Canyon Diablo (meteorite)
|Structural classification||Coarse Octahedrite|
|Composition||7.1% Ni; 0.46% Co; 0.26% P; 1% C; 1% S; 80ppm Ga; 320ppm Ge; 1,9ppm Ir|
|Region||Coconino County, Arizona|
|Fall date||49000 years ago|
Etched slice showing a Widmanstätten pattern
|Related media on Wikimedia Commons|
The Canyon Diablo meteorites include the many fragments of the asteroid that created Meteor Crater, Arizona, United States. Meteorites have been found around the crater rim, and are named for nearby Canyon Diablo, which lies about three to four miles west of the crater.
The asteroid fell about 50,000 years ago. The meteorites have been known and collected since the mid-19th century and were known and used by pre-historic Native Americans. Meteor Crater, from the late 19th to the early 20th century, was the center of a long dispute over the origin of craters that showed little evidence of volcanism. That debate was largely settled by the early 1930s, thanks to work by Daniel M. Barringer, F.R. Moulton, Harvey Harlow Nininger, and Eugene Shoemaker.
In 1953, Clair Cameron Patterson measured ratios of the lead isotopes in samples of the meteorite. The result permitted a refinement of the estimate of the age of the Earth to 4.550 billion years (± 70 million years).[clarification needed]
Composition and classification
This meteorite is an iron octahedrite (coarse octahedrite). Minerals reported from the meteorite include:
- Cohenite - iron carbide
- Chromite - iron magnesium chromium oxide
- Daubréelite - iron(II) chromium sulfide
- Diamond and lonsdaleite - carbon
- Graphite - carbon
- Haxonite - iron nickel carbide
- Kamacite iron nickel alloy - the most common component.
- Base metal sulfides
- Schreibersite - iron nickel phosphide
- Taenite - iron nickel alloy
- Troilite - a variety of the iron sulfide mineral pyrrhotite. The troilite in this sample is used as the standard reference for sulfur isotope ratios.
- Moissanite - a variety of silicon carbide, the second hardest natural mineral.
Samples may contain troilite-graphite nodules with metal veins and small diamonds.
The biggest fragment ever found is the Holsinger Meteorite, weighing 639 kilograms (1,409 lb), now on display in the Meteor Crater Visitor Center on the rim of the crater. Other famous fragments:
- 485 kilograms (1,069 lb), Canterbury Museum, Christchurch, New Zealand. The largest fragment outside the United States.
- 360 kilograms (790 lb), Muséum national d'Histoire naturelle (MNHN), Paris
- 242.6 kilograms (535 lb), Lowell Observatory in Flagstaff, Arizona
- 226,8 kilograms (500 lb), MINES ParisTech Mineralogy Museum (Paris School of Mines, France)
- 225.9 kilograms (498 lb), Academy of Natural Sciences of Drexel University, Philadelphia, Pennsylvania.
- 194 kilograms (427 lb), Beloit College, Beloit, Wisconsin.
- 162 kilograms (357 lb), "Clark Iron," Meteorite Gallery, University of California, Los Angeles
- 145 kilograms (320 lb), Geology Museum, University of Wisconsin - Madison, Wisconsin.
- 136 kilograms (300 lb), Franklin Institute, Philadelphia.
- 122 kilograms (269 lb), Griffith Observatory, Los Angeles, California. Fragment loaned by the Geology Department of Pomona College.
- 179 kilograms (395 lb), Griffith Observatory, Los Angeles, California.
- 100 kilograms (220 lb), California Academy of Sciences, San Francisco.
- 54 kilograms (119 lb), Newark Museum, Newark, New Jersey.
- 28 kilograms (57 lbs), Peoria Riverfront Museum, Dome Planetarium, Peoria, Illinois
- Basket Meteorite (22 kilograms (49 lb)), Meteor Crater Museum, Arizona.
- 19 kilograms (42 lb), Wagner Free Institute of Science, Philadelphia.
- Meteoritical Bulletin Database: Canyon Diablo
- Spaceguard Foundation UK Archived 2006-11-17 at the Wayback Machine
- Roddy, D. J.; E. M. Shoemaker (1995). "Meteor Crater (Barringer Meteorite Crater), Arizona: summary of impact conditions". Meteoritics. 30 (5): 567.
- Barringer, D.M. (1906). "Coon Mountain and its Crater." Proceedings of the Academy of Natural Science of Philadelphia, 57:861–86. PDF
- Moulton, F. R. (August 24, 1929). Report on the Meteor Crater - I. Philadelphia: Barringer Crater Company.
- Moulton, F. R. (November 20, 1929). Report on the Meteor Crater - II. Philadelphia: Barringer Crater Company.
- Crowson, Henry L. (1971). "A method for determining the residual meteoritical mass in the Barringer Meteor Crater". Pure and Applied Geophysics. 85 (1): 38–68. Bibcode:1971PApGe..85...38C. doi:10.1007/bf00875398. S2CID 140725009.
- Artemieva N.; Pierazzo E (2010). "The Canyon Diablo impact event: Projectile motion through the atmosphere". Meteoritics & Planetary Science. 44 (1): 25-42. doi:10.1111/j.1945-5100.2009.tb00715.x.
- Nininger, Harvey Harlow (1956). Arizona's Meteorite Crater. Sedona, Arizona: American Meteorite Laboratory. ISBN 978-0910096027.
- Levy, David (2002). Shoemaker by Levy: The man who made an impact. Princeton: Princeton University Press. pp. 69, 73–75, 81–83. ISBN 9780691113258.
- Patterson, C. (1956). "Age of Meteorites and the Earth". Geochimica et Cosmochimica Acta. 10: 230–237. Bibcode:1956GeCoA..10..230P. doi:10.1016/0016-7037(56)90036-9.
- Canyon Diablo Meteorite; MET16, Canterbury Museum collection on eHive
- Meteorite moves to Flag
- UCLA's new Meteorite Museum rocks Archived June 8, 2013, at the Wayback Machine
- Canyon Diablo meteorite at The Franklin Institute
- Rummager's galactic find turns out to be stolen meteorite
- Long-lost meteorite comes home to Arizona
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