| Big South Fork National River and Recreation Area | |
|---|---|
| Big South Fork | |
 Rock bluffs overlooking theCumberland River in Big South Fork | |
  Big South Fork in Tennessee Show map of Tennessee Big South Fork National River and Recreation Area (the United States) Show map of the United States | |
 Interactive map of Big South Fork National River and Recreation Area | |
| Location | Scott,Fentress,Pickett, andMorgan counties inTennessee, andMcCreary County,Kentucky, United States |
| Nearest city | Oneida, Tennessee, andWhitley City, Kentucky |
| Coordinates | 36°29′11″N84°41′55″W / 36.4865°N 84.6985°W /36.4865; -84.6985 |
| Area | 125,310 acres (50,710 ha)[1] |
| Established | March 7, 1974 |
| Visitors | 797,726 (in 2022)[2] |
| Governing body | National Park Service |
| Website | https://www.nps.gov/biso/ |
TheBig South Fork National River and Recreation Area, commonly known asBig South Fork, preserves theBig South Fork of the Cumberland River and its tributaries in northeasternTennessee and southeasternKentucky.
Within it are reminders of the time when the area was subjected to logging and mining expansion. The community of No Business was located by No Business Creek in Tennessee; first settled in 1796, it had been abandoned by late 1960.[3] In addition, the formermining community ofBlue Heron, Kentucky is preserved and interpreted via signage.
The Big South Fork region contains one of the highest concentrations ofnatural bridges in the eastern United States and the area is located in parts ofScott,Fentress,Pickett, andMorgan counties in Tennessee, andMcCreary County in Kentucky. Charit Creek Lodge is a wilderness lodge, accessible by trail, located within the park.[4]
The Big South Fork was also legally designated a Kentucky Wild River by the Kentucky General Assembly through theOffice of Kentucky Nature Preserves' Wild Rivers Program.
The Big South Fork's most prominent feature is the river gorge cutting through the softer Mississippian age rock beneath the hard Pennsylvanian capstone of theCumberland Plateau. Water is the most influential agent of geologic change in the Big South Fork region. Over time water action has left many unique and amazing geologic features ranging from the river gorge with its magnificent bluffs to thenatural arches and unusualhoodoos.[5]
Due to the substantial amount of annual rainfall of the region and the action of theCumberland River and surrounding tributaries the water acts to erode the softer Mississippian rock composed oflimestone,shale, and calcareoussandstone from beneath the much harder and erosion resistant capstone composed of Pennsylvanian sandstone. Flowing water hollows out the softer layers beneath and forms waterfalls and gorges. Where there is hard capstone intact, arches can form creating natural bridges across streams or a dry ravines. Direct erosion widens a joint and forms a cavity below the more resilient rock thus creating a void between the hard capstone and the area below. As result, water eroded arches are formed in the Big South Fork.Hoodoos are a rare but intriguing feature occurring in the Big South Fork. These hoodoos form in a similar manner to those found in the western United States. Where tough capstone still exists on the side of a hill for instance, it prevents the erosion of the softer material below. The result is a naturally formed erect columnar rock where once was located a hill.[6]
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