A REEXAMINATION OF MELTWATER ROUTING IN CENTRAL NEW YORK
Geographic information system was used to ascertain the discharge pattern and direction of glacial meltwater as well as former glacial lake shorelines across the state. Topography from 10 meter digital elevations models as well as LiDAR, where available, was used to establish drainage routes through these channels as well as a reconstruction of the shoreline of glacial Lake Iroquois in central New York. Stream profiles of the channels provide insight to the relative timing of the drainage as well as the drainage direction. The shoreline of glacial Lake Iroquois was recreated by using tilted water planes at various slopes to match observed shoreline features and field observations with previous thresholds and drainages.
The profiling of the large channels has proved problematic on a regional scale as not only does the morphology of the channels change across central New York but the downward slope of the channel is not consistent with the eastern outlets proposed. Compounding this issue is the fact that there is an inability to match water planes and shoreline features of glacial Lake Iroquois in central New York such that the lake drains to the east.