The Jaramillo normal event is a period of normal polarity of Earth's magnetic field during the Matuyama 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 edit
References edit
- ^ Glen, William (1982). The Road to Jaramillo. Stanford University Press. ISBN 9780804711197.
 | This geology article is a stub. You can help Wikipedia by expanding it. |
 | This geophysics-related article is a stub. You can help Wikipedia by expanding it. |