Ozark Hill Prairie

Status
Established
Year Established
1991

Location

State
Illinois
National Forest Regions
Eastern Region (R9)
Ozark Hill Prairie RNA. Photo by Lucy Tyrrell, USDA Forest Service

Ecological and Physical Description

Size
535ac (217ha)
Elevation Range
400' (122m)
Temperature Range
90°F (32°C)
Primary Features

The RNA contains relatively undisturbed examples of hill prairie, dry upland forest, dry-mesic upland forest, and mesic upland forest natural community types. The RNA includes the major part of the Ozark Hill Prairies Natural Area, which is significant because of its very high quality loess hill-prairie natural community and the presence of the uncommon timber rattlesnake (Crotalis horridus). The southern blazing star (Liatris squarrulosa) has been found within the RNA and will be probably be listed as a State Endangered Species in the near future.

Annual Precipitation

The annual precipitation averages approximately 45 inches (114 cm), and ranges between 30 and 70 inches (76.2-177 cm). Precipitation is fairly evenly distributed throughout the year. Average annual snowfall is about 9 inches (22.8 cm), but in one-third of the winters, average annual snowfall is less than 5 inches (12.7 cm).

Nearest Weather Station

Climatological information is taken from the collection station at Anna, IL, which has records dating from 1951. The station is located 10.8 miles (17.4 km) to the northeast of the RNA.

Geology and Soils

The RNA is on the high bluffs that form the east wall of the Mississippi River valley in southern Illinois. It sits on a narrow, northerly-trending, main ridge with long lateral ridges in all directions. Closely-spaced and steep-sided canyons extend from floodplains to the crest. Massive gray limestone of the Devonian Bailey Formation forms the bedrock, and Devonian chert of the Grassy Knob Formation underlies the upper slopes. Thick deposits of silty loess dating from the Pleistocene are found on the ridges and to a lesser extent on the slopes. Most of the soils on the narrow ridge crests are Alford silt, with Elsah silt loam in the valleys.

Aquatic Features

Drainage from the RNA is into the Mississippi River, via Ripple Hollow on the eastern side of the ridge and via Clear Creek Ditch and Dongola and Happy Hollows on the western side of the ridge. The drainage pattern is grossly reticulate, with dendritic tributary patterns in the lateral valleys. There is a suggestion that springs may be present, associated with the Bailey limestone,

Flora and Fauna

Common Plant Species

Common Animal Species

Last updated February 8, 2023