DRAFT 8/8/2013 Updates at Chapter 80 -- Railroads and Incrusted Lakes
Chapter 80 -- Railroads and Incrusted Lakes The 1888 map shows the route of the St. Louis and San Francisco Railroad, 8 kilometers north of Newonia. Successfully bypassing the alleged incrusted lake, the track was laid without problem, or so the railway men might have claimed. The skeptic might accuse the railway men of imaginations run amok by what was no more than profound mud, but as we noted early in our journey, were we to dismiss speculation regarding underground waters that seem nonsensical, what a short study ours would be. Scenic Kansas (1935) by Assistant Kansas State Geologist Kenneth Landes, featured several sinkholes among the state's geologic attributes. Kansas has been the scene of a number of sinkings in historic times. In 1897 a sink of 175 feet in diameter formed directly in the path of the cross country trail near Meade. A year later an acre of land in western Pawnee County slumped and took with is the Rozel railroad station. In 1926, a sink formed southeast of Sharon Springs in Wallace County which aroused country- wide interest. Meade Salt Sink, later known as the Great Salt Well, had in fact breached the Jones and Plummer wagon road not in 1897, but 18 years earlier with a 50 to 70-meter diameter crater, 20 meters deep, filled with 7-percent saline water to 5 meters of the top. Cracks 2 to 5 meters deep, 3 to 20 centimeters wide, radiated 40 meters outward. Meade Salt Sink, 1898 or 1899 Subsidence near Sharon Springs on March 9, 1926, created sinkhole 15 meters in diameter.
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