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Neumann lines, or Neumann bands, are fine patterns of parallel lines seen in cross-sections of many in the kamacite phase, although they may appear also in octahedrites provided the kamacite phase is about 30 micrometres wide. They can be seen after a polished meteorite cross-section is treated with acid. The lines are indicative of a shock-induced deformation of the crystal, and are thought to be due to impact events on the of the .O. Richard Norton, Rocks from Space, Mountain Press Pub., 1998, , page 195.

Neumann lines are named after who discovered them in 1848 in the hexahedrite meteorite which had fallen near (present-day Broumov, ) in 1847.J. G. Burke: Cosmic Debris, Meteorites in History. University of California Press, 1986.


See also
  • Glossary of meteoritics
  • Widmanstätten pattern

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