Charlotte River (Michigan)


The Charlotte River is a tributary of the St. Marys River in the state of Michigan in the United States. The stream is long and drains an area of on the eastern Upper Peninsula. Via the St. Marys River, it is part of the watershed of Lake Huron. Via Lake Huron and the Great Lakes system, it is part of the larger watershed of the St. Lawrence River.

Course

The river's entire length and watershed are in eastern Chippewa County. As defined by the United States Geological Survey's National Hydrography Dataset, the river begins in southeastern Dafter Township, approximately south-southeast of the unincorporated community of Dafter. It flows for most of its length in Bruce Township, initially northeastward before turning southeastward at the unincorporated locality of Rosedale. It flows into the West Neebish Channel of the St. Marys River, opposite the northern end of Neebish Island and approximately southeast of Sault Ste. Marie, Michigan.
Some maps show the river's course upstream of Rosedale as the South Branch Charlotte River, with the name "Charlotte River" upstream of this point assigned to a southeastward flowing tributary. In the National Hydrography Dataset, this tributary appears only as an unnamed stream. "South Branch Charlotte River" is also listed in the Geographic Names Information System as a variant name.
The National Hydrography Dataset lists one named tributary in the Charlotte River watershed, Spring Creek, a right tributary approximately long.
Near its mouth the river flows through Michigan State University's Dunbar Forest Experiment Station, an off-campus forest management research area.

Watershed characteristics

The Charlotte River watershed consists of two HUC-12 subwatersheds, as defined by the United States Geological Survey:
NameHUC-12 codeArea
Headwaters Charlotte River040700010203
Charlotte River040700010204

In addition to Dafter and Bruce townships, the Charlotte River also drains a small portion of Soo Township. The watershed is located in a predominantly rural region, much of which has been drained for agriculture, logging, and development. Soils in the region are primarily poorly drained clays over limestone and dolomite bedrock. On average, the region receives approximately of precipitation annually, and there is usually heavy snow cover in the winter. Runoff from artesian wells contributes to the turbidity that is typical of the region's streams.
According to a 2012 report prepared for the United States Environmental Protection Agency and the Michigan Department of Environmental Quality, the watershed had an estimated population of 3,451 as of the 2010 U.S. Census. There were an estimated 1,562 households, all of which were serviced by onsite sanitary disposal systems. Land use in the Charlotte River watershed was reported as follows:
Land usePercentageArea
Forests27%
Wetlands25%
Cropland24%
Pasture18%
Low-intensity development and open space3%
Grassland3%
Bare land0.4%
High- and medium-intensity development0.4%
Open water0.08%