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- Jaramillo_normal_event abstract "The Jaramillo normal event is a period of normal polarity of Earth's magnetic field during the Matumaya Reversed Epoch. 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.".
- Jaramillo_normal_event wikiPageID "28482468".
- Jaramillo_normal_event wikiPageRevisionID "441744206".
- Jaramillo_normal_event hasPhotoCollection Jaramillo_normal_event.
- Jaramillo_normal_event subject Category:Pleistocene.
- Jaramillo_normal_event comment "The Jaramillo normal event is a period of normal polarity of Earth's magnetic field during the Matumaya Reversed Epoch. 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.".
- Jaramillo_normal_event label "Jaramillo normal event".
- Jaramillo_normal_event sameAs m.0crcpln.
- Jaramillo_normal_event sameAs Q16897749.
- Jaramillo_normal_event sameAs Q16897749.
- Jaramillo_normal_event wasDerivedFrom Jaramillo_normal_event?oldid=441744206.
- Jaramillo_normal_event isPrimaryTopicOf Jaramillo_normal_event.