The Canyon Diablometeorite refers to the many fragments of the asteroid that created Meteor Crater (also called Barringer Crater),[3]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.
History
The impactor fell about 50,000 years ago.[4] Initially known and used by pre-historic Native Americans, Canyon Diablo meteorites have been collected and studied by the scientific community since the 19th century. 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, and Harvey Harlow Nininger.[5][6][7][8][9][10][11]
Moissanite – a variety of silicon carbide, the second hardest natural mineral.
Samples may contain troilite-graphite nodules with metal veins and small diamonds.
Fragments
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:
^"Barringer Crater". Oxford Reference. Oxford. Archived from the original on November 17, 2021. Retrieved November 16, 2021.
^Roddy, D. J.; E. M. Shoemaker (1995). "Meteor Crater (Barringer Meteorite Crater), Arizona: summary of impact conditions". Meteoritics. 30 (5): 567. Bibcode:1995Metic..30Q.567R.
^Barringer, D.M. (1906). "Coon Mountain and its Crater." Proceedings of the Academy of Natural Sciences of Philadelphia, 57:861–886. PDFArchived 2016-03-04 at the Wayback Machine
^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.