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A log stuck in the narrow walls of Buckskin Gulch, about 40 feet (12 m) above ground level. Buckskin Gulch (also known as Buckskin Creek, Buckskin Wash, and Kaibab Gulch) is a gulch and canyon located in southern Kane County, Utah, near the Arizona border in the Paria Canyon-Vermilion Cliffs Wilderness. [1]
From this trailhead, some of the hike options are the North Coyote Buttes to the Wave, to Wire Pass Narrows and onward to Buckskin Gulch. The Bureau of Land Management (BLM) limits access to the North and South Coyote Buttes Wilderness Areas. The day hike to Wire Pass Narrows begins opposite the trailhead in the wash.
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.
Buckskin Mountain and three other state parks, a wildlife refuge beloved by birders and water sports are highlights of the Colorado River at Parker. Skip to main content. 24/7 Help. For premium ...
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By 1993, a National Park Service General Management Plan, involving much public input, was adopted. As part of the planning process, the National Park Service consulted with the five Native American nations affiliated with Rainbow Bridge: the Navajo, Hopi, San Juan Southern Paiute, Kaibab Paiute, and White Mesa Ute. Chief among their concerns ...
Buckskin Mountain State Park is a state park located near Parker, Arizona, United States. A second developed area of the park is known as the River Island Unit or River Island State Park. Both park areas have shoreline on the Colorado River and views of the Buckskin Mountains. The park provides camping and water recreation opportunities.
The northwestern boundary of the plateau is marked by a fault line north of the Snake Gulch which is approximately sixteen miles to the east of the Kanab Creek. The eastern boundary is marked by the so-called Houserock Valley, which is a marble platform caused by a monoclinical fold, which strata dips down 2,000 to 3,000 feet.