Panther Creek State Park

Panther Creek is a small, ephemeral creek that flows into Cherokee Lake. The name Panther Creek is associated with the creek because of its typical appearance during spring snowmelt. The term panther was first used in the 1760s by settlers to describe a large catlike animal they observed while encamped on Indian lands in western North America. Over time the panther became synonymous with a mountain lion, though the two animals are not closely related. Panther Creek State Park preserves an important remnant of the Appalachian Mountains that once covered eastern Tennessee and served as a corridor for animals migrating between east and west. The park features natural features representative of several different geologic formations: sandstone bluffs, ridges, river banks and ravines. Next Article


History of Panther Creek State Park

The Cherokee people once inhabited the land that is now Panther Creek State Park. In the early 18th century, Cherokee Indians and European settlers encountered one another on the lands surrounding Panther Creek. One thing that united these two groups was their common fear of the panther, which was called “Tonawanda” by the Cherokee and “Wachuka” by the Europeans.


The first American survey of the area, conducted in the 1760s, indicated that a “wild cat” was the creature of concern. In the late 18th century the Cherokee ceded most of their land to the federal government, which then opened the area to settlers. The area surrounding Panther Creek State Park was first settled by William and Ellen Mosely, who constructed a log cabin on the banks of the creek in 1816. In the late 1820s William’s son James Moseley constructed a gristmill on the banks of Panther Creek. The family operated the mill until 1840. In 1848 a road was constructed through the park, connecting Morristown, Tennessee with Fort Sanders, located on the opposite side of Cherokee Lake. This road, now Tennessee State Route 342, still runs through the park and continues to be maintained by the Tennessee Department of Transportation.


Geology and Landform Preservation

Panther Creek State Park features a diverse collection of geologic formations that are preserved in a natural environment. The park is located in the Ridge-and-Valley physiographic province, which is characterized by crumpled, folding rock strata. The oldest rocks in the park are the Precambrian monzonite rocks, which are igneous rocks that formed deep below the surface of the earth during the early days of Earth’s history. In the Silurian Period, between 440 million and 541 million years ago, the monzonite intruded Precambrian granite, creating the Panther Creek State Park landform. The monzonite rocks of the park were later intruded by granitoid magma that formed the granite that forms the creek’s bluffs. As the magma cooled and solidified, it created a series of parallel ridges known as anticlines. These ridges are the site of Panther Creek State Park’s most prominent landscape features. Learn more


Plant Life in the Park and its Surroundings

Many types of trees and shrubs are found in Panther Creek State Park, including hickory, oak, magnolia, dogwood, persimmon, paw-paw, and various species of ferns. The most common flowers are native violets and wild orchids. Many perennial wildflowers can be found in the park, including hepatica, wild geranium, trillium, and asters. The park’s natural areas include a grove of native oaks and maples surrounded by a series of low woodlands. The native dogwood, paw-paw, and maples are abundant in the park’s woodlands.


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