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Utah: Kodachrome Basin State Park

9 images Created 1 Jun 2013

In Kodachrome Basin State Park, Utah, USA, see Ballerina Spire and other formations. Geologists believe that ancient hot springs and geysers in the park area filled with sediment and solidified. Through time, the Entrada sandstone surrounding the solidified geysers eroded, leaving large sand pipes. 67 sand pipes rise in the park from 2 to 52 meters high. You can drive to the park from the north via a paved road from Cannonville (and from the south via Cottonwood Canyon, Road 400, a dirt road from the Page, Arizona area, passable for most vehicles in dry conditions).

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  • Ballerina Spire, Kodachrome Basin State Park, Utah, USA. Geologists believe that ancient hot springs and geysers in the park area filled with sediment and solidified. Through time, the Entrada sandstone surrounding the solidified geysers eroded, leaving large sand pipes. 67 sand pipes rise in the park from 2 to 52 meters high. You can drive to the park from the north via a paved road from Cannonville and from the south via Cottonwood Canyon, Road 400, a dirt road from the Page, Arizona area, passable for most vehicles in dry conditions.
    1303UT-1590.jpg
  • Family riders on horseback tour the Hat Shop in Kodachrome Basin State Park, Utah, USA. Geologists believe that ancient hot springs and geysers in the park area filled with sediment and solidified. Through time, the Entrada sandstone surrounding the solidified geysers eroded, leaving large sand pipes. 67 sand pipes rise in the park from 2 to 52 meters high. You can drive to the park from the north via a paved road from Cannonville and from the south via Cottonwood Canyon, Road 400, a dirt road from the Page, Arizona area, passable for most vehicles in dry conditions.
    1303UT-1594.jpg
  • Cones of Entrada Sandstone, Kodachrome Basin State Park, Utah, USA. Drive to the park from the north via a paved road from Cannonville and from the south via Cottonwood Canyon, Road 400, a dirt road from the Page, Arizona area, passable for most vehicles in dry conditions.
    1303UT-1611.jpg
  • A white mesa and log cabin south of Cannonville, Utah, USA.
    1303UT-1627.jpg
  • Cones of Entrada Sandstone, Kodachrome Basin State Park, Utah, USA. Drive to the park from the north via a paved road from Cannonville and from the south via Cottonwood Canyon, Road 400, a dirt road from the Page, Arizona area, passable for most vehicles in dry conditions. The panorama was stitched from 5 overlapping photos.
    1303UT-1606-1610pan_Kodachrome-Basin...jpg
  • Grand Staircase-Escalante National Monument, Utah, USA. This viewpoint along Cottonwood Canyon Road is about 7 miles east of Kodachrome Basin State Park. The panorama was stitched from 3 overlapping photos.
    1303UT-1573-1575pan_Grand-Staircase-...jpg
  • Human hands have scratched handprints into sandstone at a cave in Kodachrome Basin State Park, Utah, USA. Geologists believe that ancient hot springs and geysers in the park area filled with sediment and solidified. Through time, the Entrada sandstone surrounding the solidified geysers eroded, leaving large sand pipes. 67 sand pipes rise in the park from 2 to 52 meters high. You can drive to the park from the north via a paved road from Cannonville and from the south via Cottonwood Canyon, Road 400, a dirt road from the Page, Arizona area, passable for most vehicles in dry conditions.
    1303UT-1580.jpg
  • Entrada sandstone pillar, Kodachrome Basin State Park, Utah, USA. Geologists believe that ancient hot springs and geysers in the park area filled with sediment and solidified. Through time, the Entrada sandstone surrounding the solidified geysers eroded, leaving large sand pipes. 67 sand pipes rise in the park from 2 to 52 meters high. You can drive to the park from the north via a paved road from Cannonville and from the south via Cottonwood Canyon, Road 400, a dirt road from the Page, Arizona area, passable for most vehicles in dry conditions.
    1303UT-1617.jpg
  • Ballerina Spire, Kodachrome Basin State Park, Utah, USA. Geologists believe that ancient hot springs and geysers in the park area filled with sediment and solidified. Through time, the Entrada sandstone surrounding the solidified geysers eroded, leaving large sand pipes. 67 sand pipes rise in the park from 2 to 52 meters high. You can drive to the park from the north via a paved road from Cannonville and from the south via Cottonwood Canyon, Road 400, a dirt road from the Page, Arizona area, passable for most vehicles in dry conditions.
    1303UT-1583.jpg
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