Hike to the river
How deep is it?
Go down, down
Slide down from the rim. How far is it to the river?
Descend from the South Rim to the Colorado River: about a mile of rock.
Slide to walk down to the river.
Your turn
Each lab is one part of the video. Tap, drag and slide, and see what happens.
Each lab isolates one process. They are simplified teaching sketches: sped up and not to scale.
Tap the buttons and slide the sliders.
Slide down from the rim. How far is it to the river?
Descend from the South Rim to the Colorado River: about a mile of rock.
Slide to walk down to the river.
Tap any layer of rock. What world was it made in, and how old is it?
Each formation records an environment. Step down the stack: lower means older.
Tap a stripe. What was there long ago?
Simplified: the canyon has nearly 40 layers; eight main ones are shown.
Drag the land (or the slider). How high did the sea-floor rock go?
Raise the block from below sea level to its present height of up to 9,000 ft.
Slide it up! The sea rock goes way up high.
Press the flood button. Each flood carries rocks that chip the riverbed deeper.
Bedload acts as the cutting tool. Each flood lowers the channel.
Press it! Rocks in the water scrape the river bottom.
Sped up: real carving took millions of years.
Tap the cliff for a rockfall, or add rain. Watch the walls step back.
Side streams, ice wedging and rockfall widen the canyon; hard layers stay as cliffs, soft ones as slopes.
Tap for a rockfall! Slide for rain.
Lift the land, then run time. What happens if the land stays low?
Combine uplift and 6 million years of downcutting and erosion. Low land gives the river little slope to cut with.
Push the land up, then slide time!
Simplified model: depth and width grow together here.
The Grand Canyon is a giant, deep valley in the rock. Its walls go down about a mile, to a river at the bottom. How did it get there? It took four big steps.
Long, long ago, sand, mud and shells piled up in layers. Slowly, they turned into stone. Some layers were made in warm seas. One was made in a sandy desert. The rock at the very bottom is the oldest of all.
The rock on top was made under the sea. But Earth slowly pushed the whole land up, flat, like a table. Now it sits way up high.
The Colorado River runs across the high land. In floods, the water rolls rocks and sand. They scrape the bottom again and again, and the river cuts down, down, down.
Rain runs down the sides. Ice cracks the rocks. Rocks fall, and the river carries them away. That is how the canyon grew so wide.
The Grand Canyon was carved by the Colorado River, working for about 5 to 6 million years through a high plateau of layered rock.17 Geologists at Grand Canyon National Park sum up the story with one easy word, DUDE:1
The river made the canyon deep. Rain, ice and gravity made it wide.7
Before there could be a canyon, there had to be rock. The walls are built from layer upon layer of rock. The National Park Service counts nearly 40 of them.2 Most are sedimentary: loose sand, mud or bits of shell that settled, got buried and slowly turned to stone, often trapping fossils as they did.5 (Want the details of how that works? See how sedimentary rocks are formed.)
Layers pile up from the bottom, so the oldest rocks are at the bottom and the youngest are on top. Geologists call this the principle of superposition. They also know layers are first laid down flat, so tilted layers mean something moved them later.1
Each layer records a different world. Here are the main ones, from the rim down. Ages are the Park Service's best estimates.3
| Layer | Age (million years) | What the world was like | Wall shape |
|---|---|---|---|
| Kaibab Formation (rim) | 270 | Warm, shallow sea1 | Cliff |
| Toroweap Formation | 275 | Shallow sea along a shifting shore | Slope and ledges |
| Coconino Sandstone | 280 | Desert of wind-blown sand dunes, with tracks of reptiles, scorpions and spiders5 | Cliff |
| Hermit Formation | 285 | Muddy rivers, seed ferns, horsetails, a dragonfly with an 8-inch wingspan5 | Slope |
| Supai Group | 290–320 | Rivers and streams on a coastal plain5 | Ledges |
| Redwall Limestone | 340 | Warm sea full of crinoids, bryozoans and snails3 | Tall cliff |
| Tonto Group (Muav, Bright Angel, Tapeats) | 504–508 | Shallow sea with trilobites5 | Slope (Tonto Platform) |
| Vishnu Basement Rocks (inner gorge) | 1,375–1,840 | Volcanic island chains that crashed into early North America, then were squeezed and heated deep underground4 | Dark, craggy gorge |
The oldest dated rock in the canyon is the Elves Chasm granite, at about 1,840 million years old.3 Even the youngest layer on the rim, at about 270 million years, is older than the oldest known dinosaurs. That's why you won't find dinosaur fossils in the Grand Canyon.5
The record isn't complete. In places, flat layers about 500 million years old sit directly on top of the ancient Vishnu rocks, with the rocks from the time in between missing. Some were never laid down, and some were worn away. Geologists call gaps like this unconformities, and the biggest one here is famous as the Great Unconformity, where more than a billion years of history is missing.74 The rocks from the "Age of Dinosaurs" that once lay on top of the rim have mostly been eroded away too. You can still see them in nearby Red Butte and in the cliffs of southern Utah.27
The Kaibab limestone on the rim formed at the bottom of a sea. Yet today it sits as high as 9,000 feet above sea level.1 Between about 70 and 30 million years ago, plate tectonics pushed the whole region upward, creating the Colorado Plateau.1
What's strange is how it rose. The rocks of the Rocky Mountains were crunched and folded as they were pushed up. The plateau's layers were lifted high and nearly flat, like a table being raised.1 Scientists are still investigating why. A leading idea is that an ocean plate, the Farallon Plate, slid under North America at an unusually shallow angle. Another is that the crust kept rising as erosion took weight off it, a process called isostatic rebound.1
Uplift mattered because it gave the river somewhere to fall. A high plateau means a steep, fast river, and a steep, fast river can cut deep.7
Water on its own is soft, so how does a river cut through rock? It uses tools. During floods, the Colorado River sweeps along huge amounts of sand, gravel and boulders, and these rocks act like chisels, chipping away at the riverbed as they bounce along.1 Before Glen Canyon Dam was built, the river carried an average of about 500,000 tons of sediment a day.7
Three things made the Colorado an unusually good canyon-cutter:1
steep slope + big floods + rock "tools" = fast downcutting
Another key event was the opening of the Gulf of California. Once the river had a path to the sea, the lowest level it could cut down to dropped by about 5,000 feet, which set the stage for carving through the plateau.1
Landscapes are harder to date than rocks, so geologists date the deposits around the river. The Hualapai Limestone, about 6 million years old, formed in a lake and has no river sediment in it, so the Colorado wasn't flowing there yet. River gravels lie under the Sandy Point Basalt, a lava flow 4.4 million years old, so the river was flowing by then. Other deposits downstream show the river was carrying plateau rock to the sea by about 5 million years ago.1 Put together, the canyon's age comes out at about 5 to 6 million years.18
A river on its own cuts a narrow slot. The canyon is up to 18 miles wide because other forces work on the walls:7
Not every layer wears down at the same speed. Hard rocks like the Coconino Sandstone and Redwall Limestone stand as steep cliffs. Softer shales like the Bright Angel and Hermit crumble into slopes. That's what gives the canyon its stair-step look.2
The dry climate is the secret ingredient. Rain is rare, so the walls wear back slowly while the river cuts down fast. In a wetter place, rain would wash the walls into a broad, gentle valley.27 Britannica goes as far as saying that without the semiarid climate, there would be no Grand Canyon.7
This is the big surprise. The rocks are old, up to about 1.8 billion years, but the canyon cut into them is young, only about 6 million years.16 Earth is about 4,560 million years old.3 If you squeezed all of Earth's history into one 24-hour day, the Grand Canyon would appear in roughly the last two minutes.
The Park Service's Trail of Time on the South Rim lets you walk this: every meter is a million years, so the canyon's entire carving fits in your last six steps, while the rocks at the bottom are nearly 2,000 steps back.63
The basic story, DUDE, is well supported. But some chapters are still argued about, and the Park Service says so openly.12
That's normal science: the evidence points clearly to a river-carved canyon, and new data keep refining the details.
Yes. The same forces are still at work, slowly deepening and widening the canyon.1 Today it's widening faster than it's deepening: the river is now cutting through very hard ancient rock, its slope has eased, and Glen Canyon Dam has tamed its floods.1 The volcanoes were busy too. Starting about 630,000 years ago, lava poured over the North Rim and dammed the river at least 13 times. The river cut through every one.1
First, layers of sand, mud and shells piled up over hundreds of millions of years and turned into rock. Then the land was pushed up into a high plateau. About 5 to 6 million years ago the Colorado River started cutting down through it, and rain, ice and side streams widened the walls. Geologists remember it as DUDE: deposition, uplift, downcutting, erosion.
The canyon itself is about 5 to 6 million years old, based on dated rocks and river gravels along the Colorado River. The rocks in its walls are much older: from about 270 million years at the rim to about 1.8 billion years at the bottom. A few scientists argue that parts of the canyon are much older, so this is still being studied.
The canyon wasn't, but many of its rock layers formed under shallow seas. The Kaibab Limestone on the rim, the Redwall Limestone and the Tonto Group all hold fossils of sea animals such as brachiopods, crinoids and trilobites. Other layers formed in deserts of sand dunes or on muddy river plains.
The Colorado River carried it away downstream, eventually toward the Gulf of California. Before Glen Canyon Dam was built, the river moved an average of about 500,000 tons of sediment every day. The sand and gravel it carried also acted like sandpaper that helped cut the canyon.
No. The National Park Service notes that glaciers never existed in or near the Grand Canyon. Dated lava flows and river deposits show the canyon was carved over millions of years, mostly during repeated floods of the Colorado River.
Each stripe is a different rock layer formed in a different environment, so each has its own colour. Hard layers such as the Coconino Sandstone and Redwall Limestone form steep cliffs, while softer shales crumble into slopes. That mix makes the canyon's famous staircase shape.
Yes, slowly. Side streams, rain and ice keep widening it, and the river keeps cutting, although it is now working through very hard ancient rock and its flow is controlled by Glen Canyon Dam, so the canyon is widening faster than it is deepening.