The Tom S. Cooperrider - Kent Bog State Nature Preserve is a remnant of the Wisconsin Glaciation. It is a true bog with acidic waters. Unique environmental conditions have enabled it to survive.
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Location [edit]
The Kent Bog is located in its namesake city Kent, Ohio at 1028 Meloy Road at 41°7′46″N 81°21′13″W / 41.12944°N 81.35361°WCoordinates: 41°7′46″N 81°21′13″W / 41.12944°N 81.35361°W. There is parking at the beginning of the half mile boardwalk. The boardwalk trail loops around the bog, ending back at the parking lot. Along the trail there are educational signs explaining the local flora and fauna as well as the geological founding of the bog.
Geology and geography [edit]
The bog was formed during the retreat of the Wisconsin Glacier. A chunk of glacial ice broke off and was buried in sediment and glacial till from the glacial outwash. A ridge of sediment formed around the chunk of ice. This caused the formation of a deep kettle hole lake. The total original size of the kettle-hole lake was about 50 acres.
As the climate continued to warm, plant life spread over the lake. Although it is not exclusive, it is heavily dominated in sphagnum moss. This began the process by which the lake began to fill with peat becoming a bog. There are only a few areas that standing water is visible from the boardwalk.
Flora and fauna [edit]
It is a coniferous, boreal forest with many spruce, fir, and tamarack trees. The tamarack is a tree common to the upper parts of Canada and Alaska. It is able to withstand very cold temperatures. Unlike other conifers, it is deciduous losing its needles in the winter. This transforms the look of the Kent Bog during the seasons. The trees tower above the waters of the bog.
The bog is home to the spotted turtle and throughout the preserve, there are turtle tunnels under the boardwalk.
References [edit]
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