J.S. and S.W. Aber
This vicinity is part of the Osage Cuestas physiographic region, which is characterized by mixed land use—crops, grazing pasture, wooded tracts, and small towns. The nearby Verdigris River and Walnut Creek flow into Toronto Lake, a large artificial reservoir, and smaller ponds are numerous. A former Missouri Pacific railroad grade passes across this vicinity. The route is abandonned, rails and ties are removed, and the land is divided between neighboring property owners.
Surficial geology includes interbedded layers of sandstone, shale, and limestone. Oil and gas are produced in small fields nearby. The Chautauqua Hills, also known as the Cross Timbers, can be seen a short distance to the east with oak forest on sandstone outcrops.
|Left: looking toward the southeast with Toronto Lake in the right background. Diagonal path on left is the old railroad grade of the Missouri Pacific. Right: view eastward showing ponds and mixed land cover. In both views, extensive forest cover of the Chautauqua Hills is visible in the distance.|
|Left: Looking toward the northwest showing cattle, grassland, and lush green winter wheat. Right: old railroad grade of the Missouri Pacific extends to the northwest across scene center. These views of the Osage Cuestas show mostly prairie land cover and uses.|
|Views toward the southwest (left) and south-southwest (right) display cattle in prairie grassland and wooded stream valleys. Fields with greener grass were burned a few weeks earlier.|
|Authors launch a KAP rig from a pasture (left). Two horses in right background watched throughout our session. Cattle came to visit, of course (right). Cattle come for people on the ground, but horses are more interested in the kite!|
|Left: old path of the Missouri Pacific Railroad, now abandonned and returned to local private ownership. Right: soil creep on a hill side.|
|Local bedrock. Left: sandstone with iron rust (orange) and manganese stain (dark purple). Right: old quarry in the Toronto Limestone.|
Thanks to Paul Johnston for local geologic information.
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Last update: May 2014.