THE PETROGRAPHIC CONTROLS ON GYPSUM KARST SPELEOGENESIS IN SOUTHCENTRAL KANSAS
Karst features from two properties in southcentral Kansas include caves, sinkholes, springs, losing streams, and other surficial features. Caves have been hypothesized to form along the Cedar Springs Dolomite, which is found at the geologic contact between the Medicine Lodge Gypsum and the Flowerpot Shale. This study further refines the premise that caves form along the Cedar Springs Dolomite, specifically investigating the nature of the lithologic variations of this subunit.
Samples were collected from outcrops and cave passages. Elevations of samples were recorded by a handheld GPS unit for use in a relational geodatabase. These elevations help determine if samples are from the Cedar Springs Dolomite or if the samples are from other subunits within the Flowerpot Shale. Petrographic observations revealed varying lithologies ranging from dolomicrites to peldolomicrite/oodolomicrites. Future work will continue to refine the stratigraphic control on karst development on these properties to develop a larger regional model for karstification.