Generation of Watershed Basins for Prominent Sinking Streams in the Michigan Upper-Peninsula
University
Shawnee State University
Major
Geology
Presentation Types
Oral Presentation
Keywords:
Geology, Karst, Hydrology, Michigan
Abstract
The Hiawatha National Forest in the Michigan Upper-Peninsula is a karst-rich landscape that has many sinkholes, sinking streams, and springs. Pleistocene glaciations flattened the region, initiating a deranged drainage pattern that drives the dissolution of Silurian carbonates. The focus of this project is to generate watershed basins for prominent sinking streams in the region. Three watershed basins were generated in ArcGIS: Petey’s sink, Pontchartrain Shores sink, and a sink on FS 3114. The understanding of hydrologic behavior on the Michigan Upper-Peninsula is important as it assists us in better understanding how groundwater interacts with surface water in a karstic landscape.
Human Subjects
no
Faculty Mentor Name
Erik Larson
Faculty Mentor Title
Assistant Professor of Geology
Faculty Mentor Academic Department
Natural Sciences
Recommended Citation
Fitzpatrick, David, "Generation of Watershed Basins for Prominent Sinking Streams in the Michigan Upper-Peninsula" (2020). Celebration of Scholarship. 1.
https://digitalcommons.shawnee.edu/cos/2020/abstracts/1
Generation of Watershed Basins for Prominent Sinking Streams in the Michigan Upper-Peninsula
The Hiawatha National Forest in the Michigan Upper-Peninsula is a karst-rich landscape that has many sinkholes, sinking streams, and springs. Pleistocene glaciations flattened the region, initiating a deranged drainage pattern that drives the dissolution of Silurian carbonates. The focus of this project is to generate watershed basins for prominent sinking streams in the region. Three watershed basins were generated in ArcGIS: Petey’s sink, Pontchartrain Shores sink, and a sink on FS 3114. The understanding of hydrologic behavior on the Michigan Upper-Peninsula is important as it assists us in better understanding how groundwater interacts with surface water in a karstic landscape.