Kent Bog is a local (and state) treasure, and is heavily used by the people of Kent and surrounding areas.That such a place would survive in a rather heavily developed area is a bit of a miracle. I believe local support for the bog's well being has warded off one or two development schemes that would have taken place on its margins. If you get the chance, visit Kent Bog. Directions and other details are RIGHT HERE.
As fate would have it, the day that I visited was wet. Very wet. Rolling waves of showers washed over nearly all day, punctuated by brief respites from the rain. I'm certainly not going to melt, but camera gear does not like being drenched. Nonetheless, I and my camera made the trek through the bog, and managed to come away with a few images.
A couple of hundred miles to the north, Tamarack becomes extremely common but in Ohio it is limited to the relatively few bogs that remain. At some point in its distant past, Kent Bog was an open lake. It was created by a giant ice block calved from the retreating Wisconsin Glacier about 12,000 years ago. Plants more or less immediately began the process of colonizing the cold wet soil and mire left in the glacier's wake. Kettle lakes initially were ringed with plant life, including Tamarack. Over time, the plants grew out into the lake, and ultimately flora completely fills the lake - the natural fate that most Ohio bogs have experienced. Kent Bog has no open water remaining, and its thick cloak of Tamarack is essentially its last hurrah. Eventually the bog will transform into a deciduous swamp woods dominated by maple and other softwoods.
Kent Bog will be looking exceptionally showy for the next few weeks, but it looks great at any season. I hope you find the time to visit and experience one of our few remaining bogs.