Jaramillo normal event

The Jaramillo normal event is a period of normal polarity of Earth's magnetic field during the Matumaya Reversed Epoch.[1] The Jaramillo normal event is dated to 1.06 to 0.9 million years ago in the stratigraphic record of Pleistocene epoch rocks found near Jaramillo Creek in the Valles Caldera of New Mexico.

See also

References

  1. ↑ Glen, William (1982). The Road to Jaramillo. Stanford University Press.
This article is issued from Wikipedia - version of the Thursday, April 23, 2015. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.