On a high Colorado plateau, the Ancestral Puebloans built hundreds of dwellings into sandstone cliffs, then left them all behind around 1300 CE. Cliff Palace, the largest and best preserved, still stands largely intact beneath its rock alcove, doorways sealed as its builders left them.
At a glance
Mesa Verde is a flat-topped plateau stretching some 60 kilometres by 24, rising to over 2,600 metres and cut by deep canyons where Ancestral Puebloan builders raised their homes directly into the rock. The park holds thousands of archaeological sites, among them around 600 cliff dwellings, the product of nearly seven centuries of continuous occupation from roughly 600 CE until the plateau was abandoned around 1300 CE.
The cliff dwellings themselves date from only the final decades of this long history, built between about 1190 and 1280 CE. Why the Ancestral Puebloans moved from the mesa tops into the cliffs, and why they later left altogether, remains debated: proposed explanations include defence, the prolonged Great Drought of 1276 to 1299 CE, resource depletion and social change, though no evidence of warfare has been found at the site.
Key facts
- Cliff Palace: the largest cliff dwelling in North America, with 217 rooms and 23 kivas, built into a sandstone alcove roughly 90 metres wide, 30 metres deep and 30 metres high.
- Construction: small sandstone blocks, around 15 to 25 centimetres, laid in even courses with mud, water and ash mortar, and finished with the region’s characteristic T-shaped doorways.
- Kivas: circular subterranean ceremonial chambers, each serving a kin group, containing a fire pit, ventilator shaft, deflector stone and sipapu, a small hole symbolising emergence from the underworld.
- Chronology: occupied from around 600 CE, with the cliff dwellings built between roughly 1190 and 1280 CE and the plateau abandoned by about 1300 CE.
- Recognition: inscribed as a UNESCO World Heritage Site in 1978.
History
The earliest known occupation of the Mesa Verde area, the Basketmaker period, dates to around 600 to 700 CE, when people lived in pithouses dug into the ground and grew corn, beans and squash alongside hunting and gathering. During Pueblo I, roughly 700 to 900 CE, dwellings moved above ground into masonry structures, and the kiva emerged as a distinct ceremonial space evolved from the earlier pithouse.
Pueblo II, around 900 to 1100 CE, brought connections with the wider Chaco Canyon network; trade goods including turquoise, macaws, copper bells and cacao point to long-distance links reaching into Mexico. Pueblo III, from about 1100 to 1300 CE, was the period of the cliff dwellings themselves, when population peaked and the most complex structures, including Cliff Palace and Spruce Tree House, were built.
By around 1300 CE the plateau had been abandoned. Doorways were sealed with stones, suggesting a planned departure rather than flight from conflict, and tree-ring analysis of construction timbers has confirmed a severe, prolonged drought between 1276 and 1299 CE. The descendants of the Ancestral Puebloans are the modern Pueblo peoples of Arizona and New Mexico, including the Hopi, Zuni, Acoma and Taos among some fifteen other pueblos, whose oral traditions describe the migration south as a journey to find the ‘Center Place’. The site remained unrecorded by outsiders until 18 December 1888, when ranchers Richard Wetherill and Charlie Mason, tracking cattle in a snowstorm, spotted Cliff Palace across a canyon. Wetherill went on to excavate the site and sell finds to museums, and the resulting collection is now dispersed across institutions in the United States and Europe.
What you see
Cliff Palace is the park’s principal dwelling, reached only on a ranger-guided tour by ladder and cliff-side walkway. Balcony House, entered through a narrow crawlway and up vertical ladders, is considered the most physically demanding of the sites and is also ranger-guided only, not recommended for those uneasy with confined spaces or heights.
Spruce Tree House, the best preserved of the dwellings, has 130 rooms and 8 kivas and is the only major site that can normally be visited without a ranger, open year-round except in winter. The Chapin Mesa Archeological Museum traces the full sequence from Basketmaker pithouses to Pueblo III, including a reconstructed pithouse that visitors can enter. On the quieter Wetherill Mesa stands Long House, the park’s second-largest cliff dwelling, accessible only on ranger-guided tours run in summer.
Practical information
- Access to Cliff Palace and Balcony House: ranger-guided tours only, run seasonally; check the park’s official channels for current tour schedules and any charges.
- Entry: a park entrance fee applies, with additional charges for ranger-led tours; an annual national parks pass can also be used. Confirm current rates directly with the park.
- Best time to visit: ranger-guided tours of the cliff dwellings run from spring to autumn and are suspended in winter; late spring and early autumn tend to be quieter than midsummer.
Getting there
The nearest convenient airport is Durango-La Plata County Airport, about 80 kilometres east of the park. Albuquerque International Sunport lies roughly 480 kilometres to the south, and Telluride Regional Airport around 110 kilometres to the north offers a smaller regional alternative.
Nearby
- Durango, Colorado — about 80 kilometres east, the closest airport and a common base for visiting the park.
- Telluride, Colorado — around 110 kilometres north, served by its own regional airport.
- Wetherill Mesa — within the park, a quieter western section home to Long House and Step House.
Sources
- Mesa Verde National Park
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