wupatki national monument Trails

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Sunset Crater and Wupatki National Monuments Scenic Drive: Sunset Crater - Wupatki Loop Road :: Flagstaff, AZ

This 35-mile long loop drive passes a spectacular volcanoscape at Sunset Crater Volcano National Monument and explores ancient Anasazi and Sinagua ruins at Wupatki National Monument.

Sunset Crater and Wupatki National Monument :: Flagstaff, AZ

Sunset Crater National Monument is a 1,000-foot-high historic cone. Here you will find strange rivers of lava that erupted 900 years ago that look as though they happened yesterday. There are many trails to hike along and explore; visitors, however,

Wukoki Pueblo Trail :: Wupatki National Monument, AZ

Wukoki Pueblo Trail is a hiking trail in Coconino County, Arizona. It is within Wupatki National Monument. It is 0.2 miles long and begins at 4,624 feet altitude. Traveling the entire trail is 0.4 miles with a total elevation gain of 84 feet. Near th

Wupatki Pueblo Trail :: Wupatki National Monument, AZ

Wupatki Pueblo Trail is a hiking trail in Coconino County, Arizona. It is within Wupatki National Monument. It is 0.4 miles long and begins at 4,913 feet altitude. Traveling the entire trail is 0.4 miles with a total elevation gain of 85 feet. The Wu

Doney Trail :: Flagstaff, AZ

A very easy, short walk to the top of a volcanic cinder cone with an extensive view of the Painted Desert, near Wupatki National Monument. The broad, easy trail heads south toward the low saddle between two of the cinder cones. From the saddle, you c

Wupatki Ruin :: Flagstaff, AZ

A short walk around an extensive, well-preserved Sinagua Indian ruin in Wupatki National Monument. It is worthwhile spending time in the visitor center to learn about the Sinagua Indians who built Wupatki and many other structures in the area. The

Doney Trail :: Flagstaff, AZ

This very easy, short walk to the top of a volcanic cinder cone features an extensive view of the Painted Desert near Wupatki National Monument. The soft, rounded slopes, bluffs, and mesa in the distance to the northeast were formed when the soft,