South Park (Colorado basin)
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South Park is a high intermontane grassland basin, approximately 10000 ft (3000 m) in elevation, in the Rocky Mountains of central Colorado. It encompasses approximately 1,000 square miles (259 km²) around the headwaters of the South Platte River in Park County approximately 60 mi (100 km) southwest of Denver. It 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.
Geologically, the valley is 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 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 tilted 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 thorugh the center of the valley as a hogback ridge of tilted Cretaceous and Jurassic sedimentary rocks that have formed an intrusion through the other layers.
The valley is traversed by several highways, including U.S. Highway 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 Clear Creek (a tributary of the South Platte). It is also connected by Hoosier Pass to the valley to the Blue River near Breckenridge. On it 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.
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 . 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 during this time and continued to be a center of gold mining up through the middle 20th century. South Park City, a living 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 is best known as the name of an animated television series. Trey Parker, one of the creators of the South Park series, lived for a while in Fairplay. Hence, the television series is probably named after the geographic region.
External link
- Topographic map (http://terraserver.microsoft.com/image.aspx?T=2&S=17&Z=13&X=16&Y=168&W=2)