Stratigraphic nomenclature: How rocks are named

Oread Limestone road cut
Oread Limestone west of Lawrence, Douglas County.


To identify layers of rock, geologists have created several categories, the most common of which are formationsgroups, and members. In the same way that biologists use the categories of families, genera, and species to identify animals and plants (Homo sapiens is a familiar genus and species), geologists use formations, groups, and members to distinguish one rock layer from another.

The basic unit in this system of classification is the formation. A formation is a rock unit that has a distinctive appearance—in other words, a geologist can tell it apart from the rock layers around it. Formations must also be thick enough and extensive enough to plot on a map.

The sedimentary rocks of Kansas have been formally divided into many different formations, each named for the geographic locality where it was first recognized and described. The Oread Limestone, a formation common in eastern Kansas, was named in 1894 by Erasmus Haworth, the first director of the Kansas Geological Survey. He named it after Mount Oread, the hill on which the University of Kansas is located and where the limestone cropped out. The Dakota Formation, a familiar rock unit in central Kansas, got its name from the county in Nebraska where it was first described.

An important thing to remember about formations is that they often encompass a variety of rock types. For example, the Dakota Formation, although often associated with sandstone, also includes clay and shale layers. And the Oread Limestone, despite its name, contains layers of shale as well as limestone.

Formations can be lumped together into larger units called groups. For example, the Chase Group, which crops out at the surface in the Flint Hills region of Kansas, includes several different formations deposited during the Permian Period.

Formations are often subdivided into smaller units called members. For example, the Oread Limestone is divided into seven members. One of these, the Leavenworth Limestone Member, is a foot thick and can be traced for hundreds of miles. It was named for outcrops near Leavenworth, Kansas. Like formations, members keep their name no matter where they are found in Kansas.

Members make up formations. Formations make up groups. And the rocks of different groups are included under one system, based on their age. Thus, the Leavenworth Limestone Member is part of the Oread Formation, which is part of the Shawnee Group, which is part of the Pennsylvanian subsystem. The Pennsylvanian subsystem comprises rocks that were deposited during the Pennsylvanian subperiod.

When geologists propose a new name, they must publish a formal description that includes a full description of the rock unit and the location where they first found it. The procedures for classifying and naming rock units are contained in the North American Stratigraphic Code, prepared by the North American Commission on Stratigraphic Nomenclature.


Buchanan, R., 2010, Kansas Geology: An Introduction to Landscapes, Rocks, Minerals, and Fossils (2nd ed.): Lawrence, Kansas, University Press of Kansas, 240 p.

Buchanan, R., and McCauley, J. R., 2010, Roadside Kansas: A Traveler's Guide to Its Geology and Landmarks (2nd ed.): Lawrence, Kansas, University Press of Kansas, 392 p.

Kansas Geological Survey Stratigraphic Nomenclature Committee