fowler, P., ed.): pp. 851-854. |
| ⓘ Chromite Formula: Fe2+Cr3+2O4 Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
| ⓘ Copper Formula: Cu Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
| ⓘ 'Fayalite-Forsterite Series' Description: Olivine (Fa30) Reference: Mason, B. (1962) Classification of Chondritic Meteorites: American Museum Novitates, #2069. 20 pages. (May 1962).; Rull, F., Muñoz-Espadas, M.J., Lunar R. & Martínez-Frías, J. (2010) Raman spectroscopic study of four Spanish shocked ordinary chondrites: Cañellas, Olmedilla de Alarcón, Reliegos and Olivenza. Philosophical Transactions of the Royal Astronomical Society A 368 (1922): 3059-3065. (June 2010). ; Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages.ronomical Society A 368 (1922): 3059-3065. (June 2010). |
| ⓘ Ilmenite Formula: Fe2+TiO3 Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
| ⓘ Iron Formula: Fe Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
| ⓘ Iron var. Kamacite Formula: (Fe,Ni) Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
| ⓘ Isocubanite Formula: CuFe2S3 Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
| ⓘ Mackinawite Formula: (Fe,Ni)9S8 Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
| ⓘ Merrillite Formula: Ca9NaMg(PO4)7 Reference: Mold, P., Bull, R.K. & Durrani, S.A. (1982) Plutonium-244 concentrations in chondritic phosphates and their significance in fission-tracks dating of meteorites. IN: Solid State Nuclear Track Detectors: Proceedings of the 11 International Conference Bristol (Fowler, P., ed.): pp. 851-854. |
| ⓘ 'Orthopyroxene Subgroup' Reference: Mason, B. (1962) Classification of Chondritic Meteorites: American Museum Novitates, #2069. 20 pages. (May 1962).; Rull, F., Muñoz-Espadas, M.J., Lunar R. & Martínez-Frías, J. (2010) Raman spectroscopic study of four Spanish shocked ordinary chondrites: Cañellas, Olmedilla de Alarcón, Reliegos and Olivenza. Philosophical Transactions of the Royal Astronomical Society A 368 (1922): 3059-3065. (June 2010). ; Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages.ronomical Society A 368 (1922): 3059-3065. (June 2010). |
| ⓘ Pigeonite Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6 Reference: Rull, F., Muñoz-Espadas, M.J., Lunar R. & Martínez-Frías, J. (2010) Raman spectroscopic study of four Spanish shocked ordinary chondrites: Cañellas, Olmedilla de Alarcón, Reliegos and Olivenza. Philosophical Transactions of the Royal Astronomical Society A 368 (1922): 3059-3065. (June 2010). |
| ⓘ 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 Reference: Rull, F., Muñoz-Espadas, M.J., Lunar R. & Martínez-Frías, J. (2010) Raman spectroscopic study of four Spanish shocked ordinary chondrites: Cañellas, Olmedilla de Alarcón, Reliegos and Olivenza. Philosophical Transactions of the Royal Astronomical Society A 368 (1922): 3059-3065. (June 2010). |
| ⓘ 'Plessite' Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
| ⓘ Taenite Formula: (Fe,Ni) Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. ; Rull, F., Muñoz-Espadas, M.J., Lunar R. & Martínez-Frías, J. (2010) Raman spectroscopic study of four Spanish shocked ordinary chondrites: Cañellas, Olmedilla de Alarcón, Reliegos and Olivenza. Philosophical Transactions of the Royal Astronomical Society A 368 (1922): 3059-3065. (June 2010). |
| ⓘ Tetrataenite Formula: FeNi Reference: Clarke Jr, R.S. & Scott, E.R.D. (1980) Tetrataenite—ordered FeNi, a new mineral in meteorites. American Mineralogist 65(7-8): 624-639. (Jul-Aug 1980). |
| ⓘ Troilite Formula: FeS Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. ; Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages.ronomical Society A 368 (1922): 3059-3065. (June 2010). |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Copper | 1.AA.05 | Cu |
| ⓘ | Iron | 1.AE.05 | Fe |
| ⓘ | var. Kamacite | 1.AE.05 | (Fe,Ni) |
| ⓘ | Taenite | 1.AE.10 | (Fe,Ni) |
| ⓘ | Tetrataenite | 1.AE.10 | FeNi |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Isocubanite | 2.CB.55b | CuFe2S3 |
| ⓘ | Mackinawite | 2.CC.25 | (Fe,Ni)9S8 |
| ⓘ | Troilite | 2.CC.10 | FeS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Chromite | 4.BB.05 | Fe2+Cr3+2O4 |
| ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Chlorapatite | 8.BN.05 | Ca5(PO4)3Cl |
| ⓘ | Merrillite | 8.AC.45 | Ca9NaMg(PO4)7 |
| Group 9 - Silicates | |||
| ⓘ | Pigeonite | 9.DA.10 | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Unclassified Minerals, Rocks, etc. | |||
| ⓘ | 'Fayalite-Forsterite Series' | - | |
| ⓘ | 'Orthopyroxene Subgroup' | - | |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'Plessite' | - | |
List of minerals for each chemical element
| O | Oxygen | |
|---|---|---|
| O | ⓘ Chromite | Fe2+Cr23+O4 |
| O | ⓘ Ilmenite | Fe2+TiO3 |
| O | ⓘ Chlorapatite | Ca5(PO4)3Cl |
| O | ⓘ Merrillite | Ca9NaMg(PO4)7 |
| O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| O | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Na | Sodium | |
| Na | ⓘ Merrillite | Ca9NaMg(PO4)7 |
| Na | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mg | Magnesium | |
| Mg | ⓘ Merrillite | Ca9NaMg(PO4)7 |
| Mg | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Al | Aluminium | |
| Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | Silicon | |
| Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| P | Phosphorus | |
| P | ⓘ Chlorapatite | Ca5(PO4)3Cl |
| P | ⓘ Merrillite | Ca9NaMg(PO4)7 |
| S | Sulfur | |
| S | ⓘ Isocubanite | CuFe2S3 |
| S | ⓘ Mackinawite | (Fe,Ni)9S8 |
| S | ⓘ Troilite | FeS |
| Cl | Chlorine | |
| Cl | ⓘ Chlorapatite | Ca5(PO4)3Cl |
| Ca | Calcium | |
| Ca | ⓘ Chlorapatite | Ca5(PO4)3Cl |
| Ca | ⓘ Merrillite | Ca9NaMg(PO4)7 |
| Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Ca | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| 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 | ⓘ Isocubanite | CuFe2S3 |
| Fe | ⓘ Iron var. Kamacite | (Fe,Ni) |
| Fe | ⓘ Mackinawite | (Fe,Ni)9S8 |
| Fe | ⓘ Taenite | (Fe,Ni) |
| Fe | ⓘ Troilite | FeS |
| Fe | ⓘ Tetrataenite | FeNi |
| Fe | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Fe | ⓘ Iron | Fe |
| Ni | Nickel | |
| Ni | ⓘ Iron var. Kamacite | (Fe,Ni) |
| Ni | ⓘ Mackinawite | (Fe,Ni)9S8 |
| Ni | ⓘ Taenite | (Fe,Ni) |
| Ni | ⓘ Tetrataenite | FeNi |
| Cu | Copper | |
| Cu | ⓘ Copper | Cu |
| Cu | ⓘ Isocubanite | CuFe2S3 |
References
Sort by
Year (asc) Year (desc) Author (A-Z) Author (Z-A)Mason, B. (1962) Classification of Chondritic Meteorites: American Museum Novitates, #2069. 20 pages. (May 1962).
Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
Clarke Jr, R.S. & Scott, E.R.D. (1980) Tetrataenite—ordered FeNi, a new mineral in meteorites. American Mineralogist 65(7-8): 624-639. (Jul-Aug 1980).
Mold, P., Bull, R.K. & Durrani, S.A. (1982) Plutonium-244 concentrations in chondritic phosphates and their significance in fission-tracks dating of meteorites. IN: Solid State Nuclear Track Detectors: Proceedings of the 11 International Conference Bristol (Fowler, P., ed.): pp. 851-854.
Grady, M.M (2000). Catalogue of Meteorites (5/e). Cambridge University Press: Cambridge; New York; Oakleigh; Madrid; Cape Town. 689 pages.
Rull, F., Muñoz-Espadas, M.J., Lunar R. & Martínez-Frías, J. (2010) Raman spectroscopic study of four Spanish shocked ordinary chondrites: Cañellas, Olmedilla de Alarcón, Reliegos and Olivenza. Philosophical Transactions of the Royal Astronomical Society A 368 (1922): 3059-3065. (June 2010).
Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages.
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