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Vermilion Cliffs National Monument is located in northern Coconino County, Arizona, United States, immediately south of the Utah state line. This national monument, 293,689 acres (118,852 ha) [ 1 ] in area, protects the Paria Plateau, Vermilion Cliffs , Coyote Buttes , and Paria Canyon .
The Vermilion Cliffs are composed of the resistant red sandstone beds of the Lower Jurassic Moenave and Kayenta Formations. [2] They are made up of deposited silt and desert dunes, cemented by infiltrated carbonates and intensely colored by red iron oxide and other minerals, particularly bluish manganese.
The Rapid City Historic Commercial District, sometimes called the Rapid City Downtown Historic District, is a 21-acre (8.5 ha), multi-block historic district in downtown Rapid City, South Dakota, United States. It includes 47 commercial buildings dating from the late 19th to early 20th centuries that formed the core of Rapid City's early economy.
Thin ridges created by the erosion of differentially cemented, large-scale eolian cross bedding within Navajo sandstone. The Wave is a sandstone rock formation located in Arizona, US, near its northern border with Utah. The formation is situated on the slopes of the Coyote Buttes in the Paria Canyon-Vermilion Cliffs Wilderness of the Colorado ...
The Paria Canyon-Vermilion Cliffs Wilderness is a 112,500 acres (455 km 2) wilderness area located in northern Arizona and southern Utah, United States, within the arid Colorado Plateau region. The wilderness is composed of broad plateaus , tall escarpments , and deep canyons .
The northeast, east, and south of Buckskin Mountain can be accessed from U.S. Route 89A (US 89A) from House Rock, Arizona, via the House Rock Road (BLM Road 1065).The road is almost due-north trending, and in Utah, the road becomes the House Rock Valley Road, connecting to U.S. Route 89 (US‑89), 17 miles (27 km) west of Big Water.
Coyote Buttes is a section of the Paria Canyon-Vermilion Cliffs Wilderness managed by the Bureau of Land Management (BLM), spanning extreme south-central Utah and north-central Arizona, south of US 89 halfway between Kanab, Utah and Page, Arizona. It is divided into two areas: Coyote Buttes North and Coyote Buttes South.
The distinct shapes of these rocks result from an erosion-resistant layer of rock atop relatively softer sandstone. Goblin Valley State Park and Bryce Canyon National Park , also in Utah about 190 miles (310 km) to the southwest, contain some of the largest occurrences of hoodoos in the world.