- Manson crater
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Main article: Iowa geology
Manson impact location shown in red on bedrock map of Iowa.
The Manson impact crater is near the site of Manson, Iowa where an asteroid or comet nucleus struck the Earth during the Cretaceous Period, 74 Ma (million years ago).[1] It was one of the largest known impact events to have happened in North America.[2]Previously it was thought to have led to the extinction of the dinosaurs until isotopic ages proved that it was too old.
No surface evidence exists due to comparatively recent coverage by glacial till, and the site where the crater lies buried is now a flat landscape. But, hidden about 20 to 90 m (66 to 300 ft) below the surface is a buried structure about 38 km (24 mi) in diameter. It lies under the southeast corner of Pocahontas County and extends under portions of three adjoining counties. That an anomalous structure underlaid the area was known from unusual water well drill cuttings in 1912 of deformed rock, "crystalline clast breccia with a melt matrix" as a later report described it.[3]. A research investigation was started in 1955, and it was labeled a "cryptovolcanic structure" (a hypothetical volcanic steam explosion). Further investigation was undertaken by Robert S. Dietz who proposed an impact origin in 1959 and by Nicholas Short in 1966 who produced evidence of shocked quartz grains which confirmed the impact origin of the structure.
In 1991 and 1992 the U.S. Geological Survey along with others including the Iowa Geological Survey conducted detailed research in part to test the possible connection of the Manson Crater with the Cretaceous–Tertiary extinction event. The 40Ar/39Ar isotope ratio dating of the core from the impact structure gave an age of about 74 Ma, or about 10 Ma older than the K–T boundary.[4]
The impactor is considered to have been a stoney meteorite about 2 km (1.2 mi) in diameter. The site at the time was the shore of a shallow inland sea[5] the Western Interior Seaway. The impact disrupted granite, gneiss, and shales of the Precambrian basement as well as sedimentary formations of Paleozoic age, Devonian through Cretaceous. Limestone layers that give the rest of Iowa hard water were instantaneously vaporized down to the basement rocks, giving Manson the anomalous soft water that it has today.[6]
References
- ^ "Manson". Earth Impact Database. University of New Brunswick. http://www.passc.net/EarthImpactDatabase/manson.html. Retrieved 2008-12-30.
- ^ "The Manson imact was the biggest thing that has ever ocurred on the mainland United States. Of any type. Ever," Bill Bryson, A Short History of Nearly Everything 2003:238.
- ^ Koeberl and Anderson 1996.
- ^ Izett, G. A.; Cobban, W. A.; Obradovich, J. D.; Kunk, M. J. (1993). "The Manson Impact Structure: 40Ar/39Ar Age and Its Distal Impact Ejecta in the Pierre Shale in Southeastern South Dakota". Science 262 (5134): 729–732. doi:10.1126/science.262.5134.729. PMID 17812340.
- ^ Bryson 2002:237.
- ^ Bryson 2002:237.
- Christian Koeberl and Raymond R. Anderson, eds; 1996, The Manson Impact Structure, Iowa: Anatomy of an Impact Crater, Geological Society of America Special Paper 302, ISBN 0-8137-2302-7
- Raymond R. Anderson, 1999, Iowa's Manson Impact Structure, Iowa DNR
- Additional material from Iowa DNR with image links
- Detailed illustrated time sequence of the Manson impact event from NASA
External links
U-Haul truck design website featuring the Manson impact
Coordinates: 42°35′N 94°33′W / 42.583°N 94.55°W
Categories:- Earth Impact Database
- Impact craters of the United States
- Cretaceous impact craters
- Geology of Iowa
- Geography of Pocahontas County, Iowa
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