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  • A pronghorn forages in the grasses of the San Rafael Valley, Utah. <br />
<br />
The Pronghorn (Antilocapra americana), is a species of artiodactyl mammal native to interior western and central North America. Though not an antelope, it is often known colloquially in North America as the Prong Buck, Pronghorn Antelope or simply Antelope, as it closely resembles the true antelopes of the Old World and fills a similar ecological niche due to convergent evolution. It is the only surviving member of the family Antilocapridae.
    UT-Pronghorn-SanRafael1.tif
  • A pronghorn forages in the grasses of the San Rafael Valley, Utah. <br />
<br />
The Pronghorn (Antilocapra americana), is a species of artiodactyl mammal native to interior western and central North America. Though not an antelope, it is often known colloquially in North America as the Prong Buck, Pronghorn Antelope or simply Antelope, as it closely resembles the true antelopes of the Old World and fills a similar ecological niche due to convergent evolution. It is the only surviving member of the family Antilocapridae.
    UT-Pronghorn-SanRafael3.tif
  • Pronghorns forage in the grasses and sage of the San Rafael Valley, Utah. <br />
<br />
The Pronghorn (Antilocapra americana), is a species of artiodactyl mammal native to interior western and central North America. Though not an antelope, it is often known colloquially in North America as the Prong Buck, Pronghorn Antelope or simply Antelope, as it closely resembles the true antelopes of the Old World and fills a similar ecological niche due to convergent evolution. It is the only surviving member of the family Antilocapridae.
    UT-Pronghorn-SanRafael2.tif
  • Because of its proximity to the popular Goblin Valley State Park, is easily explored, and has narrow passages as fine as any other Southwest slot, Little Wild Horse Canyon has become the most visited location in the San Rafael Swell, within Utah's Crack Canyon Wilderness Study Area.
    UT-LittleWildHorseCanyon.tif
  • Because of its proximity to the popular Goblin Valley State Park, is easily explored, and has narrow passages as fine as any other Southwest slot, Little Wild Horse Canyon has become the most visited location in the San Rafael Swell, within Utah's Crack Canyon Wilderness Study Area.
    UT-LittleWildHorseCanyon-from-above.tif
  • Because of its proximity to the popular Goblin Valley State Park, is easily explored, and has narrow passages as fine as any other Southwest slot, Little Wild Horse Canyon has become the most visited location in the San Rafael Swell, within Utah's Crack Canyon Wilderness Study Area.
    UT-LittleWildHorseCanyon3.tif
  • Because of its proximity to the popular Goblin Valley State Park, is easily explored, and has narrow passages as fine as any other Southwest slot, Little Wild Horse Canyon has become the most visited location in the San Rafael Swell, within Utah's Crack Canyon Wilderness Study Area.
    UT-LittleWildHorseCanyon2.tif
  • Because of its proximity to the popular Goblin Valley State Park, is easily explored, and has narrow passages as fine as any other Southwest slot, Little Wild Horse Canyon has become the most visited location in the San Rafael Swell, within Utah's Crack Canyon Wilderness Study Area.
    UT-LittleWildHorseCanyon1.tif
  • Eardley Pool sits near the mouth of Eardley Canyon, in Utah's San Rafael Reef at the eastern edge of the San Rafael Swell.<br />
<br />
The swell, approximately 75 miles (121 km) by 40 miles (64 km), consists of a giant dome-shaped anticline of sandstone, shale, and limestone that was pushed up millions of years ago. Since that time, infrequent but powerful flash floods have eroded the sedimentary rocks into numerous valleys, canyons, gorges, mesas and buttes.
    UT-EardleyPool-SanRafaelReef3.tif
  • Eardley Canyon cuts sharply through Utah's San Rafael Reef, at the eastern edge of the San Rafael Swell.<br />
<br />
The swell, approximately 75 miles (121 km) by 40 miles (64 km), consists of a giant dome-shaped anticline  of sandstone, shale, and limestone that was pushed up millions of years ago. Since that time, infrequent but powerful flash floods have eroded the sedimentary rocks into numerous valleys, canyons, gorges, mesas and buttes.
    UT-EardleyCanyon.tif
  • Eardley Pool sits near the mouth of Eardley Canyon, in Utah's San Rafael Reef at the eastern edge of the San Rafael Swell.<br />
<br />
The swell, approximately 75 miles (121 km) by 40 miles (64 km), consists of a giant dome-shaped anticline  of sandstone, shale, and limestone that was pushed up millions of years ago. Since that time, infrequent but powerful flash floods have eroded the sedimentary rocks into numerous valleys, canyons, gorges, mesas and buttes.
    UT-EardleyPool-SanRafaelReef.tif
  • Eardley Pool sits near the mouth of Eardley Canyon, in Utah's San Rafael Reef at the eastern edge of the San Rafael Swell.<br />
<br />
The swell, approximately 75 miles (121 km) by 40 miles (64 km), consists of a giant dome-shaped anticline  of sandstone, shale, and limestone that was pushed up millions of years ago. Since that time, infrequent but powerful flash floods have eroded the sedimentary rocks into numerous valleys, canyons, gorges, mesas and buttes.
    UT-EardleyPool-SanRafaelReef2.tif
  • Eardley Canyon cuts sharply through Utah's San Rafael Reef, at the eastern edge of the San Rafael Swell.<br />
<br />
The swell, approximately 75 miles (121 km) by 40 miles (64 km), consists of a giant dome-shaped anticline  of sandstone, shale, and limestone that was pushed up millions of years ago. Since that time, infrequent but powerful flash floods have eroded the sedimentary rocks into numerous valleys, canyons, gorges, mesas and buttes.
    UT-EardleyCanyon2.tif
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