Montezuma Castle National Monument
Montezuma Castle National Monument, Ancient cliff dwelling in Camp Verde, Arizona, United States
Montezuma Castle is a prehistoric cliff dwelling in Camp Verde, Arizona built as a five-story structure with twenty rooms. The construction sits in a natural alcove about 90 feet (27 meters) above the Beaver Creek valley floor and was built entirely from local limestone and wood.
The site was built between 1100 and 1425 and then abandoned for reasons still unknown. President Roosevelt made it a protected monument in 1906, turning it into one of the first officially preserved indigenous sites in the United States.
The builders shaped rooms directly into the rock face and used the stone as both back wall and ceiling for their homes. Visitors today can still see how these people applied limestone mortar and fitted wooden beams to create multiple floors.
A paved trail with signs leads from the entrance to several viewing points below the dwelling. Access to the structure itself is not allowed to protect the site, and visitors can only observe the building from below.
The name has no connection to the Aztec ruler because the inhabitants left the site forty years before he was born. Early European settlers gave the place this misleading name because they believed the Aztecs had lived this far north.
Location: Yavapai County
Inception: December 8, 1906
Operator: National Park Service
Opening Hours: Monday-Sunday 08:00-17:00
Website: https://nps.gov/moca
GPS coordinates: 34.61243,-111.84166
Latest update: December 4, 2025 23:03
Arizona contains geological formations spanning millions of years alongside evidence of Spanish colonial settlement and prehistoric cultures. The landscape includes sandstone canyons such as Antelope Canyon X and Canyon de Chelly National Monument, extensive desert areas with saguaro and organ pipe cacti, and volcanic remnants at Sunset Crater. Historical sites include Spanish missions like Tumacácori, pueblo ruins at Montezuma Castle, and mining towns such as Bisbee and Jerome. The state holds significant paleontological sites at Petrified Forest National Park, where fossilized tree trunks from the Triassic period lie exposed, and cave systems like Kartchner Caverns with active speleothem formations. The Vermilion Cliffs region displays layered sandstone formations including The Wave, while the Chiricahua Mountains show volcanic rock pinnacles formed from welded ash. Waterfalls such as Havasu Falls and Grand Falls result from geological faulting and seasonal water flow. Archaeological sites document occupation by the Hohokam, Sinagua, and Ancestral Puebloans between 300 and 1400 CE. Tonto Natural Bridge forms one of the largest travertine bridges in North America, while Besh-Ba-Gowah shows Salado culture construction methods from the 13th century. The territory spans from the Sonoran Desert in the south to the Colorado Plateau in the north, creating distinct climate zones and ecosystems within a compact area.
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