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Explorer Zebulon Pike first coined the name the Flint Hills in 1806 when he entered into his journal, "passed very ruff flint hills". The underlying bedrock of the hills is a flinty limestone. The largest town in the area is Manhattan, Kansas, and the hills can be accessed from the Flint Hills Scenic Byway, which passes through the region.
The Flint Hills Discovery Center is a municipal heritage and science center located in the city of Manhattan, Kansas. Featured within the facility are exhibits detailing local history and preservation of the Flint Hills , a theater, a specialized interactive playground for youth and parents, and a temporary exhibition gallery.
Flint Hills National Wildlife Refuge (NWR) is a wildlife refuge located north and east of the city of Hartford, Kansas, United States, in northwestern Coffey and southeastern Lyon Counties. It was established in 1966 as part of the U.S. Army Corps of Engineers , John Redmond Reservoir flood control project. [ 1 ]
Flint Hills Scenic Byway is a portion of K-177 located in the Flint Hills region of the state, stretching from Interstate 35 at Cassoday north to US-56 at Council Grove. Along the byway there are rolling hills and some of the only tallgrass prairie left in North America. It is a National Scenic Byway. The section of K-177 from I-70 north to K ...
For years, the restaurant was a huge draw for Strong City, a town of 400 nestled in the Flint Hills. Now, a new chef is taking over and will try to bring it back to its early glory.
The Konza Prairie Biological Station is a 8,616-acre (3,487 ha) protected area of native tallgrass prairie in the Flint Hills of northeastern Kansas. "Konza" is an alternative name for the Kansa or Kaw Indians who inhabited this area until the mid-19th century. [1] The Konza Prairie is owned by The Nature Conservancy and Kansas State University.
Over 60 million years of erosion, the Rocky Mountains created a wedge of material extending to the Flint Hills of eastern Kansas. [2] Quaternary rocks in Kansas consist of these: glacial drift; river silt, sand, and gravel; dune sand; and wind-blown silt. The Quaternary Period in western Kansas was very similar to the Neogene, continual erosion ...
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