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  2. San Rafael Swell - Wikipedia

    en.wikipedia.org/wiki/San_Rafael_Swell

    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.

  3. Assembly Hall Peak - Wikipedia

    en.wikipedia.org/wiki/Assembly_Hall_Peak

    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 ...

  4. Category:San Rafael Swell - Wikipedia

    en.wikipedia.org/wiki/Category:San_Rafael_Swell

    Main page; Contents; Current events; Random article; About Wikipedia; Contact us; Pages for logged out editors learn more

  5. Pediocactus bradyi subsp. despainii - Wikipedia

    en.wikipedia.org/wiki/Pediocactus_bradyi_subsp...

    It is endemic to the state of Utah in the United States, where it is limited to the San Rafael Swell in Emery County, Utah at elevations of 1450 to 2080 meters. [3] There are two populations totaling about 6000 individuals. [5] It is threatened by a number of human activities. [6] It is a federally listed endangered species of the United States.

  6. Goblin Valley State Park - Wikipedia

    en.wikipedia.org/wiki/Goblin_Valley_State_Park

    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]

  7. San Rafael Group - Wikipedia

    en.wikipedia.org/wiki/San_Rafael_Group

    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 .

  8. Muddy Creek (central Utah) - Wikipedia

    en.wikipedia.org/wiki/Muddy_Creek_(central_Utah)

    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]

  9. Emery County, Utah - Wikipedia

    en.wikipedia.org/wiki/Emery_County,_Utah

    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.

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