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May 16, 2008Matter

Cherty Limestone

   Erosion resistant
Residual flint lag deposit
Sustains topographic relief

B ack in January this location appeared considerably different, as can be reviewed in an earlier latentsifier post. I have now photographed Konza in the winter and spring, and have assigned myself the task of recording all four of the major seasons in this unique biosphere. Here are examples of the limestone rocks that are abundant in these hills and are accountable for the shape of the land and its resistance to agricultural. The Flint Hills region presents an appealing juxtaposition of gentle ruggedness.

“No one knows what causes an outer landscape to become an inner one.” - Margaret Atwood


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