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Heredia meteorite, San Pablo Canton, Heredia Province, Costa Ricai
Regional Level Types
Heredia meteoriteMeteorite Fall Location
San Pablo CantonCanton
Heredia ProvinceProvince
Costa RicaCountry

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Latitude & Longitude (WGS84):
10° 0' 0'' North , 84° 5' 59'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
San Pablo21,662 (2016)0.6km
San Rafael8,887 (2018)1.5km
Heredia21,947 (2016)1.8km
San Josecito12,195 (2018)1.9km
San Francisco55,923 (2018)3.3km
Mindat Locality ID:
293056
Long-form identifier:
mindat:1:2:293056:8
GUID (UUID V4):
f686f00a-55f7-4bb9-92a3-6bf05aab53a7


Ordinary chondrite, brecciated (H5,br)
Fall, 1 April 1857; 1 kg

An unusually bright nighttime bolide, flashing at times, and accompanied by detonations and clouds of smoke was seen. Many stones were found, but apparently, only the largest stone was preserved (~1 kg). The interior of the meteorite is mostly a motley of variously colored gray and brownish regions interrupted by moderately large silicate-rich clasts, occasional relic chondrules, and tiny flecks of Fe-Ni metal. Brecciation is evident and the meteorite is also gas-rich. Olivine (Fa18)and Ca-rich pyroxene ('bronzite') are characteristic of the H-chondrite geochemical group. Mineralogically, the meteorite consists primarily of olivine and pyroxene accompanied by smaller amounts of plagioclase, troilite, and Fe-Ni metal. While accessory chromite, copper, schreibersite, and minor sulfides are also reported the meteorite does not seem to have received extensive petrographic attention (at least in English). Veining and extensive brecciation were accompanied, presumably, by at least moderate levels of shock. Chronological studies have, however, been made and a cosmic ray exposure age (CRE) of 11.1 Ma is reported.

The H-group chondrites represent over 35% of all well-classified, witnessed falls. Heredia itself was the 25th witnessed fall classified exactly as an 'H5' — a subgroup that now contains 174 members (as of early 2017). Heredia is also the only confirmed meteorite fall from Costa Rica. Approximately half of the large stone was obtained by the University of Göttingen with 410 g remaining in 2004.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


8 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 Diagram

Detailed Mineral List:

Chromite
Formula: Fe2+Cr3+2O4
Reference: Farrington, O.C. (1915). Catalogue of the meteorites of North America: Memoirs of the National Academy of Sciences, Vol. 13: Washington. 545 pages.; 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: Composition (Fa18).
Reference: Farrington, O.C. (1915). Catalogue of the meteorites of North America: Memoirs of the National Academy of Sciences, Vol. 13: Washington. 545 pages.; Mason, B. (1963) Olivine in ordinary chondrites. Geochimica et Cosmochimica Acta 27(9): 1011-1023. (Sept 1963).; Soto, G.S. (2004) Meteoritos y Meteoros en Costa Rica (Verdaderos, Posibles y Falsos) [In Spanish]: Revista Geológica de América Central 31: 7-23.
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.
'Orthopyroxene Subgroup'
Reference: Soto, G.S. (2004) Meteoritos y Meteoros en Costa Rica (Verdaderos, Posibles y Falsos) [In Spanish]: Revista Geológica de América Central 31: 7-23.
'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
Reference: Farrington, O.C. (1915). Catalogue of the meteorites of North America: Memoirs of the National Academy of Sciences, Vol. 13: Washington. 545 pages.
'Pyroxene Group'
Formula: ADSi2O6
Reference: Farrington, O.C. (1915). Catalogue of the meteorites of North America: Memoirs of the National Academy of Sciences, Vol. 13: Washington. 545 pages.
Schreibersite
Formula: (Fe,Ni)3P
Reference: Farrington, O.C. (1915). Catalogue of the meteorites of North America: Memoirs of the National Academy of Sciences, Vol. 13: Washington. 545 pages.
Taenite
Formula: (Fe,Ni)
Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
Troilite
Formula: FeS
Reference: Farrington, O.C. (1915). Catalogue of the meteorites of North America: Memoirs of the National Academy of Sciences, Vol. 13: Washington. 545 pages.; Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Copper1.AA.05Cu
Iron1.AE.05Fe
var. Kamacite1.AE.05(Fe,Ni)
Schreibersite1.BD.05(Fe,Ni)3P
Taenite1.AE.10(Fe,Ni)
Group 2 - Sulphides and Sulfosalts
Isocubanite2.CB.55bCuFe2S3
Mackinawite2.CC.25(Fe,Ni)9S8
Troilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
Chromite4.BB.05Fe2+Cr3+2O4
Unclassified Minerals, Rocks, etc.
'Fayalite-Forsterite Series'-
'Orthopyroxene Subgroup'-
'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
'Pyroxene Group'-ADSi2O6

List of minerals for each chemical element

OOxygen
O ChromiteFe2+Cr23+O4
O Pyroxene GroupADSi2O6
O Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
NaSodium
Na Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
AlAluminium
Al Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Si Pyroxene GroupADSi2O6
Si Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
PPhosphorus
P Schreibersite(Fe,Ni)3P
SSulfur
S TroiliteFeS
S IsocubaniteCuFe2S3
S Mackinawite(Fe,Ni)9S8
CaCalcium
Ca Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
CrChromium
Cr ChromiteFe2+Cr23+O4
FeIron
Fe ChromiteFe2+Cr23+O4
Fe Schreibersite(Fe,Ni)3P
Fe TroiliteFeS
Fe IsocubaniteCuFe2S3
Fe Iron var. Kamacite(Fe,Ni)
Fe Mackinawite(Fe,Ni)9S8
Fe IronFe
Fe Taenite(Fe,Ni)
NiNickel
Ni Schreibersite(Fe,Ni)3P
Ni Iron var. Kamacite(Fe,Ni)
Ni Mackinawite(Fe,Ni)9S8
Ni Taenite(Fe,Ni)
CuCopper
Cu CopperCu
Cu IsocubaniteCuFe2S3

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Farrington, O.C. (1915) Catalogue of the meteorites of North America: Memoirs of the National Academy of Sciences, Vol. 13: Washington. 545 pp.
Keil, Klaus (1962) On the phase composition of meteorites. Journal of Geophysical Research, 67(10), 4055-4062. (Sept 1962).
Mason, B. (1963) Olivine in ordinary chondrites. Geochimica et Cosmochimica Acta, 27(9), 1011-1023. (Sept 1963).
Zähringer, J. (1968) Rare gases in stony meteorites. Geochimica et Cosmochimica Acta, 32(2), 209-237.
Ramdohr, P. (1973) The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pp.
Graf, Th. and Marti K. (1995) Collisional history of H chondrites. J. Geophys. Res. (Planets) 100, 21247–21263.
Grady, M.M (2000). Catalogue of Meteorites (5/e). Cambridge University Press: Cambridge; New York; Oakleigh; Madrid; Cape Town. 689 pp.
Soto, G.S. (2004) Meteoritos y Meteoros en Costa Rica (Verdaderos, Posibles y Falsos). Revista Geológica de América Central, 31, 7-23 (in Spanish).

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