- Meteorite Type: Iron IAB-MG, Found in United States, 1891
- Meteorite Weight: 5-10 grams
- Meteorite Measurements: Varies
- Additional Information: A genuine iron meteorite from Meteor Crater for only $25! We choose from the current available lot. Your specimen will be from 5-10 grams in size.
Canyon Diablo 5-10g
25 in stock
25 in stock
Iron IAB-MG, Found in United States, 1891
Meteor Crater is the most recognizable and best-known meteorite feature on Earth and is visited by many thousands of tourists annually. Estimates of its age vary from 25,000 to 50,000 years, but all parties concur that it is the finest and best-preserved large meteorite crater on our planet.
It was also the first proven meteorite crater. Geologist, miner, entrepreneur, and visionary Daniel Barringer was convinced the feature was a meteorite crater, defying the popular opinion of so-called experts at the time. Barringer spent a fortune searching for what he believe to be a giant meteorite buried under the crater. He was right about the crater, but wrong about the meteorite. We now know that the mass fragmented and part of it vaporized upon impact. But Barringer’s insight and determination gave him an honored place in meteorite history and the site is still sometimes referred to as Barringer Crater.
Another key figure in space rock history, innovative meteoriticist H.H. Nininger, conducted many years of important research at the site and also opened the world’s first private meteorite museum alongside nearby Route 66. Meteor Crater was studied by legendary geologist Gene Shoemaker and some of the NASA Apollo astronauts were trained there prior to their moon missions.
Canyon Diablo is a steep-sided ravine some distance west of the crater and meteorites found around the crater take their name from it (the convention being that meteorites are named after the nearest town or geographical feature to their fall location and they could hardly be named after the crater that they, themselves, formed). Meteor Crater is internationally recognized as a scientific site of unique importance and meteorite collecting there is no longer permitted. Older specimens that were found during the first half of the 19th century, or earlier, when collecting was still allowed are, therefore, highly desirable.