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Cathedral Rock is a natural sandstone butte near Sedona, Arizona, and one of the most-photographed sights in Arizona, United States. [3] The rock formation is located in the Coconino National Forest in Yavapai County, about 1 mi (1.6 km) west of Arizona Route 179, and about 2.5 mi (4.0 km) south of the "Y" intersection of State Routes 179 and 89A in uptown Sedona.
Slide Rock State Park is an Arizona State Park located in Oak Creek Canyon 7 miles (11 km) north of Sedona, Arizona, United States.It takes its name from a natural water slide formed by the slippery bed of Oak Creek.
Bell Rock is a butte just north of the Village of Oak Creek, Arizona, United States, south of Sedona in Yavapai County. With an elevation at its summit of 4,919 feet (1,499 m), it is just west of Courthouse Butte. Its panoramic views make it a popular landmark and tourist attraction.
Oak Creek, a tributary of the Verde River, flows along the bottom of the canyon, and is one of the few perennial streams in the high desert region of northern Arizona. Oak Creek is largely responsible for carving the modern Oak Creek Canyon, although movement along the Oak Creek Fault, a 30-mile (48 km) long north–south normal fault line, is thought to have played a role as well.
Spider Rock Pinnacle Balanced Rock The West and East Mitten Buttes Window Rock. Antelope Canyon; Canyon de Chelly National Monument. Spider Rock; Capitol Butte; Cathedral Rock, Red Rock State Park, Sedona; Cathedral Rock (Coconino County, Arizona) Chaistla Butte; Chiricahua National Monument. Big Balanced Rock; Duck on a Rock; Mushroom Rock ...
The Palatki Heritage Site is an archaeological site and park located in the Coconino National Forest, near Sedona, in Arizona, United States at approximately 34°54′56″N 111°54′08″W. In the Hopi language Palatki means 'red house'.
In the case of a massive rock slide reported Saturday, Jan. 28, in New Mexico, that riddle was solved when someone checked a Google Maps photo for the spot. That July 2022 image seems terrifying ...
The formation is the most prominent layer of the red rocks of the Sedona area due the presence of hematite – iron-oxide (rust) – giving the sandstone a red color. The Schnebly Hill Sandstone formation comprises three sections: the Bell Rock member, the Fort Apache member, and; the Sycamore Pass member. [7]