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Contact information
For information on Wisconsin's natural communities, contact:
Ryan O'Connor
Natural Heritage Inventory Assistant Ecologist
608-266-7714

Dry Cliff

State Rank: S4     Global Rank: G4G5   what are these ranks?

Definition

General natural community overview

Counties shaded blue have documented occurrences for Dry Cliff in the Wisconsin Natural Heritage Inventory database.

In most of Wisconsin the bedrock is buried beneath glacial materials that were deposited during the Pleistocene Ice Age. In glaciated regions, cliffs are associated with certain stretches of the Great Lakes coasts, stream-carved gorges, and the vestigial remnants of ancient, eroded mountain ranges and escarpments. In the "Driftless Area" of southwestern Wisconsin the mantle of glacial drift is absent and erosion has exposed sedimentary bedrock of Paleozoic age at many locations, most often as a linear series of vertical cliffs.

Technically, a cliff is a geologic feature, not a plant community; however they are important habitat for a number of plant and animal specialists. They can occur on virtually any rock type. Rock type, exposure, surrounding land cover and other factors create a wide variety of environmental conditions that may influence species composition. The presence or absence of fractures and other features that may hold soil particles and moisture, or the alternation of strata composed of different rock types that have different properties, can affect habitat suitability for plants and animals.

A greater proportion of limestone (dolomite) cliff sites tend to be dry compared to sandstone cliff sites, due to the potential for capillary action in sandstone to hold and slowly transport the water that is essential for plant survival. A soil profile is generally absent, or may occur as localized, usually thin deposits on ledges or in cracks. Dry cliffs may be influenced by aspect, local hydrology, or the proximity of waterbodies. Series of dry cliffs may include stretches or patches that are moist, and these often support additional species. The separation of "dry" from "moist" cliffs can be somewhat artificial, and the totality of the environment should be considered when assessing conservation values and opportunities.

Dry cliff communities occur on many different rock types, and vary in species composition. Scattered pines, oaks, cedars, and drought-adapted shrubs such as bush honeysuckle (Diervilla lonicera) and huckleberry (Gaylussacia baccata) often occur on the margins of the exposed rock, or where mineral soil has accumulated on ledges or in fissures. Floristic homogeneity between cliffs is typically rather low, but representative herbs may include the ferns common polypody (Polypodium vulgare), smooth cliff brake (Pellaea glabella), rusty woodsia (Woodsia ilvensis), and northern fragile fern (Cystopteris fragilis), along with wild columbine (Aquilegia canadensis), harebell (Campanula rotundifolia), sand cress (Arabidopsis lyrata), sleepy catchfly (Silene antirrhina), pale corydalis (Capnoides sempervirens), and rock spike-moss (Selaginella rupestris). Dry cliffs are frequently colonized by crustose lichens, which may be the most common inhabitants of bare rock environments for decades or even centuries.

Plant species composition is strongly influenced by the plant community in the immediate vicinity of the cliff, but also includes bare rock specialists, among which are some of Wisconsin's most dramatic examples of disjunct species. An example of a disjunct species is the population of Lapland rose-bay (Rhododendron lapponicum) that grows on a sandstone cliff along the Wisconsin River in the Central Sand Plains. One other population of this species is known from Wisconsin, but the next closest population is on an Adirondack mountaintop in rural New York.

Cliffs are used for denning and roosting by mammals, for nesting and roosting by birds, as hibernacula by herptiles, and also provide suitable conditions for specialized invertebrates. Besides insects, the latter group includes several very rare terrestrial gastropods.

Rare animals

Species of Greatest Conservation Need

Wisconsin Wildlife Action Plan graphic

The following Species of Greatest Conservation Need are listed according to their level of association with the Dry Cliff natural community type, based on the findings in Wisconsin's 2015 Wildlife Action Plan.

Scores: 3 = high association, 2 = moderate association, and 1 = low association. See the key to association scores for complete definitions.

Aquatic and terrestrial snailsScore
Black StriateStriatura ferrea3
Broad-banded ForestsnailAllogona profunda2
Wing SnaggletoothGastrocopta procera2
Appalachian PillarCochlicopa morseana1
Trumpet ValloniaVallonia parvula1

BirdsScore
Peregrine FalconFalco peregrinus3

Butterflies and mothsScore
Columbine Dusky WingErynnis lucilius2

Grasshoppers and alliesScore
Plains Yellow-winged GrasshopperArphia simplex1
Speckled Rangeland GrasshopperArphia conspersa1

MammalsScore
Big Brown BatEptesicus fuscus2
Eastern PipistrellePerimyotis subflavus2

ReptilesScore
GophersnakePituophis catenifer3
Gray RatsnakePantherophis spiloides3
Timber RattlesnakeCrotalus horridus3
North American RacerColuber constrictor2
Prairie SkinkPlestiodon septentrionalis1
Western WormsnakeCarphophis vermis1

Please see Section 2. Approach and Methods of the Wildlife Action Plan to learn how this information was developed.

Rare plants

The Natural Heritage Inventory has developed scores indicating the degree to which each of Wisconsin's rare plant species is associated with a particular natural community or ecological landscape. This information is similar to that found in the Wildlife Action Plan for animals. As this is a work in progress, we welcome your suggestions and feedback.

Scores: 3 = "significantly associated," 2 = "moderately associated," and 1 = "minimally associated."
Scientific Name Common Name Score
Anemone multifida var. multifida Cut-leaved Anemone 3
Anticlea elegans ssp. glaucus White Camas 1
Asplenium pinnatifidum Pinnatifid Spleenwort 3
Boechera missouriensis Missouri Rock-cress 3
Carex albicans var. albicans Dry Woods Sedge 2
Carex backii Rocky Mountain Sedge 2
Draba arabisans Rock Whitlow-grass 3
Draba cana Hoary Whitlow-grass 3
Gymnocarpium jessoense ssp. parvulum Northern Oak Fern 3
Huperzia appressa Mountain Fir Moss 2
Huperzia porophila Rock Clubmoss 1
Minuartia dawsonensis Rock Stitchwort 3
Moehringia macrophylla Large-leaved Sandwort 3
Pellaea atropurpurea Purple-stem Cliff-brake 3
Phemeranthus rugospermus Prairie Fame-flower 2
Pseudognaphalium saxicola Cliff Cudweed 3
Rhamnus lanceolata var. glabrata Lanced-leaved Buckthorn 2
Rhododendron lapponicum Lapland Azalea 1
Rhus aromatica Fragrant Sumac 1
Salix sericea Silky Willow 1
Scutellaria parvula var. parvula Small Skullcap 2
Viola sagittata var. ovata Sand Violet 1

Landscapes

The following Ecological Landscapes have the best opportunities to manage for Dry Cliff, based on the Ecological Landscapes of Wisconsin Handbook.


Map of the Ecological Landscapes of Wisconsin.


Major (3 on map)
A major opportunity for sustaining the natural community in the Ecological Landscape exists, either because many significant occurrences of the natural community have been recorded in the landscape or major restoration activities are likely to be successful maintaining the community's composition, structure, and ecological function over a longer period of time.

Important (2 on map)
Although the natural community does not occur extensively or commonly in the Ecological Landscape, one to several occurrences do occur and are important in sustaining the community in the state. In some cases, important opportunities may exist because the natural community may be restricted to just one or a few Ecological Landscapes within the state and there may be a lack of opportunities elsewhere.

Present (1 on map)
The natural community occurs in the Ecological Landscape, but better management opportunities appear to exist in other parts of the state.

Threats/Actions

Wisconsin Wildlife Action Plan graphic

What are conservation actions?

Conservation actions respond to issues or threats, which adversely affect species of greatest conservation need (SGCN) or their habitats. Besides actions such as restoring wetlands or planting resilient tree species in northern communities, research, surveys and monitoring are also among conservation actions described in the WWAP because lack of information can threaten our ability to successfully preserve and care for natural resources.

Threats/issues and conservations actions for natural communities

Considerations

The following are additional considerations for Dry Cliff in Ecological Landscapes with opportunities for protection, restoration, and/or management. For more information, see the Wildlife Action Plan.

Central Lake Michigan Coastal

Ecologically important stretches of the dolomitic Niagara Escarpment occur along the east side of the Fox River Valley, north of Lake Winnebago, and in northeastern Brown County, near Red Banks.

Central Sand Plains

Unglaciated exposures of Cambrian sandstones are uncommon but prominent features in this landscape, where they occur in association with eroded landforms such as ridges, mounds, knobs, and pinnacles, some of which are very unusual in the Midwest. Good examples occur at Mill Bluff State Park (Monroe County), in stream gorges and elsewhere on the Black River State Forest (Jackson County), and at Quincy Bluff and Wetlands State Natural Area (Adams County).

Forest Transition

Rock outcroppings provide some cliff habitat in places such as the Dells of the Eau Claire River County Park, and Rib Mountain State Park, both in Marathon County.

North Central Forest

Bedrock features are scarce and localized here except in the Penokee Range, on the landscape$apos;s northern fringe, where there are a number of dry cliffs and “balds” (bedrock glades). There are also a few cliff sites in the eastern part of the Ecological Landscape. Examples can be found on the Iron County Forest (basalt), along the Montreal River (also Iron County) and on the Chequamegon-Nicolet National Forest (e.g., McCaslin Mountain, a quartzite monadnock in Forest County).

Northeast Sands

Bedrock exposures are uncommon features in the Northeast Sands. They do occur along some of the high gradient streams in the landscape such as the Menominee and Peshtigo, and in association with isolated geologic rock features such as Butler Rock (Oconto County), Thunder Mountain (Marinette County), The Dalles of the Menominee River (Marinette County), and Hagar Mountain (Oconto County).

Northern Lake Michigan Coastal

Cliffs of the dolomitic Niagara Escarpment are striking landscape features on the west side of the Door Peninsula. Examples can be found at Peninsula and Potawatomi State Parks, Ellison Bay Bluff State Natural Area, and Death$apos;s Door County Park.

Southern Lake Michigan Coastal

The youngest bedrock exposures in Wisconsin are dolomites of Devonian age, which outcrop as low cliffs and ledges at a few locations near Lake Michigan. Examples may be seen at several locations within the Milwaukee County Park system, such as at Estabrook Park.

Southwest Savanna

Stream cut valleys expose Paleozoic sandstones and dolomites at sites such as Governor Dodge State Park, where the park$apos;s trail system permits close examination of the bedrock.

Superior Coastal Plain

Wave-carved sandstone cliffs are found on rocky headlands along the northern margin of the Bayfield Peninsula, and along the coasts of some of the Apostle Islands (including North Twin Island and Stockton Island Cliffs). Separation of dry from wet cliffs is difficult, and perhaps artificial, as even the driest bedrock associated with the Lake Superior coast may be bathed in fogs or subject to wave spray during storms.

Western Coulee and Ridges

Sandstones and dolomites of Paleozoic age outcrop at many locations, most extensively in the valleys formed by large rivers such as the Mississippi, Wisconsin, Chippewa and Black. The many good examples include Ferry Bluff (Sauk County), the Kickapoo Reserve and Wildcat Mountain State Park (Vernon County), and Maiden Rock Bluff (Pepin County).

Western Prairie

Significant bedrock exposures of dolomite and sandstone occur at Kinnickinnic and Willow River State Parks, Apple River Canyon State Natural Area, and at locations in Polk County within the St. Croix-Namekagon National Scenic Riverway.

Photos


Dry Cliff Photos

Dry Cliff Photo

Dry Cambrian sandstone cliff along the Wisconsin River. Wisconsin Dells, Sauk County.

Photo by W.A. Smith.

Dry Cliff Photo

Dry Cliff in the Driftless Area. Levis Mound, Clark County.

Photo by Emmet Judziewicz.

Dry Cliff Photo

White cedar on fissured dolomite ledges, April 2000.

Photo by Eric Epstein.

Dry Cliff Photo

Dry cliff flora: Aquilegia, Woodsia ilvensis, Viola pedata. Sandstone bluff, Quincy Bluff And Wetlands State Natural Area, Adams County.

Photo by Eric Epstein.

Dry Cliff Photo

Dry, red cedar-capped Dolomite Cliff along the Mississippi River, Pepin County.

Photo by Eric Epstein.

Dry Cliff Photo

Limestone rock outcroppings w/ garlic mustard, columbine, walking fern, & Pellaea glabella.

Photo by Christina Isenring.

Dry Cliff Photo

Photo by Thomas Meyer.

Dry Cliff Photo

Photo by Thomas Meyer.

Dry Cliff Photo

Dry Cliff, Cambrian Sandstone.

Photo by Eric Epstein.

Dry Cliff Photo

Dry cliff - Castle Mound, Jackson County.

Photo by Eric Epstein.

Note: photos are provided to illustrate various examples of natural community types. A single photograph cannot represent the range of variability inherent in a given community type. Some of these photos explicitly illustrate unusual and distinctive community variants. The community photo galleries are a work in progress that we will expand and improve in the future.

Last revised: Tuesday, November 28, 2017