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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. [4] [5]
Family Butte is located 28 miles (45 km) north of Hanksville, Utah, in the San Rafael Swell on land managed by the US Bureau of Land Management.Precipitation runoff from this butte's south and east slopes drains into Little Ocean Draw → Chute Canyon → Wild Horse Creek → Muddy Creek → Dirty Devil River → Colorado River, whereas the north and west slopes drain to Muddy Creek via Reds ...
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]
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.
The San Rafael Group is a geologic group or collection of related rock formations that is spread across the U.S. states of New Mexico, Arizona, Utah and Colorado. As part of the Colorado Plateau , this group of formations was laid down in the Middle Jurassic during the Bajocian , Bathonian and Callovian Stages .
The highway follows a long valley in Eastern Utah between the Wasatch Plateau on the west and the San Rafael Swell on the east. The highway serves the primary and most active coal producing region in Utah, accounting for about 2% of the coal supply of the United States [ 2 ] Several of the routes that spur from SR-10 to cross the Wasatch ...
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