About South Park


South ParkSouth Park is a high intermontane grassland basin, approximately 10,000 ft (3,000 m) in elevation, in the Rocky Mountains of central Colorado. It encompasses approximately 1,000 square miles (2,590 km² or 640,000 acres) around the headwaters of the South Platte River in Park County approximately 60 mi (100 km) southwest of Denver. It is the southernmost of three such large mountain valleys in Colorado, along with North Park and Middle Park. The largest town in the basin is Fairplay, which sits near the northern end. In 2009, South Park was designated as a National Heritage Area.

Geologically, the valley is a wide faulted syncline sitting between the Front Range to the east and the Sawatch Uplift to the west. The Mosquito Range forms a high barrier along the western side of the valley. The long-extinct Thirty-Nine Mile volcanic field is located just to the southeast. The valley is mostly underlain by Paleozoic and Mesozoic sedimentary rocks concealed by a thin layer of gravel laid down by glaciation during Pleistocene time. The underlying rocks are dipping slightly to the east. The eastern (and newer) side of the valley is underlain primarily by Pierre Shale laid down during Cretaceous time. The western (and older) side of the valley, on the west side of Red Hill, is underlain primarily by Permian and Pennsylvanian rocks. Red Hill runs through the center of the valley as a hogback ridge of tilted Cretaceous and Jurassic sedimentary rocks.

Gold mining in South Park began in 1859. Extensive placer deposits were mined along the west side of the park, and lode deposits were mined in the Mosquito Range. The extensive gravel ridges east of Fairplay are the result of dredging for gold. (see Gold mining in Colorado). Although South Park contains some of the same geologic formations that yield oil and gas in the Denver Basin further east, efforts to find commercial oil and gas in South Park have so far proven unsuccessful. A minor amount of uranium has been mined from sandstone in South Park (see Uranium mining in Colorado).

The valley is traversed by several highways, including U.S. Route 285, which enters the valley from the eastern side over the Front Range at Kenosha Pass, providing a vehicle link to Denver. The highway crosses Red Hill at Red Hill Pass. On its northern side, the valley is connected by several high mountain passes to the valley of the North Fork of the South Platte River (a tributary of the South Platte). It is also connected by Hoosier Pass to the valley to the Blue River near Breckenridge. On its southwestern side, at the southern end of the Mosquito Range, it is connected by Trout Creek Pass to the upper valley of the Arkansas River near Buena Vista. U.S. Highway 24 enters South Park from the east at Wilkerson Pass.

Like much of the mountainous areas of Colorado, the valley was inhabited by Utes before the arrival of white settlers in the middle 19th century. It was explored by John C. Fremont during his second expedition in 1844. In 1859 the discovery of placer gold in the streams of the valley during the Colorado Gold Rush led to an influx of prospectors and miners. The town of Fairplay was founded as a more law-abiding place to live than the older, nearby town of Tarryall during this time and continued to be a center of gold, and later silver mining up through the middle 20th century. South Park City, an open air museum outside Fairplay, provides a historical recreation of the gold rush days. The basin was connected to Denver by railroad with the extension of the Denver, South Park and Pacific Railroad over Kenosha Pass in 1879.

Since the late 1990s, South Park has been best known for giving its name to the animated series South Park. Trey Parker, one of the creators of the South Park series, grew up in Conifer, about 40 miles (65 km) east of Fairplay. The famous “South Park” series has made this area popular.