Waterfowl Identification Guide Comprehensive Conservation Plan Phone: 218-8474431 |
Geographic/Ecosystem Setting
Three landscapes come together in Minnesota: prairies, deciduous woods, and coniferous forests of the north. This variation in landscape is caused by changes in climate and precipitation from north to south and is reflected in the wide diversity of plants and animals inhabiting the state (Wendt and Coffin 1988; Hargrave 1993; Aaseng, et al. 1993). The Districts own land within all three habitat types and all have changed dramatically since settlement; none more than the prairie landscape (Figure 1).
Prairie Grasslands
At one time, the western edge of Minnesota was continuous prairie and scattered woodlands dotted with small wetlands, known as potholes. Snow melt and spring rains were contained in these small wetlands and released slowly into surrounding streams. The wetlands acted like a natural flood control system. All of this has changed since settlement. Now, only 150,000 acres of native prairie remain out of an original 18 million (Noss, et al. 1995). In some areas, virtually all of the potholes have been drained. Remnants of prairie and their associated wetlands are scattered and rare. They form the last refuge for many species of prairie plants and wildlife.
Deciduous Woods
The deciduous forest of Minnesota extends from the northern aspen parkland to maple basswood forests of the southeast. The term "deciduous" refers to trees that lose their leaves in the fall. There are many forest communities within this landscape. The northern aspen parkland is typical of a more Canadian landscape, with open understory, wet meadows, aspen, willow, and alder thickets. The communities include wild flowers like the northern gentian and prairie-fringed orchid, wildlife such as the moose, sandhill crane, sharp-tailed grouse, black-billed magpie, and yellow rail. Further south, the deciduous forest changes to one dominated by maple and basswood and scattered oak savannahs. Birds of these hardwood forests include the tufted titmouse, scarlet tanager, eastern screech owl, broad-winged hawk, barred owl, redeyed vireo, and wood thrush to name just a few. Wild flowers in the spring are a special feature of these woods including trillium, hepatica, blood root, trout lily, Dutchman's breeches, and spring beauty (Moyle and Moyle 1977; Henderson and Lambrecht 1997).
Figure 1: Minnesota Wetland Management Districts Ecosystems
Coniferous Forest
The coniferous forests dominate the northeastern portion of Minnesota. They are characterized by red and white pines, balsam-fir, spruce, and white cedar mixed with other deciduous species. While the coniferous forests dominate Minnesota landscapes, the Districts own very little in this landscape and have focused acquisition on the prairie grasslands which are more productive for waterfowl.
Climate
The climate of Minnesota is seasonal and highly variable. Average annual precipitation ranges from 20 inches in the northern aspen parklands to 32 inches in the southwestern prairie coteau. Within the eastern Great Plains, precipitation falls during two peak periods, one in early summer and a less pronounced peak in September. Average maximum annual temperature ranges from 50 degrees Fahrenheit in the northern aspen parklands to 58 degrees Fahrenheit in the prairie coteau. Average minimum annual temperature ranges from 23 degrees F in the aspen parklands to 36 degrees F in the prairie coteau. The growing season ranges from 125 days in the aspen parklands to 180 days in the prairie coteau (Hargrave 1993; Ostlie et al. 1996).
Hydrology
Conversion of the prairie to agriculture and the general development of the area over the past 130 years have greatly changed the region's hydrology. The Districts contain five major watersheds: the Red, the Upper Mississippi, the Minnesota, the Missouri, the Cedar and Des Moines Rivers. Of these, the Red, Minnesota, and Des Moines are clearly the most important hydrologically and culturally in terms of water flow, impacts to land use, and associated water resources. The Minnesota River is considered the state's most polluted river. The Red River watershed has been degraded by dam construction, agricultural practices, channelization, and loss of riparian vegetation.
The Red River is the only major American river that drains northward into Hudson Bay. Total drainage area in the U.S. is 39,200 square miles, of which 17,806 are in Minnesota. Due to regional patterns in precipitation, evapotranspiration, soils, and topography, the Red receives most of its flow from its eastern tributaries. Ten of these tributaries traverse the Districts.
Many rivers in the Districts have been channelized in the downstream reaches to improve agricultural drainage. Most of the small wetlands that once held spring melts have been drained for agriculture through ditches or subsurface tile systems. Partially as a result of this facilitated drainage, damaging summer floods are becoming more common.
River hydrology has been further altered through the construction of approximately 270 flood control structures within the Minnesota basin of the Red River. Despite these flood control projects, the Red remains a flood-prone system due to heavy spring snow melt, the flatness of the area, and snow/ice melting in the upstream area of the basin before that in the downstream areas.
The Roseau, Red Lake, Wild Rice, and Buffalo rivers account for three-fourths of the flood damage on the Minnesota tributaries. The Minnesota River drains an area of 15,500 square miles within the District area. The Minnesota River begins in Browns Valley, where it is separated from the watershed of the Red River (Lake Traverse) by the Big Stone Moraine. As it flows toward its meeting with the Mississippi, the Minnesota River is impeded by four flood control reservoirs located at Big Stone, Big Stone/Whetstone, Marsh Lake, and Lac Qui Parle. Two smaller dams near Granite Falls slow the flow, but do not impound any water within the floodplain. One small hydroelectric dam operates near Mankato on the Blue Earth River. Flooding along the Minnesota is common within the floodplain, but does not have the same cultural or ecological impacts as on the Red River because the steep slopes of the Minnesota contain the river.
Southwestern Minnesota differs dramatically from the flat topography to the north and east. The Coteau des Prairies region grades from gently undulating to steeply rolling and hilly. These glacial moraines and ridges are well drained and have few depressions. This area flows mostly southwest into the Missouri River. The outer edges of the Coteau are less well drained and contain numerous wetlands and lakes. The Big and Little Sioux rivers are the two largest rivers in this area. Both flow to the southwest and into Iowa.
Geology
The area has a varied geological history but throughout the region, the departure of the last glacier, The Wisconsin, is still evident upon the land. The retreating glacier left behind gently rolling hills of gravel deposits with many scattered potholes, remnants left by melting glacial ice. In relative geologic time, the rivers that drain this land are new and inefficient (Ojakangas and Matsch 1982).
The southwest corner of Minnesota escaped the Wisconsin glaciation and features more bedrock exposures because that area escaped a blanket of glacial till or drift. Big Stone District is named after some of the rocky features of the bedrock exposure. Rivers and streams in this area are better developed, resulting in more efficient drainage systems.
Thousands of natural basins were left in the wake of thawing ice. Glacial lakes, the largest of these being Lake Agassiz, left behind a series of beaches and as they overflowed, they cut huge river channels. Lake Agassiz created a moraine at Browns Valley that spilled over to become the glacial River Warren, later named the Minnesota River. The water volume of the Minnesota is a fraction of the River Warren, which flowed through its broad river valley with high stream terraces, dwarfing today's river. The Minnesota has eroded deeply into the glacial sediment and has exposed some of the world's oldest rocks along its narrow valley.
Wind-blown loess was also a major influence in the soils of Minnesota, especially in southwest Minnesota. The disintegration of the Wisconsin Glacier left a distinctive, fine-textured till containing a high volume of Paleozoic limestone and Cretaceous shale fragments. Combined with the loess swept by surface winds, it is the parent material for most of today's prairie soils of western and southern Minnesota.
Note: The above information is an excerpt taken from the Detroit Lakes WMD Comprehensive Conservation Plan (CCP). The above cited references and other useful information can be found by reviewing the full plan at the following link: Detroit Lakes CCP.
