top of page

IAB

page top
Campo del Cielo

Name

*click on the Name for more information

Structure Class

Iron

Chemical Class

IAB-MG

Country

Argentina

Year found

1576

Mass

50 t

[Museum Collection]

(1) 165kg   (2) 23kg   (3) 5.7kg   (4) 5.7kg

(5) 2.28kg   (6) 1781.3g

EL ABIPÓN, Environs of Gancedo, situated to the extreme S. W. of the Chaco government; (φ = 27°30'S, λ = 61°42'W). Found, 1936.Iron, (undescribed).1 specimen, the dimensions are approximately 73 X 50 X 40 cms., weight 460 kg. The meteorite was found by a day laborer, in the place «Campo del Cielo». The meteorite was received by the Museum of Natural History (Buenos Aires, Argentina) in 1942. EL MATACO, near to Gancedo, Mariano Moreno department, Santiago del Es­tero province; (φ = 21°30'S, λ = 61°42'W) Found, 1937.Iron, (undescribed).1 specimen, weight 998 kg.The meteorite was found by a rural 50 meters from the place where the grand iron meteorite El Toba was found in the year 1923. It is in the Museum of Rosario City, (Santa Fe province, Argentina, where is exhibited in one of its square, in the open air. EL TONOCOTE, environs of Gancedo, Chaco government; (φ = 27°30'S, λ = 61'42'W). Found, 1931.Iron, (undescribed).1 specimen, weight 850 kg.The meteorite was brought in the year of 1931, as a donation for the Dirección de Geologia y Mineria (Buenos Aires, Argentina). NIHUA, environs of Gancedo, Chaco government; (φ = 27°30'S, λ = 61°42'W). Found, 1948.Iron, (undescribed).1 specimen, weight 15 kg.The meteorite was brought in the year of 1948, as a donation for the Dirección de Geologia y Mineria (Buenos Aires, Argentina). PINALTÁ, environs of Gancedo, Mariano Moreno department, Santiago del Estero province; (φ = 27°30'S, λ = 61°42'W) Found, 1937.Iron, (undescribed).1 specimen, weight 8.92 kg.The meteorite was found near the grand mass El Motaco and was brought in the year of 1937, as a donation for the Museo de Ciencias Naturales (Buenos Aires, Argentina). Source: List and date on new Argentine meteorites not included in the Prior­Hey catalogue, 1953, compiled by Dr. L. O. Giacomelli and sent to E. L. Krinov in letter of July 4, 1962. DISCOVERY OF EL PATIO IRON METEORITE, ARGENTINA Name: EL PATIO.The place of fall or discovery: Santiago del Estero Province (boundary with the Chaco Province), Argentina; φ =- 27°40' S, λ = 61°44' W.Date of fall or discovery: FOUND, before 1960.Class and type: IRON, hexahedrite.Number of individual spe­cimens: 1. Total weight: 350 kg.Circumstances of fall or discovery: The meteorite was preserved in the place of found. Source: Report of Dr. L. O. Giacomelli (Buenos Aires, Argen­tina) in a letter 11.11 1965 and an article: W. A. Cassidy, et all. ((Meteorites and Craters of Campo del Cielo, Argentina), p. 29, September, 1964; Lamont Geological Observatory, U. S. A. DISCOVERY OF EL TACO IRON METEORITE, ARGENTINA Name: EL TACO.The place of fall or discovery: Santiago del Estero Province (boundary with the Chaco Province), Argentina; φ = 27°41' S, λ = 61°47' W.Date of fall or discovery: FOUND, 1962. Class and type: IRON, hexahedrite.Number of individual spe­cimens: 1.Total weight: 3090 gr. Circumstances of fall or discovery: The meteorite was found by a farmer plowing a cotton field. The meteorite is in the U. S. National Museum (Washington, USA). Source: Report of Dr. L. O. Giacomelli (Buenos Aires, Argenti­na) in a letter, 11.11 1965 and an above article. Correction:: A letter from Dr. Roy F. Schall (Pittsburgh, USA), April 1, 1966 reports that «The weight of «El Taco» is in units of kilograms, not grams (Met. Bull. No. 33, March, 1965; Science 149, 1055 (1965)). Also, Dr. H. Hinterberger of the Max-Planck-Institut, Mainz, Germany, has weighed «El Taco» and found its mass to be 1998 kg.

Canyon Diablo

Name

*click on the Name for more information

Structure Class

Iron

Chemical Class

IAB-MG

Country

United States of America

Year found

1891

Mass

30 t

[Museum Collection]

(1) 1.1kg   (2) 726.8g   (3) 676.2g   (4) 157.6g

(5) 105.5g   (6) 13.5g   (7) 10.6g   (8) 10.1g

(9) 8.0g  (10) 4.002g (11) 3.990g  (12) 2.898g

(13) 2.696g  (14)2.098g  (15) 68.4g

DISCOVERY OF BLOODY BASIN IRON METEORITE, USA Name: BLOODY BASIN.The place of fall or discovery: Bloody Basin, Yavapai County, Arizona, USA: φ = 34°10' N, λ = 111°43' W. Date of fall or discovery: FOUND, September, 1964.Class and type: IRON, coarse octahedrite. Number of individual spe­cimens: 1.Total weight: 5074 gr. Circumstances of fall or discovery: The meteorite was found by A. Morriston while hun­ting. The meteorite is preserved in the collections of Arizona State University (Tempe, USA). Source: Report of Dr. Ch. F. Lewis (Tempe, USA) in a letter, 11.9 1965. DISCOVERY OF FAIR OAKS IRON METEORITE, USA Name: FAIR OAKS.The place of fall or discovery:  Near Fair Oaks, Yavapai County, Arizona, USA; φ = 34°44' N, λ = 112°44' W. Date of fall or discovery: FOUND, October, 1937; brought to scientific notice in 1964. Class and type: IRON, coarse octahedrite.Number of individual spe­cimens: 1.Total weight: 787 gr Circumstances of fall or discovery: The meteorite was found by J. Coates while hunting. The meteorite is preserved in the collections of Arizona State University (Tempe, USA). Source: Report of Dr. Ch. F. Lewis (Tempe, USA) in a letter, 11.9 1965. OILDALE, Kern County, California, USA; φ = 35°25' N, λ = 119°0' W. Recognized 1957.IRON, octahedrite.50.1 gr, in Inst. Meteor., Univ. New Mexico, USA. DISCOVERY OF THE PANAMINT RANGE, CALIFORNIA, IRON METEORITE Name: PANAMINT RANGE Place of find: West slope of Panamint Range, Inyo County, California, USA. Approximately 36°30'N, 117°30'W. Date of find: Between 1950 and 1964. Class and type: Iron. Coarse octahedrite. Ni = 7.17%, Co = 0.3% (E. Olsen, analyst: X-ray fluorescence method). Number of individual specimens: 1 Total weight: 204 grams at present. Original finder cut off a small slice. Original weight estimated at 230 grams. Circumstances of find: Found by unnamed prospector, who, in 1960, left it with Mr. James Minette, mine geologist for U.S. Borax Co., Boron, California. Mr. Minette sent it to the Field Museum, Chicago, Illinois, in late 1973. Comments: Polished section studied by Dr. V.F. Buchwald of Copenhagen; it is a highly shock-altered iron of the crater-forming kind. Its location, about 680 km west of the Canyon Diablo find, and the absence of a known and verified meteorite crater in the area, strongly suggest it is a piece of transported Canyon Diablo meteorite. Superficially the piece looks very much like Canyon Diablo individuals, with small pockets of adhering clay in surface flutings. Its bandwidth, however, is at the lower limit of values reported for Canyon Diablo, 1.5-2.5 mm. The specimen is located at the Field Museum of Natural History, Chicago. Source: Dr. E. Olsen, Field Museum of Natural History, Chicago, Illinois, USA.

Hickman

Name

*click on the Name for more information

Structure Class

Iron

Chemical Class

IAB complex

Country

Australia

Year found

2018

Mass

3.55 kg

[Museum Collection]

(1) 21.9g

History: Found by a gold prospector in June 2018, 2.5 km SE of Hickman crater. The specimen was sold to a local mineral dealer who brought it to the 2020 Tucson Gem and Mineral show, where it was purchased by Keith and Dana Jenkerson and subsequently sold to Don Hurkot. Other meteorites have reportedly been found in the area. Physical characteristics: The irregularly shaped mass has a red-brown surface and numerous regmaglypts. Petrography: (C. Herd and P. Hill, UAb) Petrographic investigation of a 1 × 3 cm polished and etched surface reveals a well-developed Widmanstaetten pattern with kamacite bandwidth 1.1±0.3 mm (n=6), consistent with a medium octahedrite. No inclusions were observed. Terrestrial alteration extends along grain boundaries into the interior. Geochemistry: ICP-MS data, using sample of North Chile (Filomena) as standard (C. Herd, P. Hill, and S. DuFrane UAb): Ni = 7.7, Co = 0.48 (both wt%); Ir = 2.5, Ga = 64, Ge = 266, As = 16.7, Sb = 0.427, Ru = 4.8, Re = 0.23, Os = 2.2, W = 0.6, Pt = 5.5, Cu = 162 (all μg/g). Classification: (C. Herd, UAb): IAB iron, medium octahedrite. Most likely belongs to the Main Group, by comparison with Wasson and Kallemeyn (2002). Specimens: Type specimen consisting of a 27.0 g representative specimen at UAb. Main mass with Don Hurkot.

Maslyanino

Name

*click on the Name for more information

Structure Class

Iron

Chemical Class

IAB complex

Country

Russia

Year found

1992

Mass

26 kg

[Museum Collection]

(1) 9.30g   (2) 11.0g

A mass of 26 kg was found by agronomist V. G. Okel' in a wheat field near Maslyanino village. Classification, information, type sample (1.4 kg): Marina A. Ivanova, Committee on Meteorites, Russian Academy of Sciences, Ul. M. Ulyanovoi 3, korp. 1, Moscow 117313, Russia. Analysis: 12.43% Ni; 70 ppm Ge; 1.0 ppm Ir; 29 ppm Ga; L. D. Barsukova and G. M. Kolesov, Vernadsky Institute of Geochemistry and Analytical Chemistry, RAS, Moscow. The main mass is at the Geological Museum of the Geological and Geophysical Institute of the Siberian Branch RAS, Universitesky Avenue 3, Novosibirsk 630090, Russia.

Mundrabilla

Name

*click on the Name for more information

Structure Class

Iron

Chemical Class

IAB-ung

Country

Australia

Year found

1911

Mass

24 t

[Museum Collection]

(1) 102.5g   (2) 35g   (3) 21.1g   (4) 22.2g

DISCOVERY OF MUNDRABILLA IRON METEORITE, WESTERN AUSTRALIA Name: MUNDRABILLA. The place of fall or discovery: The Nullarbor Plain, to the north of the Transcontinental Railway,Western Australia; φ = 30°47'S, λ =127°33'E. Date of fall or discovery: FOUND, March 1966. Class and type: IRON, medium octahedrite. Number of individual specimens: 2 Total weight: 10-12 tons and 5 1/2 tons. Circumstances of the fall or discovery: The meteorites were found by geologists R. B. Wilson and A. M. Cooney while engaged on a geological survey. Both masses are lying within only very slight depressions in clayey soil, some 180 m apart. The larger mass tends to have a crude conical to hemispherical shape with the nose partially buried in the soil. The axis is inclined at an angle of approximately 60°. Evidence of fragmentation of a larger mass is afforded by a sharp, angular, vertical face on the larger mass, which matches both in size and shape, a similar sharp face on the smaller mass. Preliminary study indicates that the meteorite came from the west at relatively low velocity and high angle. The larger mass has been presented to the Western Australian Museum, while the smaller mass is in Geosurveys possesion (Adelaide, South Australia). Source: Report of Dr. R. B. Wilson (Adelaide, South Australia) in a letter 1.4. 1967.

Shawnee

Name

*click on the Name for more information

Structure Class

Iron

Chemical Class

IAB-MG

Country

United States of America

Year found

2010

Mass

 8.18 kg

[Museum Collection]

(1) 36.3g

History: A single 8181 g mass was acquired at an estate sale in Shawnee, Kansas. The meteorite had been used for many years as a doorstop by a couple that lived in Shawnee. The owners of the meteorite originally owned farm ground in Barton County, Kansas, but lived for the better part of their lives in Shawnee. Unfortunately, the exact find location is unknown. A small end piece was sent to ASU and confirmed to be a meteorite. Physical characteristics: Surface shows some fusion crust and minor weathering with broad regmaglypts. Petrography: (L. Garvie, ASU) Etched sections show a coarse Widmanstätten structure, with stubby kamacite, bandwidth 1.3 mm. Kamacite lamellae display subboundaries and numerous μm-sized phosphide precipitates. Sub-millimeter schreibersite common within some kamacite grains and at grain boundaries. Neumann bands straight and well developed in rhabdite-free grains. Thin taenite and plessite cover several percent by area. Inclusions common - one 7 × 5 cm slice exhibits several (to 2 cm) irregular silicate-graphite-troilite-schreibersite regions. Silicates consist of olivine, low-Ca pyroxene, clinopyroxene, and plagioclase. Slice contains several 1-mm blocky schreibersite with cohenite rims. Geochemistry: Bulk composition: INAA data (Activation Laboratories - Ancaster, Ontario): Co 0.46 mg/g, Ni 74 mg/g, Ga 57 μg/g, Ge 180 μg/g, Ir 2.24 μg/g, and Au 1.50 μg/g. Classification: Iron meteorite, IAB-MG, coarse octahedrite, moderately shocked. Specimens: Type specimens - two slices with total weight of 144.6 g.

Udei Station

Name

*click on the Name for more information

Structure Class

Iron

Chemical Class

IAB-ung

Country

Nigeria

Year found

1927

Mass

103 kg

[Museum Collection]

(1) 10.6g

NW5549

Name

*click on the Name for more information

Structure Class

Iron

Chemical Class

IAB-MG

Country

(Northwest Africa)

Year found

2008

Mass

12 kg

[Museum Collection]

(1) 36.93g   (2) 246.0g   (3) 46.90g   

(4) 42.77g

Petrography: UCLA samples from two masses; in these and in web photos, silicates are common. We examined two sides of a slice with total area 25 cm2. Silicate abundance ~15 vol%, troilite ~1.5 vol%. Kamacite lengths only ~1.5x widths, making width determination uncertain; best estimate 1.6±0.3 mm. Neumann lines abundant. Some silicates contain abundant small metal grains. A few large (3x4 mm) kamacite lamellae with incompletely resorbed taenite. Geochemistry: Co (mg/g) 4.55, Ni (mg/g) 68.8, Ga (µg/g) 81.6, Ge (µg/g) 370, As (µg/g) 4.1, Ir (µg/g) 4.1, Au (µg/g) 1.49. Submitter: J. T. Wasson, UCLA.

bottom of page