CHARACTERIZATION OF WETLAND SOIL AND SEDIMENTS AT STARLING NATURE SANCTUARY, MARION COUNTY, INDIANA
The Fishback Creek valley is incised through Wisconsinan-aged glacial deposits and into Illinoian-aged glacial deposits, both of which are primarily till. The floodplain deposits lie on the eroded Illinoian till and consist of a gravel lag layer overlain by sandy alluvium with a cap of silt and clay from overbank flood deposits and colluvial slopewash. The upper 40 cm of the deposits show evidence of 19th century agricultural use.
Soil characterization was accomplished by examination and description of soil cores. Correlation was accomplished by using multiple transects of soil cores. Aerial photography was used to plan locations of wells and cores, determine locations of agricultural tiles, and determine the current drainage pattern. Soil and sediment cores were used to characterize the stratigraphic and hydrogeologic setting of the sanctuary. Monitoring wells were installed to determine the hydrologic regime and groundwater quality of the sanctuary. Data regarding the location of groundwater seeps, monitoring wells, and agricultural tiles as well as the boundaries of vegetation types and standing water at various hydroperiods were collected using survey-grade GPS for later input and analysis in a GIS