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The Flint Hills, historically known as Bluestem Pastures or Blue Stem Hills,[1] are a region in eastern Kansas and north-central Oklahoma named for the abundant residual flint eroded from the bedrock that lies near or at the surface. It consists of a band of hills stretching from Kansas to Oklahoma, extending from Marshall and Washington Counties in the north to Cowley County, Kansas and Kay and Osage Counties in Oklahoma in the south, to Geary and Shawnee Counties west to east.[2] Oklahomans generally refer to the same geologic formation as the Osage Hills or "the Osage."

Flint Hills
Map of the Flint Hills ecoregion
LocationManhattan, Kansas (largest), Great Plains, United States
Coordinates37°17′00″N 96°40′31″W
Length157 mi (253 km)
Width93 mi (150 km)
Area9,936 sq mi (25,730 km2)
Elevation1,680 ft (512 m)
WebsiteFlint Hills Website

The Flint Hills Ecoregion is designated as a distinct region because it has the densest coverage of intact tallgrass prairie in North America. Due to its rocky soil, the early settlers were unable to plow the area, resulting in the prevalence of cattle ranches as opposed to the crop land more typical of the Great Plains. These ranches rely on annual controlled burns conducted by ranchers every spring to renew the prairie grasses for cattle to graze.

The Flint Hills Discovery Center, a science and history museum focusing on the Flint Hills, opened in Manhattan, Kansas, in April 2012.


Description


Konza Prairie Preserve, a tallgrass prairie in the Flint Hills
Konza Prairie Preserve, a tallgrass prairie in the Flint Hills
A walking trail in the Konza Prairie shows the height of the grasses in the fall.
A walking trail in the Konza Prairie shows the height of the grasses in the fall.

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.


Geology


The rocks exposed in the Flint Hills were laid down about 250 million years ago during the Permian Period. During this time, much of the Midwest, including Kansas and Oklahoma, was covered with shallow seas. As a result, much of the Flint Hills is composed of limestone and shale, with plentiful fossils of prehistoric sea creatures. The most notable layer of chert-bearing limestone is the Florence Limestone Member, which is approximately 45-foot thick (14 m). Numerous roadcuts of the Florence Member are prominent along Interstate 70 in Riley County, Kansas. Unlike the Pennsylvanian limestones to the east, however, many of the limestones in the Flint Hills contain several bands of chert or flint. Because chert is much less soluble than the limestone surrounding it, the weathering of the limestone has left behind a clay soil with abundant chert gravel. Most of the hilltops in the region are capped with this chert gravel.

The highest point in the Flint Hills is Butler County High Point, with an elevation of 1680 ft (512 m).[3]


Environment


Due to shallow outcroppings of limestone and chert that lay just underneath the soil surface, corn and wheat farming were not practical over much of the area since plowing the land wasn't feasible. For this reason, cattle ranching became the main agricultural activity in the region.

Never having been ploughed over and sparsely developed, the Flint Hills represent the last expanse of intact tallgrass prairie in the nation.[4] They present the best opportunity for sustained preservation of this unique habitat that once covered the vast Great Plains. Most of the plains, such as the Central tall grasslands to the north, have better soil than the Flint Hills and a richer plant cover, but have almost entirely been converted to farmland.[2]

Landscape of Flint Hills
Landscape of Flint Hills

Tallgrass prairie is renewed by fire and grazing, which also keeps back the growth of trees and shrubs. Prominent grass species are big bluestem (Andropogon gerardi), switchgrass (Panicum virgatum), and Indian grass (Sorghastrum nutans).

Animals native to the Flint Hills include the American bison, which once grazed the area by the millions and were almost entirely exterminated, but have now been reintroduced. The elk that once roamed the region are gone.

The United States Environmental Protection Agency and the World Wildlife Fund have designated the Flint Hills as an ecoregion, distinct from other grasslands of the Great Plains.[5][6]

Four tallgrass prairie preserves are located in the Flint Hills. The largest of these, the Tallgrass Prairie Preserve, in the Osage Hills near Pawhuska, Oklahoma boasts a large population of bison and is an important refuge for other wildlife such as the greater prairie chicken (Tympanuchus cupido). The other preserves in Kansas, are the 17-square-mile (44 km2) Tallgrass Prairie National Preserve in northern Chase County near Strong City,[7][8] the Flint Hills Tallgrass Prairie Preserve east of Cassoday, "the Prairie Chicken Capital of the World",[9] and the Konza Prairie, which is managed as a tallgrass prairie biological research station by Kansas State University and is located near Manhattan.




See also



References


  1. U.S. Geological Survey Geographic Names Information System: Flint Hills
  2. Klinkenborg, Verlyn (April 2007). "Splendor of the Grass: The Prairie's Grip is Unbroken in the Flint Hills of Kansas". National Geographic. Archived from the original on February 26, 2018. Retrieved March 27, 2007.
  3. "Flint Hills". Peakbagger.com. November 1, 2004. Retrieved July 24, 2014.
  4. Berger, Joel; Beckmann, Jon (February 19, 2020). "Animals large and small once covered North America's prairies – and in some places, they could again". The Conversation. Retrieved December 16, 2020.
  5. "Ecoregion Maps and GIS Resources". United States Environmental Protection Agency. Retrieved April 10, 2008.
  6. "Flint Hills tall grasslands". Terrestrial Ecoregions. World Wildlife Fund. Retrieved April 17, 2007.
  7. "Tallgrass Prairie National Preserve". U.S. National Park Service. July 7, 2014. Retrieved July 24, 2014.
  8. "Kansas Nature Conservation, Environment Issues". The Nature Conservancy. April 11, 2014. Archived from the original on May 1, 2010. Retrieved July 24, 2014.
  9. "Kansas Nature Conservation, Environment Issues | The Nature Conservancy". Nature.org. April 11, 2014. Archived from the original on February 9, 2009. Retrieved July 24, 2014.


Maps
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На других языках


[de] Flint Hills

Die Flint Hills, historisch auch als Bluestem Pastures oder Blue Stem Hills bekannt,[1] sind eine Region im östlichen Kansas und im nördlichen Zentral-Oklahoma in den Vereinigten Staaten und wurden nach den reichlich vorhandenen Resten von Feuerstein benannt, die aus dem Grundgestein erodiert wurden und nahe oder an der Oberfläche liegen. Sie bestehen aus einem Band von Hügeln, das sich von Kansas bis Oklahoma erstreckt, vom Marshall und Washington County im Norden bis Cowley County, Kansas sowie Kay und Osage County in Oklahoma im Süden und vom Geary County im Westen bis zum Shawnee County im Osten.[2] Im Süden schließen sich die Osage Hills an.
- [en] Flint Hills



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