
Montezuma Castle National Monument
Interesting facts
- Neither half of the name fits: the Sinagua had no link to the Aztecs, and the building was less a castle than an early multi-storey apartment block.
- Residents almost certainly climbed in on portable ladders, which could be pulled up to leave attackers facing a sheer cliff face.
- Its roof beams came mostly from Arizona sycamore, with ash, alder, ponderosa pine, Douglas fir and pinyon pine also used for the ceilings.
- Studies of the walls show the builders mixed several different mud mortars, each suited to a particular need such as strength, durability or colour.
- In the mid-11th century the eruption of Sunset Crater, about 60 miles to the north, briefly emptied the area before the Sinagua returned to the valley.
- Volcanic ash from that eruption may have enriched the soil, helping the larger-scale farming that sustained the valley in later generations.
- The ruined neighbouring site, Castle A, was excavated in 1933, and its finds gave archaeologists a far clearer picture of daily life in the valley.
- An army doctor, Edgar A. Mearns, described the dwelling in Popular Science Monthly in 1890, before heavy looting stripped much of the site.
- Its designation as a monument owed much to the efforts of archaeologist Edgar Lee Hewett and Iowa senator John F. Lacey.
- A survey in the early 1990s recorded about 784 species of plants and animals within the monument, only around 11 per cent of them non-native.
Why it is worth it
Set into a recess about 27 metres (90 feet) up a pale limestone cliff above Beaver Creek, Montezuma Castle is one of the best-preserved cliff dwellings in North America. The five-storey building of stone and mud mortar holds at least twenty rooms and was home to perhaps thirty people at its peak. It was raised by the Southern Sinagua, a farming people of the Verde Valley in central Arizona, with the main construction dated to roughly 1125–1173 and further work carried out in the 13th century. Its position high in the cliff kept it dry, defensible and shaded from the summer sun, which is a large part of why its walls and roof beams have survived so well.
The name is a historical mistake. Early European-American settlers assumed such a structure must be connected with the Aztec ruler Montezuma, yet the dwelling had been abandoned for more than forty years before he was born. The Sinagua left the valley by about 1400. Nearby stood a far larger complex, known as Castle A, with an estimated 45 rooms; it burned in the late 14th century and survives only as low foundations at the foot of the cliff. Many present-day Native American communities trace their ancestry to people who lived in and around the cliff dwelling.
On 8 December 1906 President Theodore Roosevelt proclaimed Montezuma Castle a national monument, one of the first four created under the new Antiquities Act. The dwelling is seen from a short paved trail that loops along the creek below the cliff. A detached unit of the monument about 18 km (11 miles) to the north-east, Montezuma Well, protects a spring-fed limestone sinkhole some 118 metres across, with Sinagua dwellings in its rim and the remains of an irrigation canal that once watered fields below.
Getting there
Montezuma Castle lies just north of Camp Verde in Yavapai County, Arizona, close to exit 289 of Interstate 17. The largest nearby city is Prescott Valley, about 44 km away in a straight line. The nearest airport is Flagstaff Pulliam Airport (FLG), about 60 km to the north; Phoenix Sky Harbor International Airport (PHX) lies further south along Interstate 17.
Plan your visit
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Nearby places
- Cathedral Rock (Sedona) 23.4 km · rock-formation
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From the encyclopaedia
Montezuma Castle National Monument protects a well-preserved cliff dwelling located in Camp Verde, Arizona. The National Monument also protects and preserves the Castle A site, a contemporaneous dwelling site located near the cliff dwelling. The construction of the Montezuma Castle and Castle A sites are both attributed to the Southern Sinagua people, a pre-Columbian archaeological culture that may be closely related to several ancestral indigenous peoples of the southwestern United States. Archaeological evidence suggests that the dwelling was constructed as early as 1125 AD and occupied until as late as 1395 AD.
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