Michigan's Natural Communities
Granite Bedrock Glade
State Rank: S2
Global Rank: G3G5
County Distribution Map
Granite bedrock glade consists of an open forested or savanna community found where knobs of granitic bedrock types are exposed at the surface. The sparse vegetation consists of scattered open-grown trees, scattered shrubs or shrub thickets, and a partial turf of herbs, grasses, sedges, mosses, and lichens. Granite bedrock glades typically occupy areas of steep to stair-stepped slopes, with short cliffs, and exposed knobs of bedrock. The community occurs in the western Upper Peninsula with primary concentrations in Marquette, Baraga, and Dickinson Counties.
A broad range of igneous and metamorphic rocks, including gneiss, schist, granite, and quartzite, are often loosely referred to as “granitic” or “granite.” Granite bedrock glade occurs on granite, schist, gabbro, gneiss, slate, “iron formations,” greenstones, and a diversity of other resistant igneous and metamorphic rock types of the Michigamme Highlands that formed during the Precambrian Era, approximately 600 to 3,500 million years ago. These rock types form large rounded ridges that were shaped and polished by the continental ice sheets about 10,000 years ago.
The community occurs both inland and adjacent to the Lake Superior shoreline. Granitic bedrock glades typically occupy areas of steep to stair-stepped slopes, with short cliffs, exposed bedrock knobs, and talus slopes occurring at the base of the bedrock exposures. The forest types surrounding granitic bedrock are typically dry-mesic northern forest or mesic northern forest. Along the Lake Superior shoreline, boreal forest is a common associate and in localized areas, granite bedrock glade can occur adjacent to granite bedrock lakeshore, granite lakeshore cliff, volcanic cobble shore, and sand and gravel beach.
Soil development is generally restricted to cracks and depressions within the rock, where plant debris and sand and gravel resulting from mechanical and biological weathering of the bedrock can accumulate. These soils are typically very shallow and low in nutrients. Thin soils are typically 1 to 4 cm (0.4 to 1.6 in) deep, strongly acidic, and characterized by low moisture availability. Exfoliation of rock slabs and frost wedging is characteristic of granite and contributes to soil formation. Numerous large boulders, slabs, and small granitic rocks occur scattered throughout the glades, and talus slopes occur at the base of many bedrock exposures.
Windthrow, desiccation, fire, and exfoliation of rock slabs are all important natural processes for bedrock glade communities. Windthrown trees are common as a result of thin soils and strong winds associated with Lake Superior. Thin soils, cold winter temperatures, steady winds, and summer droughts make vegetation especially prone to desiccation. Rain that lands on sloping bedrock outcrops quickly runs off to lower elevation areas, further contributing to dry conditions and removing accumulated plant debris and small rock debris that could otherwise initiate soil formation. Glades are subject to fires from both lightning and human sources. Both white pine and red pine form a supercanopy and are prime targets for lightning strikes associated with Lake Superior storms. The open structure and elevated position of glades make them ideal places for historic and modern human gathering, which were and are associated with escaped campfires.
Vegetation goes through a slow succession from lichens and mosses in moist rock depressions to gradual establishment of mats of herbaceous vascular plants. As soil gradually develops, these mats begin supporting localized clumps of shrubs and small trees. Dominant trees of the open canopy include stunted red oak (Quercus rubra) and white pine (Pinus strobus). Other common trees, occurring in the scattered and low canopy and also as saplings in the understory, include red pine (P. resinosa), quaking aspen (Populus tremuloides), big-toothed aspen (P. grandidentata), and paper birch (Betula papyrifera). Common shrubs include low sweet blueberry (Vaccinium angustifolium), Canada blueberry (V. myrtilloides), bearberry (Arctostaphylos uva-ursi), common juniper (Juniperus communis), serviceberry (Amelanchier interior), wild red raspberry (Rubus strigosus), smooth sumac (Rhus glabra), choke cherry (Prunus virginiana), pin cherry (P. pensylvanica), and bush honeysuckle (Diervilla lonicera). Among the commonly occurring forbs are cow-wheat (Melampyrum lineare), slender ladies’-tresses (Spiranthes lacera), large-leaved aster (Aster macrophyllus), jumpseed (Polygonum virginianum), western smartweed (Polygonum douglasii), wild strawberry (Fragaria virginica), and harebell (Campanula rotundifolia). Commonly occurring graminoids include Pennsylvania sedge (Carex pensylvanica), poverty grass (Danthonia spicata), hair grasses (Deschampsia flexuosa and D. cespitosa), rice grass (Oryzopsis pungens), and panic grasses (Panicum columbianum, P. depauperatum, and P. linearifolium). Common ferns include rusty woodsia (Woodsia ilvensis), marginal woodfern (Dryopteris marginalis), spinulose woodfern (D. carthusiana), common polypody (Polypodium virginianum), maidenhair spleenwort (Asplenium trichomanes), and bracken fern (Pteridium aquilinum). Areas of exposed bedrock are dominated by a diverse array of lichens (e.g., Cladina spp.) and mosses (e.g., Polytrichum spp.).
Ants are quite abundant in this dry, thin-soiled environment. Black bears use this habitat, possibly because of the abundant ants, other insects, and wild fruit.
- Dryopteris filix-mas (male fern, state special concern)
- Dryopteris fragrans (fragrant cliff woodfern, state special concern)
- Opuntia fragilis (fragile prickly-pear, state endangered)
- Ribes oxyacanthoides (northern gooseberry, state special concern)
- Woodsia alpina (northern woodsia, state threatened)
- Falco columbarius (merlin, state threatened)
- Falco peregrinus (peregrine falcon, state endangered)
- Haliaeetus leucocephalus (bald eagle, state threatened)
Biodiversity Management Considerations
The thin soils and lichen cover are easily destroyed by off-road vehicles or excessive foot traffic. Many seasonal cabins are built within the glades, resulting in major degradation, including the introduction of non-native plants. Fill is often introduced for septic systems, also increasing habitat for invasive plants. Invasive plants that threaten the diversity and community structure in granite bedrock glade include sweet cherry (Prunus avium), sheep sorrel (Rumex acetosella), common mullein (Verbascum thapsus), spotted knapweed (Centaurea maculosa), ox-eye daisy (Chrysanthemum leucanthemum), hawkweeds (Hieracium spp.), common St. John’s-wort (Hypericum perforatum), timothy (Phleum pratense), Canada bluegrass (Poa compressa), and Kentucky bluegrass (P. pratensis). Monitoring and control efforts to detect and remove invasive plants are critical to the long-term viability of bedrock glades. Maintaining a mature, unfragmented forested buffer around bedrock glades may help limit the local seed source for invasive species distributed by wind or birds.
Open conditions within glades can be maintained by allowing wildfires to move through the community where safety and other conditions permit. Prescribed fire management of adjacent dry-mesic forests should include areas of bedrock glade when feasible.
Species composition may vary with bedrock type and aspect.
Similar Natural Communities
Northern bald, granite bedrock lakeshore, granite cliff, granite lakeshore cliff, volcanic bedrock glade, volcanic bedrock lakeshore, volcanic cliff, sandstone bedrock lakeshore, sandstone cliff, and dry-mesic northern forest.
- Albert, D.A., P. Comer, D. Cuthrell, D. Hyde, W. MacKinnon, M. Penskar, and M. Rabe. 1997. The Great Lakes bedrock lakeshores of Michigan. Michigan Natural Features Inventory, Lansing, MI. 218 pp.
- Catling, P.M., and V.R. Brownell. 1999. The flora and ecology of southern Ontario granite barrens. Pp. 392-405 in Savannas, barrens, and rock outcrop plant communities of North America, ed. R.C. Anderson, J.S. Fralish, and J.M. Baskin. Cambridge University Press, Cambridge, UK. 480 pp.
- Dorr, J.A., Jr., and D.F. Eschman. 1970. Geology of Michigan. University of Michigan Press, Ann Arbor, MI. 470 pp.
- Faber-Langendoen, D., ed. 2001. Plant communities of the Midwest: Classification in an ecological context. Association for Biodiversity Information, Arlington, VA. 61 pp. + appendix (705 pp.).
- Given, D.R., and J.H. Soper. 1981. The arctic-alpine element of the vascular flora at Lake Superior. National Museums of Canada, Publication in Botany 10: 1-70.
- LaBerge, G.L. 1994. Geology of the Lake Superior region. Geoscience Press, Phoenix, AZ. 313 pp.
- Reed, R.C., and J. Daniels. 1987. Bedrock geology of northern Michigan. State of Michigan Department of Natural Resources. Map: 1: 500,000.
- Shure, D.J. 1999. Granite outcrops of the southeastern United States. Pp. 99-118 in Savannas, barrens, and rock outcrop plant communities of North America, ed. R.C. Anderson, J.S. Fralish, and J.M. Baskin. Cambridge University Press, Cambridge, UK. 480 pp.
- Simpson, T.B., P.E. Stuart, and B.V. Barnes. 1990. Landscape ecosystems and cover types of the reserve area and adjacent lands of the Huron Mountain Club. Occasional Papers of the Huron Mountain Wildlife Foundation, Number 4. 128 pp.
- Kost, M.A., D.A. Albert, J.G. Cohen, B.S. Slaughter, R.K. Schillo, C.R. Weber, and K.A. Chapman. 2007. Natural Communities of Michigan: Classification and Description. Michigan Natural Features Inventory, Report No. 2007-21, Lansing, MI.
Page updated on 02-11-2008