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Flint Hills, Kansas EarthCache

This cache has been archived.

legolaws: This one needs to go, per last message of a geocacher the signage is gone.

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Hidden : 12/8/2009
Difficulty:
1 out of 5
Terrain:
1 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

Located along Carnahan Rd. in Pott. County. This is located at a scenic overlook.

The scenic attributes of the tallgrass prairie: spaciousness, expansive grasslands, and rolling terrain are exemplified in the Flint Hills. The least disturbed and largest remaining tracts of tallgrass prairie lie in the Flint Hills, a sixty mile wide band extending from Oklahoma to this area. This region is truly unique in the North American landscape, and is worthy of preservation as a resource of national signifigance.
The Flint Hills are underlain by layers of limestone and shales which were deposited by ancient inland seas that covered the mid continent millions of yeras ago. Large quantities of flint and chert nodules formed within the limestone, as percolating waters dropped silica around bits of shell and plant stems.
Later the region was uplifted and the seas drained. Sixty million years of erosion removed the overlying sediments. The limestones, more arrestant than the shales, formed the numerous ridges. The hard, insoluble chert nodules have been left behind to give the Flint Hills their name. The flat topped hills and deeply dissected scarps with terraced slopes provide splendid scenic vistas.

The Flint Hills were created approximately 250 million years ago during the Permian Period. During this time much of the Midwest, including Kansas and Oklahoma, were covered with shallow seas. As a result, much of the Flint Hills are 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. It is approximately 45 feet thick; numerous roadcuts of the Florence Member are prominent along Interstate 70 in Riley County, Kansas. Many of the honey-colored limestones have been used for building blocks. The non-chert-bearing limetones are best for this, since the chert is extremely hard to cut, yet it can fracture quite easily.

Beginning in the mid-1800s homesteaders replaced the American Indian in the Flint Hills. Due to shallow outcroppings of limestone and chert, farming was not practical over much of the area, and cattle ranching became the main agricultural activity in the region. Still sparsely developed, the Flint Hills represent the last expanse of tallgrass prairie in the nation.

Logging Requirements:

First, go to the coordinates and find the plaque/sign and email me the name of the person who gave the quote written on the plaque/sign.

Second, look to the west and include in your email your best guess as to how tall the limestone hill is.

Third, take a picture of yourself in front of the Flint Hills at this location. Hope you enjoy the trip through the Flint Hills!

Congratulations to JJTally on the FTF!

Additional Hints (No hints available.)