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Cedar Bog Nature Preserve is the largest and best calcareous bog or fen in Ohio. One of the most characteristic plants of this preserve is white cedar or arbor-vitae. Significant boreal, as well as prairie and coastal plain species, occur here. Some of the more unusual plants include showy lady's-slipper orchid, smaller fringed gentian, swamp ...
in Uncategorized. Cedar Bog will be closed to the public on the dates listed in the picture. Print page. A national natural landmark, Cedar Bog Nature Preserve is the largest and best example of a boreal and prairie fen complex in Ohio.
Cedar Bog in Ohio is a rare and special ecosystem, featuring both a fen and swamp forest environment. The landscape is mostly flat, with open wetlands and sections of dense forest. Unlike true bogs, which are acidic, fens like Cedar Bog are fed by mineral-rich groundwater, creating more alkaline conditions that support a wider variety of plant species.
Cedar Bog is a protected area of about 450 acres of land which remains from the original area of approximately 7,000 acres. Cedar Bog is, in actuality, a “fen” and not a bog. A fen is a wetland area that drains water, whereas a bog retains water. Cedar Bog State Nature Preserve is a fen left behind by the retreating glaciers of the ...
Cedar Bog located in Champaign County, Ohio, is not actually a bog. A bog receives water through rainwater, and loses water through evaporation. As time goes on plants decay and settle on the bottom where water can no longer escape. Cedar bog is a fen, which gains water through rain and springs. Cedar bog is in the middle of the low crest ...
Modern Cedar Bog. Though it might appear to be a relatively large fen, Cedar Bog is only a fraction of the size it was thousands of years ago. Significant land-use changes, including the human-made drainage modification of the Mad River during the early 1900s, eliminated thousands of acres of what was once part of this natural fen environment.
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Cedar Bog (Fen) Landscape. At Cedar Bog, the landscape of the fen is defined by its unique geology and hydrology. The fen sits atop limestone and gravel deposits left behind by retreating glaciers, creating an environment where cool, mineral-rich groundwater seeps to the surface. This constant flow of groundwater maintains a neutral to slightly ...
