1966 Map of Park City

About this map

Diamond Caverns and Jessie James Cave highlight the subterranean character of this landscape at the southern edge of Mammoth Cave National Park. The mid-1960s terrain is defined by a karst topography of sinkholes and ridges known as The Knobs, including Bald Knob and Brushy Knob. The Louisville and Nashville railroad corridor serves as the primary artery through Park City, which appears here with its local High Sch and Evergreen Cem. Settlement patterns follow the winding routes south of the rail line, connecting smaller communities like Merry Oaks, Apple Grove, and Stovall. Rural life is centered around several modest congregations, such as Walnut Hill Ch and Cedar Hill Ch, while the drainage of Little Sinking Creek illustrates the complex hydrology of the Barren County countryside.