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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 ...
It is known for its hiking and mountain biking trails, scenic views, and open spaces. The 1,514-acre (613 ha) park was established in 1976. [ 3 ] A 75-acre (30 ha) district, including the shrimping village and a prehistoric shell midden , were added to the National Register of Historic Places in 1979 for having state-level significance in ...
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.
The main population of the county lives along the base of these mountains. The San Rafael Swell occupies most of the area to the east. The San Rafael Reef. The western side of the county is the most populated and contains numerous small communities residing in an agricultural valley that roughly parallels the Manti National Forest to the west.
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 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. [4] [5]
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.
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]
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