Water-year[B]Average flowMaximumMinimum
1951 8,290 410,000 124.0
1952 2,021 20,500 20.0
1953 173 4,110 .3
1954 430 27,900 .1
1955 645 18,600 0
1956 180 6,170 0
1957 1,774 25,000 0
1958 3,092 27,200 78.0
1959 1,609 22,600 139.0

Table 3. Stream-flow in Cubic Feet per Second, Marais des Cygnes River Near Ottawa, Kansas. Drainage Area: 1,250 Square Miles.

Water-yearAverage flowMaximumMinimum
1951 2,113 142,000 25.0
1952 542 12,000 .2
1953 36.5 2,690 .2
1954 73.6 5,660 .5
1955 75.7 5,240 .7
1956 26 1,590 .7
1957 442 11,200 .7
1958 775 9,130 5.6

Table 4. Stream-flow in Cubic Feet per Second, Marais des Cygnes River at Trading Post, Kansas. Drainage Area: 2,880 Square Miles.

Water-yearAverage flowMaximumMinimum
1951 5,489 148,000 36.0
1952 1,750 20,400 3.0
1953 261 7,590 0
1954 334 12,500 0
1955 786 16,100 .2
1956 202 10,000 0
1957 871 14,700 0
1958 2,453 20,400 120.0
[C]1959 750 10,900 3.4

DESCRIPTION OF NEOSHO RIVER

The Neosho River, a tributary of Arkansas River, rises in the Flint Hills of Morris and southwestern Wabaunsee counties and flows southeast for 281 miles in Kansas, leaving the state in the extreme southeast corner (Fig. 1). With its tributaries (including Cottonwood and Spring rivers) the Neosho drains 6,285 square miles in Kansas and enters the Arkansas River near Muskogee, Oklahoma (Schoewe, 1951:299). Upstream from its confluence with Cottonwood River, the Neosho River has an average gradient of 15 feet per mile. The gradient lessens rapidly below the mouth of the Cottonwood, averaging 1.35 feet per mile downstream to the State line (Anonymous, 1947:12). The banks of the meandering, well-defined channel vary from 15 to 50 feet in height and support a deciduous fringe-forest. The spelling of the name originally was "Neozho," an Osage Indian word signifying "clear water" (Mead, 1903:216).