Jaramillo subchron

E1740071 UNEXPLORED

The Jaramillo subchron is a brief interval of normal geomagnetic polarity that occurred within the predominantly reversed Matuyama chron during the early Pleistocene.

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All labels observed (1)

Label	Occurrences
Jaramillo subchron canonical	1

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Matuyama reversed chron → contains → Jaramillo subchron ⓘ