When precipitation (rain or snow) falls on the land, it absorbs into the ground and becomes groundwater, or it washes over the land as “runoff.” As runoff moves over the land, it can pick up pollutants that can be transported to the lake. As development in a watershed increases, there is often a concurrent increase in the amount of runoff. Lake water quality is often a reflection of land use (i.e., urban, forested, agricultural, wetland) in the watershed. Lakes in highly developed watersheds tend to have poorer water quality than lakes in less developed watersheds.
Water draining from the upper portions of the Silver Lake watershed (i.e., the extended watershed) flows through Lake Holiday and Upper Silver Lake before discharging to Silver Lake which, in turn, flows to Silver Creek and Lake Michigan. There is an approximate 80-foot elevation difference between Wyckoff Lake in the upper portion of Silver Lake’s extended watershed and Silver Lake, and an approximate 6-foot elevation difference between Silver Lake and Lake Michigan. The levels of Lake Holiday, Upper Silver and Silver Lakes are controlled by dams, and Lake Holiday and Silver Lake have court-ordered lake levels.
Land cover data derived from aerial photography (Michigan Resource Information System, MIRIS, 1978) is available for the entire state through the Michigan Geographic Data Library. With this data set, various land use classifications can be combined to show the generalized land cover in a watershed. The historical land cover data can then be compared to more recent aerial photography to evaluate changes in land cover over time. In the Silver Lake watershed about half of the land is forested and wetland, about one-third is agricultural and the remainder is urbanized, with most of the development concentrated around the lakes in the watershed. Most of the agricultural land in the watershed is located within the extended watershed and does not drain directly to Silver Lake.
One type of land cover that is often given special attention is wetland. In addition to fish and wildlife habitat, wetlands help filter pollutants, minimize flood potential and perform other important functions. Wetland inventory maps are available for much of the state through the Michigan Geographic Data Library. These maps were created by combining information from the U.S. Fish and Wildlife Service National Wetland Inventory, MIRIS land cover, and hydric soils data from the U.S Department of Agriculture Natural Resources Conservation Service. These maps can be used to identify the generalized location of wetlands throughout a watershed. Over 2,000 acres of the Silver Lake watershed is classified as wetland.
Hydrologic soil classifications can be useful in evaluating runoff potential in a watershed. Soils that are predominately sandy tend to have a high infiltration rate and low runoff potential. By contrast, loam and clay soils tend to have a low infiltration rate and a higher runoff potential. Most of the soils in the Silver Lake watershed are sandy and have a high infiltration rate and low runoff potential.
Generalized mapping of groundwater elevations in the state has been compiled by the Michigan Department of Environmental Quality in collaboration with the U.S. Geological Survey, Michigan State University and others. Groundwater flow within Silver Lake’s extended watershed is intercepted by the Golden Drainage Ditch, while much of the groundwater in the immediate watershed flows directly toward the lake.
A watershed is the land area surrounding a lake from which water drains to the lake. The imaginary line that defines a watershed is the watershed boundary, or is sometimes called the drainage divide. A watershed can be big or small, and the size and shape depends on the “lay of the land” and the number and length of tributary streams.
The information below was derived from an article entitled Mapping and Understanding Your Lake’s Watershed. Click here for a print version of this article.