Form Object


Planes of Fame Air Museum, Valle Arizona Guide US Marine Corps Air Station, Yuma

Winslow — Meteor Crater Visitor's Center
Arizona Aviation Museum Guide

Meteor Crater Visitor's Center
20 miles West of Winslow off of I-40
Meteor Crater Enterprises
P.O. Box 70
Flagstaff, AZ 86002-0070

Meteor Crater is a meteorite impact crater located approximately 43 miles (69 km) east of Flagstaff, near Winslow in the northern Arizona desert of the United States. Because the US Department of the Interior Division of Names commonly recognizes names of natural features derived from the nearest post office, the feature acquired the name of “Meteor Crater” from the nearby post office named Meteor. The site was formerly known as the Canyon Diablo Crater, and fragments of the meteorite are officially called the Canyon Diablo Meteorite. Scientists refer to the crater as Barringer Crater in honor of Daniel Barringer who was first to suggest that it was produced by meteorite impact. The crater is privately owned by the Barringer family through their Barringer Crater Company, which proclaims it to be “the first proven, best-preserved meteorite crater on earth.” [3]

Despite its importance as a geological site, the crater is not protected as a national monument, a status that would require federal ownership. It was designated a National Natural Landmark in November 1967. [3]

Meteor Crater lies at an elevation of about 1,740 m (5,709 ft) above sea level. It is about 1,200 m (4,000 ft) in diameter, some 170 m deep (570 ft), and is surrounded by a rim that rises 45 m (150 ft) above the surrounding plains. The center of the crater is filled with 210–240 m (700–800 ft) of rubble lying above crater bedrock. One of the interesting features of the crater is its squared-off outline, believed to be caused by pre-existing regional jointing (cracks) in the strata at the impact site. [3]

Formation of the crater — The crater was created about 50,000 years ago during the Pleistocene epoch when the local climate on the Colorado Plateau was much cooler and damper. At the time, the area was an open grassland dotted with woodlands inhabited by woolly mammoths and giant ground sloths. It was probably not inhabited by humans; the earliest confirmed record of human habitation in the Americas dates from long after this impact. [3]

The object that excavated the crater was a nickel-iron meteorite about 50 meters (54 yards) across, which impacted the plain at a speed of several kilometers per second. Impact energy has been estimated at about 10 megatons. The speed of the impact has been a subject of some debate. Modeling initially suggested that the meteorite struck at a speed of up to 20 kilometers per second (45,000 mph), but more recent research suggests the impact was substantially slower, at 12.8 kilometers per second (28,600 mph). It is believed that about half of the impactor's 300,000 metric tons (330,000 short tons) bulk was vaporized during its descent, before it hit the ground. The impactor itself was mostly vaporized; very little of the meteorite remained within the pit that it had excavated. [3]

Discovery and investigation — The crater came to the attention of scientists following its discovery by European settlers in the 19th century. Dubbed the Canyon Diablo crater - from Canyon Diablo, Arizona, the closest community to the crater in the late 19th century, 12 miles (19 km) northwest of the crater, but now a ghost town - it had initially been ascribed to the actions of a volcano. This was not an unreasonable assumption, as the San Francisco volcanic field lies only about 40 miles (64 km) to the west. [3]

Geology — The impact created an inverted topography so that the layers immediately exterior to the rim are stacked in opposite order in which they normally occur; the impact overturned and inverted the layers to a distance of one to two kilometers outward from the crater's edge. Specifically, climbing the rim of the crater from outside, one finds: [3]

  • Coconino Sandstone (sandstone formed 265 million years ago) nearest the top of the rim
  • Toroweap Formation (limestone formed 255 million years ago)
  • Kaibab Formation (dolomite formed 250 million years ago)
  • Moenkopi Formation (mudstone formed 200 million years ago) nearest the outer foot of the rim

Meteor Crater today — Meteor Crater is today a popular tourist attraction privately owned by the Barringer family, with an admission fee charged to see the crater. The Meteor Crater Visitor Center on the north rim features interactive exhibits and displays about meteorites and asteroids, space, the solar system and comets. It features the American Astronaut Wall of Fame, and such artifacts on display as an Apollo boilerplate command module (BP-29), a 1,406 pound meteorite found in the area, and meteorite specimens from Meteor Crater that can be touched. Formerly known as the Museum of Astrogeology, the Visitor Center includes a movie theater, a gift shop, and observation areas with views inside the rim of the crater. Guided tours of the rim are offered daily. [3]

  • NASA Apollo Command Module Boilerplate (BP-29A)

Special Thanks

A very special thanks to Bob Dell for providing us with photos from this location.


  1. Meteor Crater Visitor's Center, website
  2. Google Earth, Satellite Image
  3. Wikipedia, , Meteor Crater
  4. Dell, Bob. BP-29A Photo

Copyright © 2014 Skytamer Images, Whittier, California
All rights reserved