The-Barbee-Lakes-Diagnostic-Study
THE BARBEE LAKES DIAGNOSTIC STUDY KOSCIUSKO COUNTY, INDIANA INTRODUCTION The Barbee Lakes chain is composed of seven interconnected, natural lakes situated west of North Webster, Indiana (Figure 1). Specifically, the lakes are located in Sections 20, 21, 26, 27, 28, 29, 33, and 34, Township 33 North, Range 7 East, in Kosciusko County. The lakes’ watershed stretches southeast into Whitley County, encompassing approximately 33,150 acres (13,420 ha) or 52 square miles (133 km2). Water from the lakes discharge to Lake Tippecanoe. From Lake Tippecanoe, water drains through the Tippecanoe River to the Wabash River, eventually reaching the Ohio River in southwestern Indiana. The Barbee Lakes and their watershed formed during the most recent glacial retreat of the Pleistocene era. The advance and retreat of the Saginaw Lobe of a later Wisconsian age glacier as well as the deposits left by the lobe shaped much of the landscape found in northeast Indiana (Homoya et al., 1985). In Whitley and Kosciusko counties, the receding glacier left a nearly level topography dotted with a network of lakes, wetlands and drainages. The Barbee Lakes are located in the central portion of the Northern Lakes Natural Area (Homoya et al., 1985). The Northern Lakes Natural Area covers most of northeastern Indiana where the majority of the state’s natural lakes are located. Natural communities found in the Northern Lakes Natural Area prior to European settlement included bogs, fens, marshes, prairies, sedge meadows, swamps, seep springs, lakes, and deciduous forests. Historically, much of the Barbee Lakes watershed was likely swamp habitat. Upland areas were likely forested with oak and hickory species.
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