When the Grand Canyon Formed: The 6 vs. 70 Million Year Debate

The Grand Canyon as we see it today began taking shape roughly 5 to 6 million years ago, when the Colorado River first carved its continuous path across northern Arizona. But the full story is more complicated: parts of the canyon existed tens of millions of years before that river ever flowed through them. The modern canyon is essentially a patchwork, stitched together from older canyon segments that were carved by different rivers at different times and later connected into one enormous gorge.

The 6 Million vs. 70 Million Year Debate

For decades, geologists agreed the Grand Canyon was carved starting around 5 to 6 million years ago, when the Colorado River established its current course to the sea. Then, in 2012, a study published in Science upended that timeline. Using a technique that measures how quickly rocks cooled as they were exposed near the surface, researchers found evidence that the western Grand Canyon had been excavated to within a few hundred meters of its modern depth by about 70 million years ago. That would place the canyon’s origins in the age of dinosaurs, nearly 60 million years earlier than the standard model.

The finding ignited a fierce debate. Other researchers pushed back, pointing to geological evidence that didn’t fit a 70-million-year-old canyon. Sediment deposits, lava flows, and the chemistry of ancient water all suggested the eastern portions of the canyon were far younger. The disagreement ultimately led to a more nuanced answer: neither side was entirely wrong.

A Canyon Built in Pieces

The leading explanation today is that the Grand Canyon formed through the gradual merging of older, separate canyon segments. A 2014 study in Nature Geoscience proposed that the modern canyon was created 5 to 6 million years ago through the integration of these older paleocanyons, some of which date back to the Laramide period, roughly 85 to 40 million years ago.

During the Laramide period, tectonic forces buckled and folded the landscape across what is now Arizona, creating mountain ranges and warping rock layers into steep folds called monoclines. Rivers carved canyons through this shifting terrain, including segments on the Hualapai Plateau in the western Grand Canyon region. One major paleocanyon system, the Milkweed-Hindu channel, drained to the northeast until tectonic folding dammed it. Another segment near present-day Peach Springs was similarly blocked by deformation in the Paleocene or early Eocene, roughly 60 to 50 million years ago.

These ancient canyon fragments sat disconnected for millions of years. The western Grand Canyon appears to be the oldest piece, potentially reaching near-modern depths by 70 million years ago. The eastern canyon is considerably younger, carved mostly within the last 5 to 6 million years. Think of it less like a single river digging one long trench and more like separate ditches that were eventually linked into a continuous channel.

How the Colorado River Connected Everything

The event that finally created the Grand Canyon we recognize today was the integration of the Colorado River into a single, through-flowing system. Before about 6 million years ago, water from the Colorado Plateau didn’t drain to the Gulf of California. Instead, it pooled in interior basins, including a large body of water called ancestral Lake Hopi on the plateau’s southern margin.

Around 6.8 million years ago, geological evidence shows something dramatic happened. Sediment accumulation rates in the Bidahochi Basin (where Lake Hopi sat) jumped tenfold, from about 3 meters per million years to 50 meters per million years. The chemical signature of the sediments changed too, suggesting a major new drainage had suddenly begun feeding into the basin. Large freshwater lakes and rivers appeared in the area.

The leading theory for what happened next involves spillover. As water levels rose, the lake eventually topped a critical threshold at the southern edge of the Kaibab Plateau, near what is now the Grandview area, at roughly 2,285 meters elevation. Once water breached this divide, it cascaded into lower basins to the west and south, rapidly cutting downward through the soft and fractured rock. The Colorado River arrived downstream of the Grand Canyon sometime between 5.6 and 5.25 million years ago, completing the connection to the sea.

The Plateau That Made It Possible

None of this carving would have been possible without the Colorado Plateau rising high enough to give the river the gravitational energy it needed. The plateau’s uplift happened in three major pulses. The first occurred between 80 and 50 million years ago, raising the region by about 1 kilometer at a slow rate of roughly 0.03 millimeters per year. A second, faster phase between 35 and 15 million years ago added another 1.5 kilometers of elevation. A final phase of uplift began around 5 million years ago, coinciding neatly with the period of most intense canyon carving.

Each pulse of uplift steepened the gradient of rivers flowing off the plateau, giving them more erosive power. The combination of rising land and a newly integrated river system created the conditions for the Colorado to slice through layer after layer of ancient rock.

How Fast the Canyon Is Still Being Cut

The Grand Canyon isn’t finished. The Colorado River continues to deepen its channel, though rates vary dramatically along its length. In the eastern Grand Canyon, the river cuts downward at roughly 170 to 230 meters per million years. That translates to about 0.17 to 0.23 millimeters per year, or roughly the thickness of two sheets of paper annually.

Upstream of Lees Ferry, near the canyon’s head, rates are slower at about 110 to 130 meters per million years. But in Glen Canyon, just above Grand Canyon, erosion has accelerated sharply in the last 250,000 to 500,000 years, jumping from about 60 meters per million years to as much as 400 meters per million years. This acceleration likely reflects a “knickpoint,” essentially a steep section of riverbed that migrates upstream over time like a waterfall slowly eating its way backward.

The Rocks at the Bottom Are Far Older

While the canyon itself is millions of years old, the rocks it exposes are vastly older. The deepest layer visible at the bottom, a collection of dark, twisted rocks called the Vishnu Basement Rocks, spans from 1.84 billion to 1.375 billion years old. The oldest identified formation, the Elves Chasm pluton, crystallized 1.84 billion years ago, making it nearly half the age of Earth itself. These rocks formed deep underground as part of ancient mountain-building events long before the canyon existed. The Colorado River simply revealed them by cutting downward through the overlying layers.

This is part of what makes the Grand Canyon so remarkable as a geological record. The carving process took millions of years, but it opened a window into nearly 2 billion years of Earth’s history, stacked in colorful horizontal bands from rim to river.