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Northern Research Station

Big Lake-Seven Beaver

Status
Established
Year Established
2024

Location

State
Minnesota
Lake shore studded with rocks
Photo Credit
Courtesy photo by Ethan Perry, Minnesota Department of Natural Resources.

Inland strand beach on the shore of Seven Beaver Lake.

The Big Lake-Seven Beaver RNA on the Superior National Forest protects part of the largest, most complex peatland in the Northern Superior Uplands Section, and part of the largest unfragmented patch of mature upland forest in Minnesota outside of the Boundary Waters Canoe Area Wilderness. These plant communities still resemble the presettlement vegetation of the area described in the 1882 Public Land Survey. The lack of roads, absence of recent large-scale logging, and large size of the RNA allow for natural functioning of ecological processes, supporting an array of plants and animals found in these ecosystems.

Ecological and Physical Description

Size
5,518ac (2,233ha)
Elevation Range
1,670' (509m) - 1,752' (534m)
Temperature Range
-1°F (-18°C) - 75°F (24°C)
Primary Features

Ecological Classification & Inventory

  • Sections:  Mixed Forest Province, Northern Superior Uplands Section
  • Subsections:  Laurentian Uplands Subsection (212Le)
  • Landtype Associations:  Seven Beaver Peatland (212Le08), with the western end in the Big-Bird Lake Moraine LTA (212Le11)
Annual Precipitation

Annual precipitation averages 28.7 inches (73 cm); Average seasonal snowfall is 65.1 inches (165.4 cm).

Nearest Weather Station

Brimson (station ID number: GHCND: USC00210989, latitude 47.25°, longitude -91.86°). The station is about 18 mi (29 km) south of the RNA.

Geology and Soils

The Big Lake-Seven Beaver RNA is located in the Superior Uplands physiographic province which is actually the southernmost lobe of the Laurentian Upland Province—an important part of the Canadian Shield which forms part of the North American Craton—the extremely stable part of the North American continent.  Within the boundaries of the RNA, there are four distinct bedrock lithologies:  an anorthositic intrusion, a troctolitic western margin intrusion, gabbro of the Greenwood Lake Intrusion, and troctolites of the South Kawishiwi Intrusion.

Soils are characterized by predominantly flat to concave, acidic, very deep, organic deposits formed in Rainy lobe ground moraine depressions in central and eastern portions of the RNA. A carpet of sphagnum moss covers the upper mantle of the deposit and usually thickens towards the center of the RNA. Acidity tends to lessen with depth, ranging from 3.5 to 4.5 within the sphagnum mantle and from 4.5 to 5.5 in the lower tiers (USDA 2022). These very poorly drained organic soils (with water tables at or near the soil surface for much of the year), fall primarily within the Greenwood series, associated with vast expanses of lowland black spruce-dominated peatlands, and linear map units of the mucky Bowstring series, primarily alder swamps and wet meadows north of Big Lake and along flood prone areas of the North River (NRCS 2022).

Aquatic Features

Seven Beaver Lake borders a portion of the southeast portion of the RNA and is a large, shallow, undeveloped lake, its shoreline primarily open shrub and graminoid dominated wetlands. Wild rice grows sparsely throughout much of the lake, including the mouth of the North River. Big Lake is deeper with a densely forested shoreline. Big Lake borders the western portion of the RNA with forested uplands that include vernal pools.

The North River and its floodplain dominate the eastern portion of the RNA and is part of the uppermost portion of the St. Louis River. The North River, for most of its length, is only a few yards wide, expanding to 30 yards at the mouth (Fedora 2005). Its floodplain is dominated by extensive open rich fens. The corridor supports extensive populations of two rare plant species.

Flora and Fauna

Common Plant Species

Common Animal Species

Last updated August 21, 2024