Both can build peat. Their water supply helps explain why their plants and chemistry differ.
Bog: rain and snow ↓
Mainly precipitation-fed, usually acidic and low in nutrients.
Fen: groundwater enters ↖
Water moving through soil or rock brings minerals. Fens also receive precipitation.
These terms describe origin, shape, vegetation, or region, so they can overlap.
Kettle & basin: Develop in hollows; some kettles were left by melting glacial ice.
Raised & domed: Accumulating peat lifts the central surface above mineral-rich water.
Patterned: Ridges, pools, and water tracks form mosaics of bog and fen.
Pocosin: Dense shrub-and-pine peatlands of the southeastern Coastal Plain.
Mountain: Peat wetlands in cool, wet upland settings, such as Cranberry Glades.
Coastal muskeg: A regional term for peat wetlands, including those in Southeast Alaska.
Melting glacial ice can leave a lake-filled hollow. As plant mats spread and peat accumulates, a peatland may develop over thousands of years.
Pocosins belong to the southeastern Coastal Plain; they do not share the northern kettle-ice origin. At Green Swamp, shrub peatlands sit beside sunny, fire-maintained pine savannas.
Carolina bays are oval depressions that can hold several wetland types—not all are bogs or pocosins. Many of Green Swamp’s carnivorous plants grow in open savannas rather than dense shrub shade.
Prescribed fire can help maintain savannas. Drought or drainage can instead allow peat itself to burn and damage a peatland.
NOAA: pocosins · Carolina bays · Green Swamp
Educational illustrations created with AI assistance; simplified, not to scale.
A place name does not tell the whole story. Cedarburg Bog includes lakes, sedge communities, and wooded wetlands. Mineral-rich groundwater keeps much of the system near neutral pH. These photographs show the different communities within this wetland complex. Learn about Cedarburg’s wetland communities.






These examples were chosen for their different landscapes, ecological importance, and opportunities to learn. This is a representative selection, not a complete inventory or a ranking by size. Some are true bogs; others show related peatland habitats.
Tap a numbered marker for its description. On a small screen, swipe the map sideways or use the numbered guide below.
Kettle bog
A clear local example of bog development in glacial kettle holes, with an open pool, floating sedge–sphagnum mat, and tamarack wet forest.
Learn more & check visitor informationKettle bog
A floating plant mat surrounds the remaining open water of an ancient glacial kettle lake. A useful place to learn how wetland communities change across a basin.
Learn more & check visitor informationPatterned wetland complex
Our local example contains lakes, sedge communities, and wooded ridges. Mineral-rich groundwater keeps much of it near neutral pH; the name does not mean the whole complex is an acidic, rain-fed bog.
Learn more & check visitor informationPatterned peatland
An expansive northern peatland landscape where raised bogs, fens, and water tracks occur together. Big Bog State Recreation Area offers a boardwalk introduction.
Learn more & check visitor informationRaised bog
Peat accumulation has raised the central bog above its surroundings. The boardwalk introduces the striking transition from forested wetland to open bog.
Learn more & check visitor informationGlacial-basin peatland
A protected Pocono wetland known for sphagnum, cranberries, and carnivorous pitcher plants. Explore its formation and communities through the preserve’s guided programs.
Learn more & check visitor informationMountain peatland
High-elevation glades bring a very different setting to the map: open peat wetlands surrounded by Appalachian forest. Their cool mountain setting supports distinctive wetland plants.
Learn more & check visitor informationSoutheastern pocosin
A major example of dense shrub-and-pine peatland on the Atlantic Coastal Plain. Restoring water levels helps protect the peat and reduce damaging peat fires.
Learn more & check visitor informationPocosin & pine-savanna mosaic
Dense evergreen-shrub pocosin lies alongside open longleaf pine savannas. Many celebrated carnivorous plants grow in the sunny savannas, not deep within the shrub thickets.
Learn more & check visitor informationForested peatland
A peat-forming forested swamp rather than a classic open northern bog. Its restoration shows why keeping peat wet matters for habitat, carbon storage, and fire risk.
Learn more & check visitor informationRaised plateau bog
An unusual raised bog on the Olympic Peninsula, protected as a Natural Area Preserve. This is a conservation and research example; check with Washington DNR about access.
Learn more & check visitor informationMarkers show approximate locations, not wetland boundaries or trailheads. Access varies, particularly at research preserves; follow each land manager’s guidance.
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