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Longitudinal Profile for Kalamazoo River Reference Reach upstream of Plainwell, Michigan, 2021

Dates

Publication Date
Date Collected
2021-10-20

Citation

Vaughan, A.A., Fitzpatrick, F.A., and Strange, J.M., 2023, River Morphology Reference Reach Data for the Kalamazoo River Basin, Michigan Area of Concern: U.S. Geological Survey data release, https://doi.org/10.5066/P96JBHF4.

Summary

This dataset is a longitudinal profile of the river bed and water surface along the thalweg of a an approximately 500 meter (m) reach of the Kalamazoo River upstream of Plainwell, Michigan (MI). The bed profile was derived from a digital elevation model (DEM) comprising topographic and bathymetric data for the Plainwell reach. Bathymetric data in the river channel were collected in October, 2021 with a single beam sonar and Acoustic Current Doppler Profiler (ADCP) operated along two longitudinal transects and 48 cross-sectional transects, respectively. River bank topographic data were collected with a backpack-mounted terrestrial lidar unit concurrently with the bathymetric data. The water surface profile was developed from water surface [...]

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Attached Files

Click on title to download individual files attached to this item.

LongProfile_Thalweg.csv 29.32 KB text/csv
LongProfile_Thalweg.xlsx 58.53 KB application/vnd.openxmlformats-officedocument.spreadsheetml.sheet
Shapefile: Thalweg.zip
Thalweg.cpg 5 Bytes
Thalweg.dbf 122 Bytes
Thalweg.prj 434 Bytes
Thalweg.sbn 132 Bytes
Thalweg.sbx 116 Bytes
Thalweg.shp 11.18 KB
Thalweg.shx 108 Bytes

Purpose

Bathymetric and topographic elevation data were collected to characterize the geometry and geomorphology of a reference reach that is representative of less-disturbed conditions in the Plainwell-Allegan stretch of the Kalamazoo River. The goal of the reference reach analysis is to inform river restoration designs and evaluations associated with dam removal projects by developing channel criteria that meet stakeholders' priorities for hydrologic connectivity, channel stability, and fish passage within the river/floodplain system. The longitudinal profile was used to compute an average slope for the reach. Channel slope is an important boundary condition and control on hydraulic and sediment transport processes in the river system. It is therefore a key consideration for determining applicability of the data from this reference reach to a particular target restoration reach.

Additional Information

Shapefile Extension

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