![]() ![]() Along the southern border of the county on the south side of Chikaskia River is another ridge, which rises abruptly from the valley and reaches a crest about on the county line. In the northeastern corner of the county a poorly defined ridge forms the divide between Smoots Creek and North Fork of Ninnescah River. The intervening terrain, ranging in width from 10 to 13 miles, forms a gently sloping divide across the county, which is dissected by many short tributary creeks near the rivers.Ī second ridge extends southeastward from the northwestern part of the county to a narrow termination near the town of Murdock and forms the divide between South Fork of Ninnescah River and Smoots Creek, one of its major tributaries. Topographic relief in the county results from dissection by South Fork of Ninnescah River, which flows eastward across the northern third of the county, and by Chikaskia River, which parallels South Fork in the southern third of the county. ![]() The lowest points in the county are where South Fork of Ninnescah River and Chikaskia River leave the county in the east-central and southeastern parts of the county and are about 1,340 feet above sea level.įigure 3-Map of Kansas showing physiographic divisions. The altitude in these areas is about 1,800 feet above sea level. The highest points in the county are at the center of the western border and in the sand-dune area in the southwest corner. The general slope of the land surface is toward the southeast and averages 10 feet per mile. The eastern half is within the Red Hills division of the Dissected High Plains (Fig. Approximately the western half is in the High Plains and Dissected High Plains sections. Kingman County is at the southeast edge of the Kansas portion of the Great Plains physiographic province as designated by Schoewe (1949).
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