Kodachrome Basin State Park

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Coordinates: 37°30′2″N 112°0′2″W / 37.50056°N 112.00056°W / 37.50056; -112.00056
Kodachrome Basin State Park
Utah State Park
Clouds over Kodachrome Basin State Park.jpg
Named for: Kodachrome film
Country  United States
State  Utah
County Kane
Location Cannonville
 - elevation 5,800 ft (1,768 m) [1]
 - coordinates 37°30′2″N 112°0′2″W / 37.50056°N 112.00056°W / 37.50056; -112.00056
Area 2,240 acres (906 ha) [2]
Founded 1962
Management Utah State Parks
Visitation 49,806 (2011) [3]
IUCN category V - Protected Landscape/Seascape
Location of Kodachrome Basin State Park in Utah

Kodachrome Basin is a state park of Utah, USA. It is situated 5,800 feet (1,767.8 m) above sea level, 12 miles (19 km) south of Utah Route 12, and 20 miles (32 km) southeast of Bryce Canyon National Park. It is accessible from the north from Cannonville by a paved road and from the south by Road 400, a dirt road from the Page, Arizona area to Cannonville, passable for most vehicles in dry conditions. A longer but paved route to Tropic from the south is also available via US-89 and SR-12.

Geology[edit]

Some geologists believe Kodachrome Basin State Park was once similar to Yellowstone National Park with hot springs and geysers, which eventually filled up with sediment and solidified. Through time, the Entrada sandstone surrounding the solidified geysers eroded, leaving large sand pipes. Sixty-seven sand pipes ranging from two to 52 meters have been identified in the park.[1]

While others suggest these sandstone spires are the result of sandstone intrusions which were created as a result of the tectonic activity in the Plio-Pleistocene time, the time of the uplift of the surrounding plateaus. Indications for this model include the concentric vertical ring structure of the columns themselves where each of the three vertical rings of sandstone, central, inner, and outer, can be traced and matched to a distinct sedimentary formation below. Also the truncation of two of the structures, at Shepherd's Point, by Pleistocene sheet conglomerates, and other intrusions which pierce through Pleistocene river deposited conglomerates place the intrusion event in the Pleistocene. The river conglomerates are truncated by the sheet conglomerates. Sheet conglomerates are usually caused by major seismic activity. There are also quite large well-rounded clasts, ranging in size from 2.5 centimeters and greater, found along the outer layer of the sandstone spires which are from the Pleistocene river conglomerates. Smaller less rounded, more angular clasts, about a centimeter or less in width, are also found and are from the red claystones layers found in the intruded sandstones. These clearly indicate that the pierced formations were well lithified. Additionally, the area has large masses of sandstone dikes. The spires have no evidence of a chaotic, mixing flow regime, rather they indicate a laminar flow not suggestive of hot springs or geysers. The outer surface is highly lithified, but within a few millimeters, the sandstone is quite friable.

The primary argument against an intrusion event is the liquified state required for the seismic intrusions. The source sediments are Jurassic in age, therefore, it is argued, to have been lithified and unable to be liquified. But there are intrusive dikes which show liquification did occur. And the hardened red claystone layers, which are pierced, were fairly consolidated at time of the intrusion event, therefore, they required tremendous pressure in order to be pierced. Seismic pressure waves would provide such pressure. The fracturing of the claystones also suggest that the intrusive sandstones were point sources able to concentrate the fluid pressure to a small area of the overlaying rock. It is also noted that the intrusions cleanly sheared the claystones so that the concentric edge of the claystone abuts cleanly against the spires. The last two paragraphs are cited from:.[4]

History[edit]

Evidence near the park suggests that Native Americans were the first to wander through the area. Around the turn of the 20th century, cattlemen from Cannonville and Henrieville used the basin as a winter pasture. In 1948 the National Geographic Society explored and photographed the area for a story that appeared in the September 1949 issue of National Geographic. They named the area Kodachrome Flat, after the then relatively new brand of Kodak film they used.[5] In 1962 the area was designated a state park. Fearing repercussions from the Kodak film company for using the name Kodachrome, the name was changed to Chimney Rock State Park, but renamed Kodachrome Basin a few years later with Kodak's permission.[5]

Overview from Road 400

Recreational activities[edit]

Sand pipe, Kodachrome Basin State Park

Primary recreational activities in Kodachrome Basin State Park include photography, wildlife watching, camping, and hiking the park's several trails. Popular sites include Chimney Rock, Shakespeare Arch, and Ballerina Geyser. Stargazing is popular as the park sees little light pollution. Grosvenor Arch, an intricate double arch located ten miles south east of the park in the Grand Staircase-Escalante National Monument is a popular destination for many visitors. Kodachrome Basin State Park has 27 campsites, two of which are group sites as well as available showers. Campsites can be reserved at Reserve America. There are also six cabins inside the state park for lodging owned by Scenic Safaris. The Kodachrome Basin Blog has contact information for reserving the cabins. Horseback rides are also available throughout the park and surrounding wilderness areas.

References[edit]

  1. ^ a b "Kodachrome Basin State Park: About the Park". Utah State Parks. Retrieved 2011-02-09. 
  2. ^ Utah.com. "Kodachrome Basin State Park". Utah.com LC. Retrieved 2011-02-09. 
  3. ^ "Utah State Park 2011 Visitation". Utah State Parks Planning. Retrieved 28 May 2012. 
  4. ^ Hornbacher, Master's Dissertation, Loma Linda University, 1985
  5. ^ a b "Kodachrome Basin State Park - Utah". Todd's Desert Hiking Guide. 

External links[edit]