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The San Rafael Swell attracts hikers, backpackers, horseback riders, trail runners and all-terrain vehicle (ATV) enthusiasts. Many steep, narrow slot canyons popular with technical canyoneers are found in the San Rafael Reef. [6] The Eastern Reef is a possible destination for rock climbers.
Assembly Hall Peak is part of the San Rafael Swell and is located in the Mexican Mountain Wilderness Study Area which is administered by the Bureau of Land Management. [2] Towering nearly 1,300 feet above the surrounding terrain, it is situated 1.66 miles (2.67 km) east-northeast of Bottleneck Peak and 1.52 miles (2.45 km) north of Window Blind ...
The park lies within the San Rafael Desert on the southeastern edge of the San Rafael Swell, north of the Henry Mountains. Utah State Route 24 passes about four miles (6.4 km) east of the park. Hanksville lies 12 miles (19 km) to the south.
Features a reservoir and lands for off highway vehicles and mountain biking. Otter Creek State Park: Piute: 80 acres (32 ha) 5,900 ft (1798 m) 1964 31,361 Features a 3,120-acre (1,260 ha) reservoir, begun in 1897 as one of the earliest dam projects in Utah. Palisade State Park: Sanpete: 64 acres (26 ha) 5,800 ft (1768 m) 1962 113,713
Since it enters the San Rafael Swell at an elevation well below that attained by the Swell itself and continues through the Swell's entire expanse, Muddy Creek is a very ancient river course, "superimposed" on the entire San Rafael uplift and therefore predating the time when the latter arose some 60-40 million years ago. [citation needed]
Window Blind Peak is a 7,030-foot-elevation (2,143-meter) summit located in the San Rafael Swell of Emery County, Utah, U.S. [2] [3] Towering 1,800 feet above its surrounding terrain, it is the highest point of the Mexican Mountain Wilderness Study Area. [1] Ownership is administered by the Bureau of Land Management.
This mountain consists of bleached, almost white Wingate Sandstone, which is the remains of wind-borne sand dunes deposited approximately 200 million years ago in the Late Triassic, overlain and capped by Kayenta Formation, together forming the massive San Rafael Reef, which bounds the San Rafael Swell.
The San Rafael Swell region is located west of the city, while Canyonlands National Park lies to the south. Today located exclusively in Emery County, the city was split between Emery and Grand counties until January 6, 2003, when Emery County's boundaries were expanded to follow the city limits. [6]
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