Richter Lake

Status
Established
Year Established
2015

Location

State
Wisconsin
National Forest Regions
Eastern Region (R9)
Small ephemeral ponds occur in the low areas in the undulating topography of Richter Lake Hemlocks RNA. 2010 photo by Linda Parker, USDA Forest Service.

Potential Research Topics:
Surveys of ecological information are needed on this RNA including systematic flora and fauna surveys; particularly of herbaceous plants, bats, reptiles and amphibians.  The ice-walled lake plain end moraine glacial features in this area are unique because of its unmodified status.

Ecological and Physical Description

Size
330ac (134ha)
Elevation Range
1,420' (433m) - 1,475' (450m)
Temperature Range
24°F (-4°C) - 59°F (15°C)
Primary Features

Richter Lake Hemlocks Research Natural Area (RNA) is a mosaic of natural plant communities: northern mesic forest, northern wet-mesic forest, northern hardwood swamp, and a collapsed ice-walled lake plain glacial geologic feature.  It contains a microcosm of many of the predominant natural features associated with the Perkinstown End Moraine glacial deposit.  The complex topography within this RNA permits rapid changes in tree cover over short distances promoting a heterogeneous forest of many types including old-growth pockets of eastern hemlock (Tsuga canadensis).  Two rare plants, little goblin moonwort (Botrychium mormo) and autumn coralroot (Corallorhiza odontorhiza), occur here. 

Annual Precipitation

Annual precipitation averages 33 inches (84 cm), 71% of which falls between April and September.   Average seasonal snowfall is 40 inches (102 cm).

Nearest Weather Station

Medford 1 SW (station no. 475255) located about 12 mi (19 km) to the southeast of the RNA.

Geology and Soils

Bedrock of the Perkinstown End Moraine includes igneous, metamorphic, and volcanic rock. Bedrock is between 100 feet and 50 feet (30 - 15 m) of the land surface. Geomorphologic processes include till and lake deposition.
The soils of this RNA are well to moderately well drained sandy loams and silt loams. Moisture regime is dry-mesic to mesic to wet-mesic. Nutrient status is medium to rich. Sandy loam, loam, and fine sandy loam occur on 5-30% slopes. These are steep rolling soils over a loamy sand glacial till and outwash complex. These soils formed within glacial till areas but show evidence of outwash influence and occupy the backslope positions of well drained loamy pitted outwash hills. On the shoulders and backslope of end moraine hills are steep, hummocky soils that are moderately well-drained. Surface textures are sandy loam, fine sandy loam, loam, and occasionally silt loam on top of ice-walled lake plain features. These soils are generally found on 10-30% slopes.

Aquatic Features

For its relatively small size, the RNA contains numerous perennial and ephemeral woodland ponds.  The forested areas occur as low islands within a matrix of mixed conifer-hardwood swamp drained by black ash-dominated drainages. An ephemeral stream drains a marshy wetland on the southern edge.

Flora and Fauna

Common Plant Species

Common Animal Species

Last updated February 27, 2023