Late Miocene Colorado River arrival in the Bidahochi basin supports spillover origin of Grand Canyon
Summary
The timing and mechanism of the integration of the Colorado River and incision of the Grand Canyon remain among geology's enduring controversies. A key question is the configuration of the upper Colorado River watershed between 11 and 6 million years ago. In this study, we present new evidence from zircon uranium-lead geochronology for the arrival of distinctive Colorado-Green River sediment in the Bidahochi basin by 6.6 million years ago derived from the Browns Park Formation. This is coe
Content
# Late Miocene Colorado River arrival in the Bidahochi basin supports spillover origin of Grand Canyon
*Published: 2026 Apr 16*
The timing and mechanism of the integration of the Colorado River and incision
of the Grand Canyon remain among geology's enduring controversies. A key
question is the configuration of the upper Colorado River watershed between 11
and 6 million years ago. In this study, we present new evidence from zircon
uranium-lead geochronology for the arrival of distinctive Colorado-Green River
sediment in the Bidahochi basin by 6.6 million years ago derived from the Browns
Park Formation. This is coeval with an order-of-magnitude increase in
depositional rate, an increase in carbonate strontium isotope (87Sr/86Sr)
ratios, the appearance of large fish species characteristic of fast-flowing
waters, and other sedimentological changes. This evidence is consistent with the
Colorado River supplying water and sediment to the Bidahochi basin before
spillover integration of the river through the Grand Canyon.
DOI: 10.1126/science.adz6826