No-name Lake

Status
Established
Year Established
2015

Location

State
Wisconsin
National Forest Regions
Eastern Region (R9)
A view looking across No-Name Lake of a stand of White Pines; 2001 photo by Linda Parker, USDA Forest Service.

 

Potential Research Topics:
Potential research topics include successional changes, habitat characteristics along the gradient from upland to wetland, long-term forest dynamics, bat population, acid bog lake ecology, and amphibians of ponds and lakes.

Ecological and Physical Description

Size
283ac (115ha)
Elevation Range
1,460' (445m) - 1,510' (460m)
Temperature Range
24°F (-4°C) - 58°F (14°C)
Primary Features

No-name Lake Research Natural Area (RNA) has at its center an undeveloped, soft-water seepage lake in a secluded tract of older, second-growth northern hardwood/hemlock forest with a small bog lake, perennial ponds, sedge meadow, and conifer swamp.   The lowland conifer swamps and bog lake are representative of the ecological land type known as Glidden Drumlins. Other forest communities within the RNA include eastern hemlock and northern white cedar of large diameter (over 100 years old) with super-canopy white pine scattered throughout.  Sugar maple, white ash, and basswood dominate the uplands.  Black ash is common in the lowlands and on perched wetlands within the mesic forest.

Annual Precipitation

Annual precipitation averages 32 inches (81 cm), 69% of which falls between April and September. Average seasonal snowfall is 41 inches (105 cm).

Nearest Weather Station

Park Falls DNR Headquarters, station no. 476398. The station is located about 20 mi (32 km) to the southeast of the RNA.

Geology and Soils

Bedrock includes igneous, metamorphic, and volcanic rock that is generally within 5 feet of the land surface. Topography is rolling with drumlin moraines.  Geomorphologic processes include till deposition.
Soils of No-name Lake RNA are well-drained loamy sands and sandy loams in the western portion and moderately well to well drained silt loams in the eastern portion.  Soil series include the Pelissier-Pence sandy loams.  The Pelissier series consists of very deep, excessively drained soils on outwash plains, stream terraces, eskers, kames and end moraines.   The Pence series consists of very deep somewhat excessively drained soils which are shallow to stratified sandy outwash   The bog contains deep, strongly acid soils that are moderately decomposed and very poorly drained.  Organic material is derived largely from sphagnum mosses and herbaceous plants.  The water table is at the surface throughout the year.

Aquatic Features

Water resources include No-name Lake, and extensive wetlands.  No-name Lake has no stream inlet but the outflow during periods of high water is generally to the north into the Chippewa River basin. In places the poorly drained soils support ephemeral as well as permanent ponds. The ground water of some of the wetlands flows outside the RNA into the Brunet River, a high quality trout stream with natural trout reproduction.

Flora and Fauna

Common Plant Species

Common Animal Species

Last updated February 27, 2023