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High Plains History: The Red Hills

Painting by Thelma Warner

A conventional description of the Great Plains landscape of Kansas may include references to open skies, treeless flatlands, rolling hills of shortgrass and mixed-grass prairies, and colors tending toward tan and brown. However, when we look at areas in Southwest and South-Central Kansas, the former description may not always fit. Located mostly in Clark, Comanche and Barber counties along the southern border of Kansas, there exists a physiographic province known as the Red Hills. This undulating terrain of red-tinted sediments comes from an underlying geological structure that developed when the Great Plains spanned an ancient ocean.

Around 250 million years ago, during the Permean period of geologic history, this massive inland sea began an evaporation process of periodic flooding and drying leaving behind deposits of shale, siltstones, and sandstones, interspersed with layers of gypsum and anhydrite. These deposits, known as red beds, turn red, like iron oxide, when exposed to oxygen. The porous underground of the Red Hills gave rise to another geological oddity on the Great Plains. Numerous caves thread their way through the red beds. Most of the caves tend to be small and relatively unstable, but home to a variety of bats and salamanders often studied by naturalists, scientists, teachers and students from universities throughout the region. Many of the residents in these unique ecosystems tend toward rare or endangered species. This delicate ecosystem requires a limit to human visitation to preserve the fragile underground structures.

Also known as the Gyp Hills, this secondary name acknowledges the large natural deposits of gypsum in the area. The dissolution of underlying gypsum beds contributes to the formation of sinkholesas part of the scenic vistas and small steep canyons within the Red Hills. The best-known sinkholes in the area, Big Basin and Little Basin continue to draw annual visitors. Located near Ashland in Clark County, the 1,818 acre Big Basin Prairie Preserve continues to be managed by Kansas Department of Wildlife, Parks, and Tourism, having acquired it from the Nature Conservancy in 1978 on the condition that it be operated as a nature preserve. The main features include St. Jacob’s Well, a water-filled sinkhole which lies in the Little Basin, and the Big Basin sinkhole created a lush mile-wide crater-like depression.

The Preserve reached National Natural Landmark designation while being added to the National Registry in December of 1978.

Historically, the area offered a place to camp and rest for the Northern Cheyenne People during their exodus north. In the fall of 1878, more than 300 hundred Northern Cheyenne People began the extraordinary journey back to their native lands in Montana.

Today, the Preserve takes its visitors on a trip back in time, as the prairie grasses whisper and a herd of bison freely graze near the water at St. Jacob’s Well. Other animals that use the Preserve for their shelter and sustenance include White-tailed deer, wild turkey, prairie voles, and jack rabbits. This unique region welcomes frequent visitors to drive through the preserve any time of the year.

Information used for this story came from the Kansas Country Living Magazine. For High Plains Public Radio, I’m Debra Bolton in Manhattan Kansas.

High Plains History is a production of High Plains Public Radio.

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Debra Bolton began in public radio in 1980 as a classical, jazz, and folk music hosts, at different times and in the role of news reporter. She produces about two radio shows annually, one with a focus on Geography Awareness Week in music and the annual production of Cantigas de Santa Maria, which combines her passion for history and music of medieval times.