Barringer crater?
The Barringer Meteorite Crater (also known as “Meteor Crater”) is a gigantic hole in the middle of the arid sandstone of the Arizona desert. A rim of smashed and jumbled boulders, some of them the size of small houses, rises 150 feet above the level of the surrounding plain. The crater itself is nearly a mile wide, and 570 feet deep. In 1902 Daniel Moreau Barringer, a successful mining engineer, heard about the crater. When he learned that small balls of meteoritic iron were randomly mixed with the ejected rocks of the crater rim, Barringer immediately concluded that the crater had resulted from a meteorite impact. If the meteorites had fallen at a different time from the time at which the crater was formed, they would have appeared in separate layers from the ejected rock. When Europeans first discovered the crater, the plain around it was covered with chunks of meteoritic iron – over 30 tons of it, scattered over an area 8 to 10 miles in diameter. Scientists now believe that the crat