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February 25, 2025

Colorado Plateau's dramatic canyons: How rivers' ancient pauses and rapid cuts shaped them

The Colorado River, as seen from Dead Horse Point State Park in Utah, has been shaping the features of the Colorado Plateau for millions of years. Credit: Natalie Tanski
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The Colorado River, as seen from Dead Horse Point State Park in Utah, has been shaping the features of the Colorado Plateau for millions of years. Credit: Natalie Tanski

Long after tectonic plate movement has created mountains, forces such as weather and river erosion can continue to shape a landscape. One such landscape is the Colorado Plateau, which spans more than 336,000 square kilometers (83 million acres) across four states and encompasses iconic sites such as the Grand Canyon and Arches National Park.

Dramatic gorges such as these are created when a river incises into the rock below over millions of years. The rate of river incision in the Colorado Plateau has varied over time and is not well understood.

Natalie Tanski and colleagues looked at two reaches of the Colorado River to determine how and why incision varied during the Pleistocene, dating fluvial gravel deposits that form river terraces, which are steplike features that mark the former floors of river valleys. Their study is in the journal AGU Advances.

To constrain the ages of the river terraces, they used luminescence dating, which measures a mineral's release of photons to determine the last time it was exposed to sunlight or intense heat, and isochron dating, a form of radioactive dating that, in this case, measured the changing relative abundance of beryllium and aluminum isotopes.

They then simulated how and when a wave of incision may have migrated up through a in response to a change in baselevel, the lowest point that a river can erode. They compared the results to their terrace ages to determine whether drops in baselevel could have contributed to unsteady incision rates.

The researchers found that in the Moab region of the central Colorado Plateau, river incision paused from 1.8 million years ago to about 350,000 years ago. This pause was followed by a period of rapid lasting to the present, during which the river systems carved 200 meters deeper into the plateau. These shifts can be linked to base-level changes as the Colorado River established its path, eventually contributing to the shape and iconic chasm of the Grand Canyon and its tributaries.

However, this particular period of rapid erosion represents only about a quarter of the total exhumation that took place in the central Colorado Plateau over a much longer time period, suggesting that yet-unknown events occurring millions of years earlier may have also shaped the landscape.

More information: Natalie M. Tanski et al, The Mystery of Baselevel Controls in the Incision History of the Central Colorado Plateau, AGU Advances (2025).

Journal information: AGU Advances

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The Colorado Plateau's dramatic canyons, including the Grand Canyon, were shaped by varying rates of river incision over millions of years. Analysis of the Colorado River's terraces using luminescence and isochron dating revealed a pause in incision from 1.8 million to 350,000 years ago, followed by rapid erosion. This rapid incision, linked to base-level changes, carved 200 meters deeper into the plateau, but earlier events likely also influenced the landscape's formation.

This summary was automatically generated using LLM.