Bear Creek

Status
Established
Year Established
2014

Location

State
Wisconsin
National Forest Regions
Eastern Region (R9)
The warm, slow-moving water of Bear Creek is bordered by sedge meadow and alder thicket. 1997 USDA Forest Service Chequamegon-Nicolet National Forest photo.

Potential Research Topics
The large size of this site and intact gradient through various plant communities make it ideal for research in many aspects of forest ecology. In light of global climate change, its position on the edge of the climatic Tension Zone in Wisconsin makes it a valuable location to study forest adaptation to temperature and moisture changes. The presence of large, old trees allows for study of historical climate patterns on forest growth.
A small geologic ice-walled lake plain feature (an area of recessional moraine with an unusually rich species composition) with intact forest cover is a unique element for study as most of these elsewhere have been converted to agriculture.

Ecological and Physical Description

Size
1,034ac (418ha)
Elevation Range
1,290' (393m) - 1,375' (419m)
Temperature Range
24°F (-4°C) - 58°F (14°C)
Primary Features

Bear Creek contains a mosaic of high-quality community types plus a remnant old-growth white pine (Pinus strobus) forest. The site contains some of the oldest eastern hemlock (Tsuga canadensis)-hardwood stands remaining on the Medford-Park Falls District of the Chequamegon-Nicolet National Forest. Also significant is a two-mile (3 km) stretch of Bear Creek and associated high quality wetlands, contained within the RNA.  Floral diversity is high and includes several uncommon orchid species. Red-shouldered hawks (Buteo lineatus), a state-threatened species, have been seen within Bear Creek RNA and have been known to nest in the surrounding area.

Annual Precipitation

Annual precipitation averages 33 inches (84 cm), 71% of which falls between April and September. Average seasonal snowfall is 56.9 inches (144 cm).

Nearest Weather Station

Jump River 1 ESE (station no. 474080) is about 4 mi (6.4 km) north of the RNA.

Geology and Soils

The ice-walled lake plain glacial feature found on the eastern side of the RNA was formed as the glacier retreated. A wall of stagnant ice trapped the outwash sediments, creating a plateau of debris that was later covered with fine wind-borne loess deposits. Carbonates make up the bedrock of this LTA, which is between 100 feet and 50 feet of the land surface. Geomorphologic processes are till and glacial meltwater deposition. Land surface is till plain with outwash terraces.
The soils of Bear Creek RNA fall into the Freer-Almena-Auburndale Series. They are generally moderately well to poorly drained loamy and silty soils with a silt loam surface over non-calcareous sandy loam dense till. Very poorly drained nonacid organic soils are also present. Nutrient status is medium to rich.

Aquatic Features

Located within the Yellow River watershed, Bear Creek is a warm-water stream that flows south into the Chequamegon Waters Impoundment. This creek is shallow and slow-moving with water slightly stained with tannic acid from the swamp origins.   Spring rains swell the creek in April and May but in late August, it can be nearly dry in some places making it essentially non-navigable.

Flora and Fauna

Common Plant Species

Common Animal Species

Last updated February 23, 2023