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People have farmed this free Arizona canyon for 5,000 years, and still do

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Close view of White House Ruin. Postprocessed by keninglory/ Brocken Inaglory .

It’s a living Navajo world, not a ruin

Canyon de Chelly sits in northeastern Arizona, deep inside the Navajo Nation, and it costs nothing to get in.

The name comes from the Navajo word Tseyi, meaning “rock canyon,” which Spanish settlers heard and reshaped into something they could pronounce.

Three canyons spread across more than 83,000 acres here, and about 40 Navajo families still farm and raise livestock on the canyon floor. This is not a preserved-in-amber past.

People wake up here every morning.

This is an image of a place or building that is listed on the National Register of Historic Places in the United States of America . Its reference number is 70000066 ( Wikidata ).

Five thousand years of people calling this place home

No other landscape on the Colorado Plateau has been lived in this long.

Archaic people camped in these canyons as far back as 2500 BC, leaving behind fire pits and rock carvings.

Ancestral Puebloans arrived later and built cliff dwellings into the sandstone walls, staying until a long drought pushed them out around 1300 AD. The Hopi moved through seasonally after that.

Then, about 600 years ago, the Navajo settled in and stayed.

The monument became official on April 1, 1931, but the canyon’s story starts thousands of years earlier.

This is an image of a place or building that is listed on the National Register of Historic Places in the United States of America . Its reference number is 70000066 ( Wikidata ).

Spider Rock rises 750 feet straight off the canyon floor

At the point where Canyon de Chelly meets Monument Canyon, a single sandstone spire shoots up from the floor.

Spider Rock stands more than 750 feet tall, and it got there the same way most of the Southwest’s dramatic formations did: wind and water dissolved everything around it over millions of years and left the tower standing alone.

In Navajo tradition, Spider Rock is the home of Spider Woman, the figure who taught the Dine the art of weaving and whose teachings connect to the Beauty Way, a way of living in balance.

The Spider Rock Overlook on South Rim Drive draws people at sunset for good reason.

Sandstones in the Permian of Arizona, USA. The cliffs of this Arizona canyon are composed of the Lower Permian De Chelly Sandstone (pronounced "De Shay"). Most of the unit is horizontally-bedded and cross-bedded quartzose sandstones representing ancient sand sheets and desert sand dunes. A vast sand dune "sea" was present at the time - such an environment is called an "erg" (a modern example is northern Africa's Sahara Desert). The reddish-brown coloration is from hematite (iron oxide, Fe2O3). Stratigraphy: De Chelly Sandstone, Leonardian Stage, Lower Permian Locality: view from Sliding House overlook, southern rim of Canyon de Chelly, Canyon de Chelly National Monument, northeastern Arizona, USA

Drive South Rim Road and look down at ancient ruins

South Rim Drive runs 16 miles one way from the visitor center, with seven overlooks spaced along the route. Give yourself two to three hours round-trip if you stop at most of them.

From Junction Overlook, you can see the point where Canyon de Chelly and Canyon del Muerto come together below.

Sliding House Ruin appears from the rim with ancient walls that look like they’re sliding down the cliff face.

Spider Rock Overlook waits at the end of the road, and the views across the canyon and spire make it the stop most people remember the longest.

Sandstones in the Permian of Arizona, USA. The sheer walls of this Arizona canyon consist of Permian-aged De Chelly Sandstone (pronounced "De Shay"). Most of the unit is horizontally-bedded and cross-bedded quartzose sandstones representing ancient sand sheets and desert sand dunes. A vast sand dune "sea" was present at the time - such an environment is called an "erg" (a modern example is northern Africa's Sahara Desert). The reddish-brown coloration is from hematite (iron oxide, Fe2O3). Stratigraphy: De Chelly Sandstone, Leonardian Stage, Lower Permian Locality: view from Mummy Cave overlook, "Canyon del Muerto" (= Canyon of the Dead), Canyon de Chelly National Monument, northeastern Arizona, USA

North Rim Drive is where the morning light does its best work

North Rim Drive follows Canyon del Muerto for about 15 miles one way and has three overlooks. Photographers tend to prefer it in the early hours when the light falls at a low angle across the canyon walls.

Antelope House Overlook puts you above a large Ancestral Puebloan ruin sitting right on the canyon floor, named for antelope paintings a Navajo artist named Dibe Yazhi made there in the 1830s.

At some overlooks, fixed telescopes let you pick out details in the ruins that you’d otherwise miss from the rim.

This is an image of a place or building that is listed on the National Register of Historic Places in the United States of America . Its reference number is 70000066 ( Wikidata ).

White House Ruin is built into a 500-foot cliff wall

Of all the Ancestral Puebloan sites in the American Southwest, White House Ruin ranks among the most recognized. Builders carved it into a sandstone cliff and lived there from about 1060 to 1275 AD.

The name comes from the white plaster that once covered the long back wall of the upper dwelling. At its height, the complex may have held up to 80 rooms and four kivas.

The White House Trail descends 2.5 miles round trip to the ruin, and it’s the one place in the canyon you can walk without a guide.

The trail was closed for several years and reopened seasonally in mid-2024, so check current status before you plan your hike around it.

This archaeological site in Arizona's Canyon de Chelly is called "Mummy Cave". The rocks in the cliff are part of the Permian-aged De Chelly Sandstone (pronounced "De Shay"), an ancient sand dune deposit. Stratigraphy: De Chelly Sandstone, Leonardian Stage, Lower Permian Locality: view from Mummy Cave overlook, "Canyon del Muerto" (= Canyon of the Dead), Canyon de Chelly National Monument, northeastern Arizona, USA Info. at: www.nps.gov/articles/dechelly.htm

Mummy Cave has stood occupied for a thousand years

Mummy Cave sits about 300 feet above the floor of Canyon del Muerto, tucked into two deep alcoves with a three-story tower between them. Timbers in that tower date to 1284 AD.

The complex holds about 70 rooms, including spaces for living, storing food, and conducting ceremonies, and people lived here from roughly 300 AD to 1300 AD.

Two mummified bodies found in the alcoves during the 1880s gave the site its name. Scholars who study the architectural style believe some of the final builders here came from Mesa Verde.

View of rock art panel at mouth of the Canyon Photos from Canyon de Chelly National Monument near Chinle, Arizona during the development of an exotic species removal plan for tamarisk and Russian olive. Keywords: exotic species removal; rock art panel; Tamarix -- Control; (LCSH); Russian olive -- Control; Invasive plants; Petroglyphs; Rock painting

More than 2,700 archaeological sites cover these canyon walls

The canyon holds petroglyphs chipped into dark desert varnish and pictographs painted directly onto the rock, and they cover a lot of ground.

Ancient panels show human figures, animals, spirals, and handprints pressed flat against the stone. Later images record the arrival of Spanish conquistadors on horseback.

Ancestral Puebloan figures with hands pointing down signal welcome; hands pointing up signal danger. Nearly all of this rock art sits on the canyon floor, and you won’t see most of it from the rim.

That’s one more reason the guided tours are worth it.

Trail to the White House Ruin. A small tunnel near trailhead.

Hire a Navajo guide and go down into the canyon

The only way into the canyon is with an authorized Navajo guide, unless you’re walking the White House Trail on your own.

Tours run by four-wheel-drive vehicle, on horseback, or on foot, and most vehicle tours last three to six hours.

Your guide walks you through the ruins, points out rock art, and shares Navajo oral histories and personal stories about life in the canyon. Many guides grew up here and have family connections going back generations.

Book ahead if you’re coming between April and October.

Canyon de Chelly National Monument

Wild horses cross the canyon floor between the cottonwood groves

In autumn, the cottonwood trees that line the canyon floor go gold, and the color against the red sandstone walls stops people mid-step. Wild horses roam freely along the rim and down on the floor below.

Navajo families tend orchards, farms, and sheep pastures in the same canyon, the same way their families have for centuries.

The dark streaks running down the canyon walls are desert varnish, left by mineral-rich water cascading over the sandstone.

The layers of stone themselves formed during the Permian and Triassic periods, somewhere between 230 and 280 million years ago.

This is an image of a place or building that is listed on the National Register of Historic Places in the United States of America . Its reference number is 70000066 ( Wikidata ).

The welcome center sets you up before you head out

The Welcome Center opens daily at 8 a.m. and closes at 5 p.m., with closures on Thanksgiving, Christmas and New Year’s Day. Inside, a 22-minute film gives you the lay of the land, and rangers stock the place with maps.

Free ranger-led hikes run seasonally from Memorial Day through Labor Day.

One thing that catches people off guard: the Navajo Nation observes Daylight Saving Time even though the rest of Arizona does not, so adjust your clock when you cross into the Nation.

The town of Chinle, about three miles away, has lodging and food.

Canyon in Arizona, beautiful geological formations.

Canyon de Chelly leaves a mark that doesn’t fade quickly

Canyon de Chelly draws far fewer crowds than the Grand Canyon, even though it ranks among the most visited national monuments in the country. That contrast matters.

You can stand at an overlook and hear nothing but wind.

You can ride through the canyon floor and pass land that Navajo families have worked for generations. Every tour you book through an authorized Navajo-owned company puts money directly into the community.

Sandstone walls, ancient rooms built into cliffs, sacred landmarks, and a living culture that never left: there’s nothing else quite like it in the national park system.

English: Conglomerate & sandstone in the Permo-Triassic of Arizona, USA. These are rimrocks atop a canyon wall in Arizona. The lighter-colored rocks below are cross-bedded and horizontally-bedded quartzose sandstones of the Permian-aged De Chelly Sandstone (pronounced "De Shay"). Most De Chelly sandstones are ancient desert sand dune deposits. The darker-colored rocks above are the Shinarump Conglomerate, an Upper Triassic, fluvial, coarse-grained siliciclastic unit. It consists of quartzose sandstones, pebbly sandstones, and lithic conglomerates. The De Chelly-Shinarump contact is a significant unconformity - an erosion surface representing missing time. There are several types of unconformities - this is a disconformity, which has sedimentary rocks over sedimentary rocks, with parallel bedding geometries ("flat over flat"). Stratigraphy: Shinarump Conglomerate Member, lower Chinle Formation, Norian Stage, Upper Triassic disconformably overlying De Chelly Sandstone, Leonardian Stage, Lower Permian Locality: view from Antelope House overlook (Navajo Fortress overlook), northern rim of "Canyon del Muerto" (= Canyon of the Dead), Canyon de Chelly National Monument, northeastern Arizona, USA

Visit Canyon de Chelly National Monument in Arizona

To get there, take US Highway 191 to Chinle, then head east on Indian Route 7 to the visitor center. There’s no entrance fee to enter the monument.

Authorized Navajo-owned tour companies run guided canyon tours, which you can arrange at the visitor center or book in advance through the official website.

The Cottonwood Campground near the entrance is first-come, first-served.

Chinle, about three miles from the entrance, has motels and restaurants if you need a place to stay overnight.

This article was created with AI assistance and human editing.

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John Ghost is a professional writer and SEO director. He graduated from Arizona State University with a BA in English (Writing, Rhetorics, and Literacies). As he prepares for graduate school to become an English professor, he writes weird fiction, plays his guitars, and enjoys spending time with his wife and daughters. He lives in the Valley of the Sun. Learn more about John on Muck Rack.

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