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Channel Hydrogeomorphic Units 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 map of hydrogeomorphic units (HGUs) for an approximately 500 meter (m) reach of the Kalamazoo River upstream of Plainwell, Michigan (MI). HGUs are the building blocks of the riverscape, including, for example, bars, banks, riffles, and pools. The HGUs were mapped with the automated Geomorphic Unit Tool (GUT; Bangen et al., 2017; Wheaton et al., 2015) run on a digital elevation model (DEM) comprising topographic and bathymetric data for the Plainwell reach, which was developed from elevation data collected by several different methods. Bathymetric data in the river channel were collected in October, 2021 with a single beam sonar and Acoustic Current Doppler Profiler operated along two longitudinal transects and 48 [...]

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Shapefile: Plainwell_GUT_Tier3_InChannel_subGU.zip
Plainwell_GUT_Tier3_InChannel_subGU.cpg 5 Bytes
Plainwell_GUT_Tier3_InChannel_subGU.dbf 223.19 KB
Plainwell_GUT_Tier3_InChannel_subGU.prj 424 Bytes
Plainwell_GUT_Tier3_InChannel_subGU.sbn 2.97 KB
Plainwell_GUT_Tier3_InChannel_subGU.sbx 348 Bytes
Plainwell_GUT_Tier3_InChannel_subGU.shp 168.49 KB
Plainwell_GUT_Tier3_InChannel_subGU.shp.xml 19.12 KB
Plainwell_GUT_Tier3_InChannel_subGU.shx 2.32 KB

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. These mapped HGUs may be used to characterize the spatial scale, organization, and frequency of geomorphic forms in the reference reach, and thereby may be useful as a guide for the design and review of channel restoration plans. Because HGUs are formed and reworked by a specific set of processes, their identification and classification provide a basis for interpreting the origin of landforms, potential processes affecting them (erosional or depositional), and their sensitivity to and expected type of change.

Additional Information

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