A canyon, gorge or chasm, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering.
A natural arch, natural bridge, or rock arch is a natural landform where an arch has formed with an opening underneath. Natural arches commonly form where inland cliffs, coastal cliffs, fins or stacks are subject to erosion from the sea, rivers or weathering.
McCreary County is a county located in the U.S. state of Kentucky. As of the 2020 census, the population was 16,888. Its county seat is Whitley City. The county is named for James B. McCreary, a Confederate war soldier and two-time Governor of Kentucky. During his second term as governor, McCreary County was created by the Legislature and was named in his honor.
The Pennyroyal Plateau or Pennyroyal Region, often spelled Pennyrile, is a large physiographic region of Kentucky that features rolling hills, caves, and karst topography in general. It is named for Hedeoma pulegioides, a wild mint that grows in the area. It is also called the "Mississippian Plateau," for the Mississippian geologic age in which it was formed.
The Cumberland River is a major waterway of the Southern United States. The 688-mile-long (1,107 km) river drains almost 18,000 square miles (47,000 km2) of southern Kentucky and north-central Tennessee. The river flows generally west from a source in the Appalachian Mountains to its confluence with the Ohio River near Paducah, Kentucky, and the mouth of the Tennessee River. Major tributaries include the Obey, Caney Fork, Stones, and Red Rivers.
The Cumberland Plateau is the southern part of the Appalachian Plateau in the Appalachian Mountains of the United States. It includes much of eastern Kentucky and Tennessee, and portions of northern Alabama and northwest Georgia. The terms "Allegheny Plateau" and the "Cumberland Plateau" both refer to the dissected plateau lands lying west of the main Appalachian Mountains. The terms stem from historical usage rather than geological difference, so there is no strict dividing line between the two. Two major rivers share the names of the plateaus, with the Allegheny River rising in the Allegheny Plateau and the Cumberland River rising in the Cumberland Plateau in Harlan County, Kentucky.
A hoodoo is a tall, thin spire of rock formed by erosion. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the elements. They generally form within sedimentary rock and volcanic rock formations.
The Cumberland Mountains are a mountain range in the southeastern section of the Appalachian Mountains. They are located in western Virginia, southwestern West Virginia, the eastern edges of Kentucky, and eastern middle Tennessee, including the Crab Orchard Mountains. Their highest peak, with an elevation of 4,223 feet (1,287 m) above mean sea level, is High Knob, which is located near Norton, Virginia.
The Collins River is a 67-mile-long (108 km) stream in the east-central portion of Middle Tennessee in the United States. It is a tributary of the Caney Fork, and is part of the Cumberland, Ohio and Mississippi watersheds. The river drains the scenic Savage Gulf area, located just below the river's source, and empties into Great Falls Lake at Rock Island State Park.
The Falling Water River is a 46.8-mile-long (75.3 km) stream in the east-central portion of Middle Tennessee in the United States. It rises just west of Monterey at the edge of the Cumberland Plateau, and traverses the Eastern Highland Rim before dropping off to the Nashville Basin and emptying into Center Hill Lake along the Caney Fork. The river is noted for the 136-foot (41 m) Burgess Falls, which it spills over near the end of its course.
The Big South Fork of the Cumberland River is a 76-mile-long (122 km) river in the U.S. states of Tennessee and Kentucky. It is a major drainage feature of the Cumberland Plateau, a major tributary of the Cumberland River system, and the major feature of the Big South Fork National River and Recreation Area.
The Sheltowee Trace Trail is a 343-mile (552.00 km) National Recreation Trail that was created in 1979 and stretches from the Burnt Mill Bridge Trail Head in the Big South Fork National River and Recreation Area in Tennessee to northern Rowan County, Kentucky. The trail is named after Daniel Boone, who was given the name Sheltowee when he was adopted as the son of the great warrior Chief Blackfish of the Shawnee tribe.
Fall Creek Falls State Resort Park is a state park in Van Buren and Bledsoe counties, in the U.S. state of Tennessee. The over 30,638-acre (123.99 km2) park is centered on the upper Cane Creek Gorge, an area known for its unique geological formations and scenic waterfalls. The park's namesake is the 256-foot (78 m) Fall Creek Falls, the highest free-fall waterfall east of the Mississippi River.
Rock Island State Park is a state park in Warren County and White County, Tennessee, located in the Southeastern United States. The park is named after the community of Rock Island, Tennessee, which in turn received its name from an island on the Caney Fork upstream from the Collins River confluence and Great Falls Dam. Rock Island State Park is centered on a peninsula created by the confluence of these two rivers and extends downstream to the headwaters of Center Hill Lake.
The geology of Tennessee is as diverse as its landscapes. Politically, Tennessee is broken up into three Grand Divisions: East, Middle, and West Tennessee. Physically, Tennessee is also separated into three main types of landforms: river valley plain, highlands and basins, and mountains.
Pickett Civilian Conservation Corps Memorial State Park is a Tennessee state park in the upper Cumberland Mountains. It is located in Pickett County, northeast of the city of Jamestown, and is adjacent to the Big South Fork National River and Recreation Area. The park is located on 19,200 acres (78 km2) of wilderness including caves, natural bridges, and other rock formations. About 1,000 acres (4.0 km2) are managed by the Tennessee Department of Environment and Conservation as a state park, and the remainder of the property is managed by the Tennessee Division of Forestry as a state forest.
Scott's Gulf is a canyon situated along the Caney Fork River in White County, Tennessee, in the southeastern United States. The canyon stretches for approximately 18 miles (29 km) as the Caney Fork drops from the top of the Cumberland Plateau down to the eastern Highland Rim. This remote section of the river is home to a wilderness area consisting of a largely undisturbed deciduous forest, numerous waterfalls, caves and other geological formations, and Class IV and Class V whitewater rapids.
Pocket wilderness is a name used by Bowater corporation and the State of Tennessee for any of several tracts of Bowater-owned private land on and near the Cumberland Plateau that the company set aside beginning in 1970 "for preservation in its natural state, with no logging or development other than hiking trails permitted within its boundaries" and registered as Tennessee state natural areas. Several areas formerly managed as Bowater pocket wilderness are now incorporated into state-owned natural areas or National Park Service sites.
Conradina verticillata is a flowering shrub in the mint family, found in the Cumberland Plateau. It is also called Conradina montana, Cumberland rosemary or Cumberland false rosemary. It has been classified as a threatened species under the Endangered Species Act since 1991.
The geology of Kentucky formed beginning more than one billion years ago, in the Proterozoic eon of the Precambrian. The oldest igneous and metamorphic crystalline basement rock is part of the Grenville Province, a small continent that collided with the early North American continent. The beginning of the Paleozoic is poorly attested and the oldest rocks in Kentucky, outcropping at the surface, are from the Ordovician. Throughout the Paleozoic, shallow seas covered the area, depositing marine sedimentary rocks such as limestone, dolomite and shale, as well as large numbers of fossils. By the Mississippian and the Pennsylvanian, massive coal swamps formed and generated the two large coal fields and the oil and gas which have played an important role in the state's economy. With interludes of terrestrial conditions, shallow marine conditions persisted throughout the Mesozoic and well into the Cenozoic. Unlike neighboring states, Kentucky was not significantly impacted by the Pleistocene glaciations. The state has extensive natural resources, including coal, oil and gas, sand, clay, fluorspar, limestone, dolomite and gravel. Kentucky is unique as the first state to be fully geologically mapped.
