Panguitch Utah is located in southern Utah on the eastern side of the Paunsaugunt Plateau in Garfield County. Settlement of the area began in 1874. Ebenezer Bryce moved from Pine Valley and settled a site near the mouth of Bryce Canyon in 1875. Bryce used the now famous canyon as a cattle range, and it was given his name as early as 1876.

Panguitch Utah is a series of natural amphitheaters below which stands an array of white and orange limestone columns and walls sculptured by erosion. The erosion has been accomplished mainly by rain, snow, and frost prying off cliff fragments rather than by stream erosion. Nearby streams actually flow away from the canyon. The high rim country of the park is part forest dominated by fir, pine, and aspen, and part meadows of grass and sage. At lower, drier altitudes, pinon pine and Utah juniper predominate.

Panguitch Utah awaited promotion and development before its full tourism potential could be realized. National Forest Supervisor J. W. Humphrey was transferred from the La Sal National Forest to the Powell National Forest on 1 July 1915. He was amazed at the beauty and grandeur of Panguitch Utah and resolved to do all he could to promote it and make it accessible. He took visiting dignitaries to Panguitch Utah and secured funds for a passable road to the canyon rim. In 1916 Arthur W. Stevens of the Forest Service wrote an illustrated article for the Union Pacific railroad tourist magazine. J. W. Humphrey wrote a similar article for the Rio Grande railroad. These were the first descriptive articles published about Panguitch Utah . In the meantime, moving pictures and postcards began circulating and Panguitch Utah began to attract visitors from all parts of the nation. For more Panguitch Utah information resources click here.