Clinton spillway

The dam for Clinton Lake was constructed on the Wakarusa River in the late 1970s, and the spillway was carved out below the dam to hold excess water to prevent flooding if the lake's water level exceeded its capacity.

The spillway provides a rare vertical view of a sequence of rock layers that stacked one on top of the other in the Pennsylvanian subperiod about 300 million years ago. As an inland sea rose and fell over much of western North America, different types of sediments were deposited on the sea floor or along the margins of the sea, depending on the depth of the water. Those sediments were eventually buried and then compressed into limestone, shale, and other sedimentary rocks, depending on their sediment content. For example, when a clayey mud is compacted over time, it is compressed into shale, a type of mudstone.

Sequences of limestone and mudstone in the spillway exposure are part of the Oread Limestone, a formation commonly found near or at the surface throughout eastern Kansas. Strata (layers) exposed on the north face of the spillway include the Plattsmouth Limestone Member of the Oread Limestone on top down to the Amazonia Limestone Member of the Lawrence Formation.

The Oread Limestone is named after Mount Oread, the hill in Lawrence home to the University of Kansas. Geologist Erasmus Haworth was the first to describe the rock layer in 1894, which gave him naming rights. Haworth also was director of the Kansas Geological Survey in the early 1900s.


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Guidebook—Geology and Geoarcheology of Northeastern Kansas (OFR 2007-23) (pdf)