FAQ . . .
Frequently Asked Questions about Lakes
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Do I need a DNR permit to remove the cattails along my lake shore?
The control or removal of emergent aquatic vegetation, such as cattails, bulrushes or wild rice, does require a DNR aquatic plant management permit). The DNR Section of Fisheries regulates the control or removal of aquatic vegetation by physical or chemical means. Permits can be applied for through the DNR Regional Fisheries Office serving the area where your shoreline property is located. They may be contacted at (651) 259-5100 for more information.
Also see the DNR Waters information sheet titled Shoreline Alterations: Lakescaping (1.1 Mb).
What are “environmental” lakes? Are they wild? Are there restrictions on motors or hunting and fishing?
The term “environmental lake” most likely is taken from the Natural Environment lake classification found in Minnesota’s Shoreland Management Program. Many people mistakenly infer that the Natural Environment classification on many of Minnesota’s smaller, shallow lakes means they are wild lakes with limits on motors, hunting or fishing. To a degree, this is true in that Natural Environment is the strictest of the three lake classifications. However, the classification is used to determine lot size, setbacks and, to a certain degree, land uses on the adjacent land. The classification has nothing to do with surface water use of boats or motors, hunting and fishing or fish management. These are governed by other regulations. As the larger, deeper lakes that are more suitable for recreational or general development (the other two lake classifications) become developed, there is growing pressure to develop the smaller, more sensitive natural environment basins. Hence there is no guarantee that the wilderness character that some of these lakes now have will be preserved. It is a growing concern of many local governments, outdoors recreation groups and the DNR that such lakes may require more protection than currently provided in the rules.
The shoreland management rules were established in the early 1970’s and are intended to help govern the orderly development of land adjacent to Minnesota’s many lakes and rivers. The way it works is that DNR established statewide standards and lake/river classifications that local governmental units (counties and municipalities) were then required to incorporate into their land use controls (planning and zoning ordinances). To learn more, click on the Guide for Buying and Managing Shoreland. There you can find information on the lake classification system along with a more complete explanation of the shoreland management program.
How are lakes defined in Minnesota?
A lake is not defined by size or depth as some may suggest. A lake may be defined as an enclosed basin filled or partly filled with water. A lake may have an inlet and/or an outlet stream, or it may be completely enclosed (landlocked). Generally, a lake is an area of open, relatively deep water that is large enough to produce a wave-swept shore. For regulatory purposes, Minnesota has grouped its waters into two categories: public waters and public water wetlands. This makes it easier to determine whether a DNR public waters work permit (available under DNR Waters Forms) is required before changes can be made to the course, current, or cross section of these waters.
The state has an interest in protecting not only the amount of water contained in these lakes, wetlands and streams but also the container that confines these waters (i.e., lakes, wetlands, and streams). The obvious reason for these conservation measures is that these waters provide a vital habitat for fish and wildlife, as well as a place for people to fish, hunt, trap, boat, and swim. However, the most important benefits provided by these waters are less obvious:
- Substantial amounts of water are stored in these areas and it can seep into the ground to recharge ground water aquifers.
- Lakes, wetlands, and streams can store excess water in times of flooding and provide an important reserve of surface water during times of drought. These areas are nature’s water treatment systems. They provide an ideal environment for aquatic vegetation and animal organisms to purify the water we have contaminated with suspended soil (erosion), nutrients (from fertilizers and animal wastes), and other pollutants.
How do I go about naming a lake?
Naming lakes, rivers, streams or other water bodies (natural geographic features) in Minnesota is guided by the statutory process found in Minnesota Statute 83A.04 – 83A.07. The process requires 15 or more registered voters to petition the county board of commissioners in the county where the feature is located for a public hearing concerning a proposed name. If the public hearing is successful, the county board would adopt a resolution in support of the proposed name (or other name if favored by the board as a result of testimony at the hearing) and forward it to the state commissioner of natural resources. The name proposed in the resolution MUST be approved by the commissioner of natural resources to become the official name of the feature in Minnesota. Approved names are subsequently submitted to the United States Board on Geographic Names for federal approval and use.
The process to change a name is the same. However, a name that has existed for 40 years or more may not be changed. Also, the commissioner of natural resources will not approve a name that commemorates, or may be construed to commemorate, living persons. For additional information, please contact Peter.Boulay@state.mn.us; telephone (651) 296-4214.
Also see: Naming Geographic Features
What is a “spring-fed” lake?
To varying degrees many, if not most lakes receive some water from ground water sources or are “spring fed.” When swimming, one might notice colder, localized areas or areas of the lake might remain open along the shoreline during winter. Both are likely due to ground water flowing into the lake. Lakes also lose water to ground water sources. Most lakes have both; some ground water flows into the lake and some lake water flows into the ground water system or aquifer. Variations in precipitation patterns can cause the amount in or out to change significantly. Generally, complex hydrologic computer models including information such as watershed, geology, precipitation, lake level, and ground water level data are used to estimate how much is flowing in or out of the lake.
What is a meandered lake?
A meandered lake is a body of water, except streams, located within the meander lines shown on plats made by the United States General Land Office (Federal Bureau of Land Management). A meander line is a series of courses and distances to delineate the area of a body of water. It is not a boundary line, nor does it convey land ownership information.
What is the definition of public waters?
(See complete legal definition under Public Waters Work Permits Program.) Public waters are all water basins and watercourses that meet the criteria set forth in Minnesota Statutes, Section 103G.005, Subdivision 15 and are designated on the DNR’s Public Waters Inventory Maps.
What is the definition of ordinary high water level (OHWL) and why is it important?
The ordinary high water level (OHWL) is a reference point that defines the DNR’s regulatory authority over development projects that are proposed to alter the course, current, or cross section of public waters and public waters wetlands. For lakes and wetlands, the OHW is the highest water level that has been maintained for a sufficient period of time to leave evidence upon the landscape. The OHWL is commonly that point where the natural vegetation changes from predominately aquatic to predominantly terrestrial. For watercourses, the OHWL is the elevation of the top of the bank of the channel. For reservoirs and flowages, the OHWL is the operating elevation of the normal summer pool. The OHWL is also used by local units of government as a reference point from which to determine structure setbacks from water bodies and watercourses. See also legal definition under Hydrographics Program.
Also see technical paper (TP #11) “Guidelines for Ordinary High Water Level (OHWL) Determinations”. This paper reflects current terminology as well as the DNR Area Hydrologists’ addresses and phone numbers.
Why is the water level on my lake so high or so low? What is the DNR going to do about it?
The DNR does not control the water level elevation of lakes. In general, the water level of a lake is entirely dependent upon the amount of snowfall and precipitation that an area receives, how much of the resultant moisture is contributed by runoff into the lake, how much water is recharged to or discharged from the lake through ground water and how much water evaporates from the lake. In some instances, the water level is controlled by illegal human activity or beaver activity. See also the DNR Lake Level Minnesota Program, for information about lake gauge measurements and lake levels.
What is meant by “lake turnover”? How and why do lakes do this in autumn and spring?
- The key to this question is how water density varies with water temperature. Water is most dense (heaviest) at 39º F (4º C) and as temperature increases or decreases from 39º F, it becomes increasingly less dense (lighter). In summer and winter, lakes are maintained by climate in what is called a stratified condition. Less dense water is at the surface and more dense water is near the bottom.
- During late summer and autumn, air temperatures cool the surface water causing its density to increase. The heavier water sinks, forcing the lighter, less dense water to the surface. This continues until the water temperature at all depths reaches approximately 39º F. Because there is very little difference in density at this stage, the waters are easily mixed by the wind. The sinking action and mixing of the water by the wind results in the exchange of surface and bottom waters which is called “turnover.”
- During spring, the process reverses itself. This time ice melts, and surface waters warm and sink until the water temperature at all depths reaches approximately 39º F. The sinking combined with wind mixing causes spring “turnover.”
- This describes the general principle; however, other factors (including climate and lake depth variations) can cause certain lakes to act differently. A more detailed description of the physical characteristics of lakes, including temporal and density interactions, can be found at the Water on the Web site, sponsored by the University of Minnesota – Duluth and funded by the National Science Foundation.
What can I do to prevent erosion?
Two general methods are available to prevent your lakeshore from eroding: hard armoring and soft armoring. The most common hard-armor technique is riprap, which consists of placing large rocks in the water and up the slope of the eroding shoreline. Riprap is commonly used to control erosion along streambanks and lakeshores where vegetation is not sufficient to prevent erosion caused by high water or wave action. It is expensive to install and is often installed incorrectly. If installed properly, however, riprap normally provides good protection from the impact of waves and ice. Some believe that riprap is overused and unsightly and that Minnesota lakes have lost much of their natural shoreline to riprap.
In contrast to hard-armor techniques, soft-armor methods use organic and inorganic materials combined with plants to create a living barrier of protection. Bioengineering, a soft-armor method, provides erosion control through the use of live vegetation. Bioengineering can be used in addition to or in place of hard armor such as rock riprap. It creates a more natural, environmentally friendly shoreline that includes additional benefits to erosion control, such as habitat enhancement. An excellent source of information on these methods is the DNR publication “Lakescaping For Wildlife and Water Quality” available from the Minnesota’s Bookstore. A DNR public waters work permit (application available under DNR Waters Forms) may be required for both soft and hard armoring methods.
Also see: Shoreline Alteration Information Sheets
What is a Lake Improvement District (LID)?
A Lake Improvement District (LID) is special-purpose district formed around a lake in accordance with Minnesota Statutes, sections 103B.501-103B.581 . A lake improvement district is a local unit of government established by resolution of appropriate county boards and/or city governing bodies, or by the commissioner, for the implementation of defined lake management projects and for the assessment of the costs thereof.
Where can I purchase a lake map? Where can I obtain a printout with information on what kind of fish are in my lake (i.e., lake survey maps)?
What are the DNR Waters permitting requirements for lakefront property?
See the water permits page to learn when you need a permit.
Who Owns the Lake Bed?
Read the article Pardon Me Myth! Who Owns the Lake Bed? by Dave Milles.
More DNR Info . . .
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