The formation members, from bottom to top, are Canville Limestone, Stark Shale, and Winterset Limestone.
The three members form the major part of a cyclothem, created as sea water rise quickly and then gradually fall again over millions of years.
Simplified outline of a basic cyclothem as found in the geology of eastern Kansas, northwest Missouri, and southwest Iowa. After "Field Guide to Upper Pennsylvanian Cyclothemic Limestone Facies in Eastern Kansas", figure 4. Click to view at full size.
Photos
Dennis Formation Examples
Railroad cut showing Winterset Limestone, Dennis Formation, Upper Bronson Subgroup, Kansas City Group, Missourian Series, Pennsylvanian System. Note thin horizontal partings - very thin layers of shale separating the limestone periodically - a characteristic of many Kansas City Group limestone members. The thin shale layers represent a short period of time under different environmental conditions, or perhaps even a single catastrophic or large-scale event. Raytown, Missouri.
Railroad cut showing Winterset Limestone, Dennis Formation, Upper Bronson Subgroup, Kansas City Group, Missourian Series, Pennsylvanian System. Note the Stark Shale Member beneath the limestone - the softer shale has eroded and undercut the limestone above. Raytown, Missouri.
Railroad cut showing new rockfall Winterset Limestone next to older cliffs. Note the gray color of the weathered limestone vs the buff color of the new rockfall. Raytown, Missouri.
Detail of Winterset Limestone, Dennis Formation, Upper Bronson Subgroup, Kansas City Group, Missourian Series, Pennsylvanian System. Raytown, Missouri.
This page is based on this Wikipedia article Text is available under the CC BY-SA 4.0 license; additional terms may apply. Images, videos and audio are available under their respective licenses.