Chuck Sutherland

For the purpose of this blog post I will be treating Standing Stone State Park and Standing Stone State Forest as a single entity. However, they are distinct, and are managed by different entities with different objectives. Both the State Park and State Forest are located entirely within Overton County, Tennessee about 10 miles northwest of the city of Livingston. Fullscreen map. Standing Stone State Park Standing Stone State Park is approximately 1000 acres surrounding Standing Stone Lake. It is itself surrounded by 8000 acres of State Forest of the same name. The park is a celebration of the efforts of the Civilian Conservation Corp (CCC). The large earthwork dam is made of hewn sandstone. Being a State Park, this area is managed for recreation. Camping there is popular at their rustic cabins. Most people come for hiking trails, fishing, and for paddle boats or kayaking on the small lake. Standing Stone State Forest There seems to be a degree of confusion as to the mea

Geography Window Cliffs State Natural Area is located on the Eastern Highland Rim of Tennessee . It is a few miles south of Cookeville, and within Putnam County. It is within the Upper Cumberland region of Tennessee, and within Middle Tennessee. Cane Creek flows through the designated natural area before its confluence with the Falling Water River at Center Hill Lake. Botany In the valley alongside Cane Creek one can find abundant flowering patches of phacelia, phlox, and trilliums. Along the rocky ledges and cliffs watch for bright red flowers of columbine. In a few places you'll also see usnea clinging to dead trees and be reminded of Spanish moss. Geology Cliffs of Fort Payne Limestone atop steep slopes of Chattanooga Shale are the obvious geology throughout the park. The base of the valleys is Catheys-Leipers Limestone, but doesn't play a large roll in the story that one sees at the Window Cliffs. In the above recreation of a map made by Hugh Mill

Photo credit Annabelle Dempsey City Lake is an artificial impoundment located near Cookeville's Eastlake subdivision. It is within property managed by the city of Cookeville as a park, named City Lake Natural Area . While the history of City Lake in Cookeville is fascinating , I could never cover it as well as Jennie Ivey has. I will simply leave you with a brief explanation of the local geology. The karst spring which feeds the waterfall is formed at the contact of the St. Louis and Warsaw Limestones ( more about those types of waterfalls here ). It is a type of geologic contact based waterfall that is seen throughout the region. Other places include Milligan Road spring, Piper Falls, High Hope Falls, and Peters Falls (all in White County, Tennessee). The reason for this is due to an abundance of chert acting as an aquatard either in the lower portion of the St. Louis, or upper portion of the Warsaw Limestone. This prevents water from moving vertically and forces its latera