Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7013
AuthorsFolco, L.* 
Di Martino, M.* 
El Barkooky, A.* 
D’Orazio, M.* 
Lethy, A.* 
Urbini, S.* 
Nicolosi, I.* 
Hafez, M.* 
Cordier, C.* 
van Ginneken, M.* 
Zeoli, A.* 
Radwan, A. M.* 
El Khrepy, S.* 
El Gabry, M.* 
Gomaa, M.* 
Barakat, A. A.* 
Serra, R.* 
El Sharkawi, M.* 
TitleKamil Crater (Egypt): Ground truth for small-scale meteorite impacts on Earth
Issue DateFeb-2011
Series/Report no.2/39(2011)
DOI10.1130/G31624.1
URIhttp://hdl.handle.net/2122/7013
Keywordsimpact cratering
iron meteorites
shock metamorphism
Kamil Crater
Gebel Kamil
meteorite
Egypt
Subject Classification04. Solid Earth::04.04. Geology::04.04.03. Geomorphology 
AbstractSmall impact craters (<300 m in diameter) are rare on Earth and mostly deeply eroded, so that knowledge of their formation mechanism and the hazard small impactors constitute to human populations is largely based on physical models. We report on the geophysical investigation of the Kamil Crater we recently discovered in southern Egypt. The Kamil Crater is a <5 k.y. old impact crater 45 m in diameter, with a pristine ejecta ray structure. Such well-preserved structures have been previously observed only on extraterrestrial rocky or icy planetary bodies. This crater feature, and the association with an iron meteorite impactor and shock metamorphism, provides a unique impression of aspects of small-scale hypervelocity impacts on the Earth’s crust. Contrary to current models, ground data indicate that iron meteorites with masses of tens of tons may be able to penetrate the atmosphere without substantial fragmentation.
Appears in Collections:Papers Published / Papers in press

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