Camp Nine Pines

Status
Established
Year Established
2014

Location

State
Wisconsin
National Forest Regions
Eastern Region (R9)
An area of pine forest following a storm and subsequent salvage logging and prescription fire. Photo by Steven Spickerman, USDA Forest Service

 

Potential Research Topics
Camp Nine Pines RNA contains an ecosystem that was historically maintained by fire.  Researchers could investigate local fire history and effects of fire in a rare barrens ecosystem adjacent to a dry-mesic forest.  Surveys of taxa not yet recorded include amphibians, reptiles, invertebrates, bats, and other mammals.

Ecological and Physical Description

Size
872ac (353ha)
Elevation Range
1,150' (351m) - 1,340' (408m)
Temperature Range
25°F (-4°C) - 59°F (15°C)
Primary Features

Camp Nine Pines Research Natural Area (RNA) contains one of the largest blocks of natural red pine (Pinus resinosa) and white pine (Pinus strobus) on the Chequamegon-Nicolet National Forest (CNNF). The RNA features a large area of continuous canopy pine and pine-oak forest, frost pocket barrens, a wide moisture gradient from west to east, and a home range of many large mammal species. The trees now are of an older age class [12-20 inch (30-50 cm) DBH] and the community is beginning to develop old-growth characteristics. The site is also noted for its diversity of nesting interior forest wood warblers.

Annual Precipitation

Annual precipitation averages 34.3 inches (87 cm), 68% of which falls between April and September. Average seasonal snowfall is 68.1 inches (173 cm).

Nearest Weather Station

The Drummond Ranger Station is 11 mi (17.7 km) northwest of the RNA.

Geology and Soils

The eastern section of the RNA is situated on glacial end moraine grading into glacial pitted outwash as you travel west. The majority of the RNA is carbonate bedrock of the Cable Rolling Outwash LTA.  The bedrock is greater than 100 feet from the land surface. A smaller portion of the RNA consists of sandstone (LTA Ka04), which is between 100 and 50 feet of the land surface. Geomorphologic processes include glacial meltwater deposition.
Soils are well-drained sandy loam over medium-coarse sand with end moraine on the east, grading into glacial pitted outwash as you move west. Most of the soils generally fall into the Vilas-Omega association. There is a small area that is of the Cloquet-Hiawatha association.

Aquatic Features

Several small perennial ponds and ephemeral woodland pools occur in the depressions throughout this site. The ponds are the sole water source in this dry community type and are fed by ground water and precipitation. There are no streams or rivers within three miles (5 kilometers) of this site.

Flora and Fauna

Common Plant Species

Common Animal Species

Last updated February 24, 2023