Turner Falls

Turner Falls is a prominent waterfall and the centerpiece of Turner Falls Park, located within the Arbuckle Mountains of southern Oklahoma. The 77-foot cascade is formed as Honey Creek plunges over a resistant shelf of Arbuckle limestone into a natural swimming pool below. As the largest waterfall in the state, it has been a major tourist destination since the late 19th century, drawing visitors to its scenic beauty and the surrounding geological formations of the Arbuckle Mountains.

Geography and location

Turner Falls is situated in Murray County, approximately 6 miles south of the city of Davis. The waterfall lies within the rugged terrain of the Arbuckle Mountains, a region characterized by ancient, folded rock strata. The area is part of the larger Cross Timbers ecoregion transition zone. The waterfall flows within the watershed of Honey Creek, a tributary that eventually feeds into the Washita River. The surrounding landscape is managed as Turner Falls Park, a municipal park owned by the city of Davis.

History

The waterfall and surrounding area were historically within the territory of the Chickasaw Nation following their forced relocation via the Trail of Tears. The site is named for Mazeppa Thomas Turner, a Texas surveyor who reportedly first documented the falls in 1878. By the 1880s, the location began attracting visitors, facilitated by the expansion of the Santa Fe Railway through the region. In the early 20th century, the land was purchased by Dr. Elias M. Boren, who developed initial tourist facilities. The city of Davis acquired the property in 1919, formally establishing the public recreation area. The Civilian Conservation Corps contributed to developing park infrastructure during the Great Depression.

Geology and formation

The waterfall is a classic example of a caprock cascade, where a durable layer of rock overlies a softer stratum. The caprock is composed of the Arbuckle limestone, a formation dating to the Ordovician period over 400 million years ago. This limestone rests upon less resistant layers of shale and sandstone. The plunge pool at the base of the falls has been excavated by the erosive force of the falling water and abrasive sediments carried by Honey Creek. The entire region is part of the Arbuckle Mountains, an anticlinal structure that is one of the oldest geological exposures in North America, providing a window into ancient marine environments.

Tourism and recreation

As the focal point of Turner Falls Park, the waterfall anchors a major recreational destination. Primary activities include swimming in the natural pool below the falls, hiking on trails such as the path to the adjacent Collings Castle, and exploring other natural features like caves and springs. The park offers extensive amenities including campgrounds, cabins, picnic areas, and concession facilities. Annual events and its proximity to other attractions like the Chickasaw National Recreation Area and Lake Murray State Park contribute to its popularity, particularly during the summer months.

Conservation and management

The site is managed by the city of Davis through its park administration, with operations funded by visitor entrance fees. Conservation challenges include managing the environmental impact of high visitor traffic, preventing pollution in Honey Creek, and preserving the integrity of the unique geological formations. The area's ecology is part of the sensitive transition zone of the Cross Timbers. Management practices often involve coordination with state agencies like the Oklahoma Department of Tourism and Recreation and the Oklahoma Department of Environmental Quality to balance recreational use with the preservation of natural resources.

Category:Waterfalls of Oklahoma Category:Murray County, Oklahoma Category:Arbuckle Mountains