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Whitbeck, R. H., 1871-1939 (Ray Hughes) / The geography of the Fox-Winnebago valley
(1915)
Chapter III. Peculiarities of the fox river, pp. 13-23
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GEOGRAPHY OF FOX-WINNEBAGO VALLEY could scarcely have been the present one. The Wolf River now heads in Forest County and flows a hundred miles south to its present junction with the Fox, a few miles west of Oshkosh, and then its waters reverse their direction and flow 125 miles north- ward from Oshkosh to the foot of Green Bay before they reach Lake Michigan. This is certainly an unusual procedure. (See plate IV.) THE UPPER Fox RIVER The natural course of this part of the river has been so interfered with by glacial deposits that the present course bears little resemblance to the original one. At present the river winds for 107 miles with a sluggish flow through a maze of marshes and lakes, with an average fall of only 4 inches to the mile. Near Portage both the Wisconsin River and the Upper Fox flow in horse-shoe curves and come so close together (about a mile and a quarter) that at times of very high floods the Wisconsin over- flows into the Fox. A canal now connects the rivers and between Portage and Lake Winnebago nine locks render this part of the Fox navigable, but it has not been used to any large extent. The principal tributary of the Fox is the Wolf, a larger river than the Upper Fox. In the logging days this river and its branches were used to an enormous extent in driving logs to the mills, expecially to those at Oshkosh. At one time there were 43 dams on the upper Wolf and its tributaries, built to facilitate the log-driving operations. An impressive illustration of the way in which waterpower aids in building up cities is seen by comparing the upper and lower portions of the Fox. More manufacturing is done at any one of several rapids on the Lower Fox than is done on the entire 107 miles of the upper river; Berlin, with 4700 population, is the only city on this portion of the river, while there are 6 cities all larger than Berlin, in the 35 miles of the Lower Fox. LAKE WINNEBAGO PAST AND PRESENT This lake is unusual in two respects: (1) It is one of the largest of the glacial lakes entirely within the limits of one state; it is 28 miles long and 10.4 miles broad in the widest part, and covers an area of about 215 square miles.* (2) It is remarkably * The extreme shallowness of Lake Winnebago may e illustrated thus: take a sheet of paper so thin that a pile of 350 sheets is one inch high; cut out an oval shaped piece 8 inches wide and 21 inches long; this piece of paper will represent correctly the proportional length breadth, and thickness of the sheet of water which forms Lake Winnebago. I In a 14
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